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THE MINERAL STATUS O F DAIRY CATTLE IN ECUADOR AND IN MICHIGAN M ichigan S ta te U niversity University Microfilms International 300 N. Zeeb Road, Ann Arbor, Ml 48106 Ph.D. 1985 PLEASE NOTE: In all c a s e s this material has been filmed in th e best possible w ay from the available copy. Problems encountered with this d ocu m en t have been identified here with a ch eck mark V 1. G lossy photographs or p a g e s ______ 2. Colored illustrations, paper or print_______ 3. Photographs with dark b ack grou n d _____ 4. Illustrations are poor c o p y _______ 5. P a g es with black marks, not original c o p y ______ 6. Print sh ow s through as there is text on both sides of p a g e ________ 7. Indistinct, broken or small print on several pages 8. Print ex c eed s margin requirem ents______ 9. Tightly bound co p y with print lost in s p in e ________ 10. Computer printout p ages with indistinct print_______ 11. P a g e (s )_____________ lacking w hen material received, and not available from sch o o l or author. 12. Page(s) 13. Two p a ges n u m b ered 14. Curling and wrinkled p a g e s ______ 15. Dissertation co n ta in s p ages with print at a slant, filmed a s received__________ 16. Other **** **** . seem to b e m issing in numbering only as text follow s. . Text follows. 149 and A p p en d ix I I , p age 15__________________________________ University Microfilms International THE MINERAL STATUS OF DAIRY CATTLE IN ECUADOR AND IN MICHIGAN By Telmo B. O l e a s A DISSERTATION Submitted t o Michigan S t a t e U n i v e r s i t y i n p a r t i a l f u l f i l l m e n t o f t h e r e q u ir e m e n ts f o r the degre e of DOCTOR OF PHILOSOPHY Department of Animal Science 1985 ABSTRACT THE MINERAL STATUS OF DAIRY CATTLE IN ECUADOR AND IN MICHIGAN By Telmo B. O l e a s The m i n e r a l s t a t u s o f d a i r y c a t t l e was s t u d i e d in f i v e r e g i o n s in th e Chimborazo p r o v i n c e of Ecuador, and one re g i o n in Shiawassee c o u n ty , Michigan. I n o r d e r t o d i a g n o s e m i n e r a l d e f i c i e n c i e s , i m b a l a n c e s and to x icities, analyzed. m i n e r a l s in b lo o d serum, pasture and s o i l were Three farms were sampled in each re g i o n of Ecuador and one f ar m i n M i c h i g a n . B l o o d s a m p l e s were c o l l e c t e d from 10 l a c t a t i n g d a i r y cows and 10 a n i m a l s u n d e r one y e a r o f age from each farm. in each P a s t u r e and s o i l sa m ple s were taken from f i v e f i e l d s farm . H alf of each p a s t u r e s a m p l e was washed w i t h d i s t i l l e d w a t e r and t h e o t h e r h a l f was n o t , t o e s t a b l i s h t h e e x t e n t of s o i l c o n ta m i n a ti o n through m i n e r a l a n a l y s i s . S e v e r a l m i n e r a l d e f i c i e n c i e s f o r b o t h p l a n t s and a n i m a l s were found i n the r e g i o n s s t u d i e d . Most o f th e s o i l s needed l im i n g . n e c e s s a r y f o r c orn and p a s t u r e g r a s s e s . N itro g en f e r t i l i z a t i o n i s Phosphorus and potas sium f e r t i l i z a t i o n i s n e e d e d f o r c r o p s i n m o st o f t h e s o i l s s t u d i e d . Molybdenum i s needed i n one r e g i o n o f Ecuador and i n Michigan f o r legume c ro p s . Zinc i s needed i n Michigan f o r corn c u l t i v a t i o n . Coppe r f e r t i l i z a t i o n i s n e e d e d f o r l e g u m e s i n a l l t h e r e g i o n s studied. S u l f u r i s n e e d e d f o r l e g u m e s i n one r e g i o n i n Ecuador and i n Michigan. I t was co n clu d ed t h a t a n im a l s from a l l t h e r e g i o n s s t u d i e d needed n i t r o g e n , s u p p l e m e n ta t io n . calciu m , phosphorus, so d iu m and c o p p e r Z inc, manganese and s e le n iu m was d e f i c i e n t for a n im als i n s e v e r a l r e g i o n s o f Ecuador and i n Michigan. N em ato des and t r e m a t o d e s e g g s , and c o c c i d i a o o c y s t s were found i n t h e f e c e s o f a n i m a l s from a l l t h e r e g i o n s i n E c u a d o r , bu t n o t i n Michigan. I n g e n e r a l s o i l s and p a s t u r e s i n E c u a d o r a r e d e f i c i e n t i n n itrogen, copper, phosphorus, su lfu r, potassium , m anganese and c a l c i u m , molybdenum, selenium . zinc, These m in e ra l d e fic ie n c ie s d r a m a ti c a l ly decrease l iv e s t o c k production. DEDICATED TO My f a t h e r , b r o t h e r and s i s t e r s i n Ecuador, t o t h e memory o f my mother, and t o t h e R obert Cook f a m i l y in Michigan. ACKNOWLEDGMENTS The a u t h o r expresses sin cere g ratitu d e to h i s m ajor p r o f e s s o r , D r . R o b e r t M. C o o k , w h o s e c o n t i n u o u s academ ic g u id a n c e , p a t i e n c e and moral s u p p o r t made t h i s work p o s s i b l e . G ratitu d e i s a l s o e x t e n d e d t o t h e o t h e r members o f h i s g r a d u a t e c o m m i t t e e , Dr. Duane U l l r e y , Dr. J o h n G i l l , Ms. S a l l e e Anderson and Dr. A l v i n Smucker f o r t h e i r h e l p d u r in g t h e c o u rs e o f t h i s work, and f o r t h e i r academic guidance. The m o s t sincere g ratitu d e is expressed to the S w is s T e c h n ic a l C o o p eratio n for the f i n a n c i a l su p p o rt p ro v id e d for graduate school for the research p ro je c t. S incerest appreciation i s e x t e n d e d t o Dr. T o n i R i h s o f t h e S w is s T e c h n i c a l C o o p e r a t i o n f o r h i s s u p p o r t , f r i e n d s h i p and encouragement. Thanks a re exten ded t o INIAP (N atio n al In stitu te A g r i c u l t u r a l and L i v e s t o c k R e s e a r c h ) i n E c u a d o r . provided fin an cial sup p o rt for g rad u ate school of INIAP a l s o and f o r the research p r o je c t. The a u th o r i s g r a t e f u l t o Dr. Ronald N e l s o n , former chairman o f t h e A n im al S c i e n c e D e p a r t m e n t , and t o Dr. Mayn ard H o g b e r g , chairman of t h e Department of Animal S c i e n c e , f o r the f i n a n c i a l s u p p o r t through a G raduate Research A s s i s t a n s h i p . S i n c e r e s t a p p r e c i a t i o n i s extended to th e p r o f e s s o r s o f th e D e p a r t m e n t o f A n im al S c i e n c e , especially t o Dr. J. W illiam Thomas, Dr. Roy Emery, Dr. Werner B e r g e n and Dr. J o h n Huber f o r t h e i r h e l p and f r i e n d s h i p . A l s o , a s p e c i a l t h a n k s t o Dr. Kim W ilson f o r h i s f r i e n d s h i p and encouragement. G ratitu d e i s e x t e n d e d t o t h e g r a d u a t e and u n d e r g r a d u a t e s t u d e n t s of t h e Department of Animal S c i e n c e , e s p e c i a l l y those i n Dr. R o b e r t Co ok 's l a b o r a t o r y f o r t h e i r h e l p and f r i e n d s h i p . Very s p e c i a l thanks t o Miss N a t h a l i e Kik, who h e l p e d w ith a l l t h e a n a l y t i c a l work o f t h i s r e s e a r c h p r o j e c t . I n Ecuador t h e h e l p c o l l e c t i n g samples of Mr. Thelmo He rvas and Mr. F a u s t o M e r i n o i s a c k n o w l e d g e d . T h e i r f r i e n d s h i p and d e d i c a t i o n t o work i s g r e a t l y a p p r e c i a t e d . A lso in Ecuador, thank s a r e exte nded t o t h e p e r s o n n e l o f t h e N u t r i t i o n Department who made p a r t o f t h e a n a l y s e s . The a u t h o r i s m o st g r a t e f u l t o t h e d a i r y f a r m e r s i n E c ua d or and M i c h i g a n i n whose f a r m s t h e samples were c o l l e c t e d . TABLE OF CONTENTS Page INTRODUCTION 1 LITERATURE REVIEW 3 M i n e r a l S t a t u s o f S o i l - pH, n i t r o g e n , c a l c i u m , p h o s p h o r u s , p o t a s s i u m , m agnesium , s u l f u r , so d iu m , c h l o r i n e , b o r o n , i r o n , m a n g a n e s e , s e l e n i u m , c o b a l t , molybdenum, z i n c , copper. Soil analysis. 5 M ineral S tatus of Plants and Animal Requirements- Soi 1 - p l a n t and p l a n t - a n i m a l re la tio n sh ip s. N itro g en , calciu m , p h o s p h o r u s , p o t a s s i u m , so d iu m , magnesium, c o p p e r an d m o l y b d e n u m , s u l f u r , i r o n , manganese, z i n c , c o b a l t , s e le n iu m , io d in e . Plant analysis. 39 Blood M i n e r a l s and D e f i c i e n c i e s D i a q n o s i s C a l c i u m and p h o s p h o r u s , m agne sium, so dium , p o tas siu m and c h l o r i n e , i r o n , z i n c , copper, c o b a l t , manganese, se l e n i u m , i o d in e . Blood analysis. 92 G a s t r o i n t e s t i n a l P a r a s i t i s m i n D airy C a t t l e Nematodes, t r e m a to d e s , p r o to z o a . C o n t r o l , diagnosis. 103 MATERIALS AND METHODS 109 RESULTS AND DISCUSSION 116 M i n e r a l s i n S o i l s - F e r t i l i z a t i o n p r a c t i c e s in E c u a d o r . S o i l a n a l y s i s . S o i l pH, o r g a n i c m a tte r, te x tu r e , n itro g e n , phosphorus, potassium , c a l c i u m , m agnesium , sodium , c o b alt, i r o n , m an g a n es e, m olybdenum , s e l e n i u m , s u l f u r , co pper. 118 N u t r i e n t s i n P a s t u r e s - P a s t u r e management in Ecuador. Ash, c ru d e f i b e r , n i t r o g e n , c a l c i u m , p h o s p h o r u s , magnesium, p o tassiu m , sodium , c o p p e r , iro n , zin c, c o b a lt, manganese, molybdenum, se leniu m . 154 v M inerals in B l o o d - C a l c i u m , phosphorus, m agnesium , sodium and p o t a s s i u m , i r o n , c o p p e r , z i n c , manganese, s e l e n i u m , c o b a l t . 189 G astrointestinal P arasites- 212 SUMMARY 221 LITERATURE CITED 225 APPENDIX I M ethods o f e x t r a c t i o n f o r m i n e r a l s in s o i l s , c r i t i c a l r a n g e s f o r m i n e r a l s i n s o i l s , and s u f f i c i e n c y r a n g e s o f m i n e r a l s i n c o r n and alfalfa. T ypical m ineral c o n c e n tra tio n ru m in a n ts . I 1 -2 I 3 in blood of Liming recommendations. N i t r o g e n , phosphorus, p o t a s s i u m , m anganese and z i n c f e r t i l i z a t i o n g u i d e s f o r c o rn and a l f a l f a . I 4-9 I 8 Composition of a t r a c e m i n e r a l s a l t . APPENDIX I I Average m i n e r a l c o m po sitio n per farm and o f sample i n s o i l , p a s t u r e s and blood. type II -16 APPENDIX I I I B o t a n i c a l co m po sitio n of p a s t u r e sa mples. vi I l l 1-3 LIST OF TABLES page G eographical l o c a t i o n o f the r e g i o n s s t u d ie d . 110 Experimental d e s ig n s . 112 S o i l pH, organic m atter, and textu re. 120 S o i l n i t r a t e s , phosphorus, potassium, calciu m , and magnesium. 126 S o i l sodium, c o b a l t , iro n , manganese, and molybdenum. 138 S o i l s e l e n i u m , z i n c , s u l f a t e s , and copper. 146 P astu re a sh , crude f i b e r . 157 crude p r o t e i n , and P a s t u r e c a l c i u m , p h osp h o ru s, sodium, potassium , and magnesium. 163 P astu re copper, ir o n , z in c , c o b a lt , and manganese. 173 P asture molybdenum and selenium . 184 B lo o d serum c a lc iu m , p h o sp h o ru s, sodium, potassium , and magnesium. 190 B lo o d serum i r o n , c o p p e r , manganese, and selenium . 199 z in c , Blood serum c o b a lt. 210 Nematodes. 213 Nematodes, trematodes, and c o c c id ia . 215 v ii LIST OF FIGURES Page F i g u r e 1. S o i l pH 121 F ig u re 2. So il organic matter 123 F i g u r e 3. Soil nitrogen 127 F i g u r e 4. S o i l phosphorus 129 F i g u r e 5. S o i l p o tas siu m 130 F i g u r e 6. S o i l c alciu m 132 F i g u r e 7. S o i l magnesium 134 F ig u r e 8. S o i l p o t a s s i u m and magnesium a s a percen t of t o t a l bases 135 F i g u r e 9. S o i l sodium 136 F i g u r e 10. Soil cobalt 139 F i g u r e 11. Soil iron 140 F i g u r e 12. S o i l manganese 142 F i g u r e 13. S o i l molybdenum 144 F i g u r e 14. S o i l se leniu m 147 F ig u re 15. S o il zinc 148 F i g u r e 16. Soil su lfu r 151 F i g u r e 17. S o i l copper 153 F i g u r e 18. P a s t u r e ash 158 F i g u r e 19. P a s t u r e c ru de f i b e r 160 F i g u r e 20. Pasture p ro tein 161 F ig u r e 21. P a s t u r e calcium 164 F i g u r e 22. P a s t u r e phosphorus 166 F ig u re 23. P a s t u r e maganesium 168 F i g u r e 24. P a s t u r e sodium 169 v iii Figure 25. P a s t u r e potassium 171 Figure 26. P a s t u r e copper 174 Figure 27. P a s t u r e i r o n 176 Figure 28. P a s t u r e z in c 178 Figure 29. P a s t u r e c o b a l t 180 Figure 30. P a s t u r e manganese 182 Figure 31. P a s t u r e molybdenum 185 Figure 32. P a s t u r e selenium 187 Figure 33. Blood serum calcium 192 Figure 34. Blood serum phosphorus 193 Figure 35. Blood serum magnesium 195 Figure 36. Blood serum magnesium 196 Figure 37. Blood serum potas si um 197 Figure 38. Blood serum i r o n 200 Figure 39. Blood serum copper 202 F i g u r e 40. Blood serum z in c • 204 Figure 41. Blood serum manganese 206 Figure 42. Blood serum selenium 208 Figure 43. Blood serum c o b a l t 221 ix INTRODUCTION In 1976 Ecuador had an e s t i m a t e d 1,088,224 m i l k i n g cows t h a t p r o d u c e d 704 m i l l i o n kg o f m i l k (647 kg o r 1 ,4 2 6 l b / c o w / y e a r ) (M.A.G., Ecuador, 1976). the production of T h is p r o d u c t i o n i s low when compared t o the S ta te Departm ent of A g r i c u l t u r e , of M ichigan 1984), w h e re in 1983 ( M i c h ig a n 4 04 ,0 0 0 d a i r y cows p r o d u c e d 2,507 m i l l i o n kg o f m i l k f o r an a v e r a g e o f 6,2 07 kg (1 3,8 83 l b ) / c o w / y e a r . production is One o f t h e m o st i m p o r t a n t c a u s e s f o r low inadequate m in eral t o x i c i t y and i m b a l a n c e s . n u tritio n : d eficien cies, A sound m i n e r a l n u t r i t i o n p r o g r a m i s e a s y t o implement, w i t h minimal work and low c o s t . The b e n e f i t s a r e immediate. The U n iv e r s ity o f F lo r id a i s a lea d er in m ineral research in L atin America. S e v e r a l i n v e s t i g a t io n s have been ca rr ie d out in d i f f e r e n t c o u n tr ie s (McDowell e t a l . , d e f i c i e n c i e s and t o x i c i t i e s . 1983) to diagnose mineral In Ecuador (W ils o n , 1975) s o i l s , p a s t u r e s and anim al t i s s u e s h a ve been a n a ly z e d in d i f f e r e n t region s. C l i n i c a l s i g n s , rep rod uctive problem s, low production and lab ora tory s t u d ie s in d ic a te probable m ineral problems. A lthough s e v e r e m ineral d eficien cies or to x icities in a n im a l s show d r a m a ti c s i g n s , b o r d e r l i n e p r o b le m s, which a r e the most common, a r e d i f f i c u l t t o d iag no s e by c l i n i c a l s i g n s a l o n e , and t h e u se o f c h e m i c a l a n a l y s i s o f s o i l s , p a s t u r e s and a n i m a l tis s u e s is necessary. F u rth erm o re , improper m in e r a l n u t r i t i o n can be confu sed w ith o t h e r n u t r i t i o n a l p r o b l e m s , in fectio u s disease (Underwood, 1981). p a r a s i t i s m and 2 The o b j e c t i v e s o f t h i s s t u d y were t o d e t e c t p o s s i b l e m i n e r a l d e f i c i e n c i e s o r t o x i c i t i e s i n t h e C h im b o r a z o r e g i o n o f E c u a d o r thro ugh the e l e m e n t a l a n a l y s i s of s o i l s , p a s t u r e s and bloo d ; t o compare t h e s e f i n d i n g s w i t h t h e m i n e r a l s t a t u s o f a d a i r y farm i n Michigan; n u tritio n . and t o p r o v i d e r e c o m m e n d a t i o n s f o r p r o p e r m i n e r a l LITERATURE REVIEW The l i t e r a t u r e r e v i e w d e a l s w i t h 1) n u t r i e n t c o n t e n t of p a s t u r e s ; m in e ra l c o n te n t of soils; 2) 3) m i n e r a l s i n b lo o d ; and 4) g a s t r o i n t e s t i n a l p a r a s i t i s m i n ruminants. T h is r e v ie w t r i e s t o r e l a t e th e m i n e r a l s t a t u s o f t h e s o i l t o t h e m i n e r a l s t a t u s and p r o d u c t i v i t y of f o r a g e s . The e f f e c t of e l e m e n t a l c o n c e n t r a t i o n i n p l a n t s on the m i n e r a l s t a t u s o f c a t t l e and o t h e r a n im a l s i s d i s c u s s e d , as i s t h e use o f s o i l , p l a n t and anim al tissu e an aly ses as a mean o f d iag n o sin g m in eral d e f i c i e n c i e s or t o x i c i t i e s . The m i n e r a l c o n t e n t o f s o i l s i s compared t o t h e m i n e r a l r e q u i r e m e n ts o f p l a n t s , p a r t i c u l a r l y f o r a g e s f o r ruminants. The e x p e c t e d c o n s e q u e n c e s o f n u t r i e n t d e f i c i e n c i e s i n t h e s o i l on c rop y i e l d a re m entioned, as w e l l as th e p o s s i b l e e f f e c t s of fertilizatio n . Each m i n e r a l sections: 1) found in p a s tu r e s 3) in f i v e c o n te n t of the m in eral in p l a n t s in r e l a t i o n to s o i l s t a t u s and f e r t i l i z a t i o n ; forages, is d iscu ssed 2) c o n te n t of the m in e ra l in requirem ents of d a iry c a t t l e for the m in e ra ls; 4) d e f i c i e n c i e s or t o x i c i t i e s of the m i n e r a l in ruminants; 5) s o u r c e s o f t h e m i n e r a l f o r d i e t a r y s u p p le m e n ta tio n . M inerals in blood a re f i r s t d isc u sse d in term s of and the e f f e c t s o f t h e d i e t on t h e i r c o n c e n t r a t i o n . N e x t , b l o o d t e s t s t h a t c a n be u s e d t o d i a g n o s e d e f i c i e n c i e s o r t o x i c i t i e s a r e discussed. When b lood i s n o t a good i n d i c a t o r of t h e s t a t u s o f a p a r t i c u l a r m i n e r a l , a l t e r n a t i v e means of d i a g n o s i s a r e mentioned. P a r a s i t i s m i s d i s c u s s e d because v i s u a l and c l i n i c a l s i g n s of p a r a s i t e i n f e s t a t i o n c a n be c o n f u s e d w i t h m i n e r a l d e f i c i e n c i e s . The c o n t r a r y c a n a l s o o c c u r : a ttr ib u te d to parasitism . m i n e r a l d e f i c i e n c y s i g n s c a n be The d e t r i m e n t a l economic i m p l i c a t i o n s of p a r a s i t i s m in c a t t l e a re m entioned, c o n tro l are discussed. and some m e a s u r e s o f 5 M in e r a l S t a t u s o f S o i l The m i n e r a l s t a t u s o f s o i l s d e p e n d s . o n t h e i r g e o l o g i c a l form ation. The p a r e n t m a t e r i a l co m p o sitio n of the so il is p a re n t rock w eathering, the s o i l determ ined com position of the p a re n t rock. earth, of by t h e elem en tal Throughout th e h i s t o r y of the has' been s u b j e c t e d m ixing, i s r o c k so t h e tran sp o rta tio n to d isin te g ratio n , and d e p o s i t i o n . These f a c t o r s , a lo n g with c u r r e n t c l i m a t e and c ro p p r a c t i c e s , i n f l u e n c e the abundance and a v a i l a b i l i t y of m i n e r a l e le m e n t s a v a i l a b l e f o r p l a n t use (Beeson and Matrone, 1976). P l a n t growth depends on s e v e r a l e n v i r o n m e n t a l v a r i a b l e s such as t e m p e r a t u r e , m o i s t u r e s u p p l y , r a d i a n t en ergy, c om position of the atm osphere, gas c o n te n t of the s o i l , s o i l r e a c t i o n , b i o t i c f a c t o r s s u c h a s d i s e a s e s and weeds and t h e s u p p l y o f m i n e r a l n u trien t elem ents. i m p o s s i b l e t o change. some p r a c t i c e s production. Some o f these factors are d iffic u lt I n any g i v e n c l i m a t e , however, t h a t c a n be a d o p t e d or th ere are to improve a g r i c u l t u r a l I n s e v e r a l a r e a s of t h e w o r l d , s o i l f e r t i l i t y i s t h e lim itin g fa c to r for production. F e r t i l i t y i n t h e s o i l c a n be improved by s e v e r a l a g r i c u l t u r a l p r a c t i c e s such as c ro p r o t a t i o n , c o r r e c t i o n of a c i d i t y , pro per t i l l a g e , and f e r t i l i z a t i o n ( T i s d a l e and N e lson , 1975). S o i l pH and the E f f e c t o f Liming S oil production. pH i s one o f t h e m o st i m p o r t a n t factors for crop D i f f e r e n t p l a n t s p e c i e s and v a r i e t i e s have d i f f e r e n t s o i l pH r e q u i r e m e n t s , b u t most o f them t h r i v e a t pH v a l u e s c l o s e to n e u tr a l. However, p o t a t o e s grow w e l l a t pH 6.0. The growth of 6 common s c a b i n p o t a t o e s , c a u s e d by S t r e p t o m y c e s s c a b i e s , i s i n h i b i t e d when t h e s o i l pH i s 5.2 o r l o w e r ( A g r i o s , 197 8). Scab r e s i s t a n t v a r i e t i e s , however, produce b e t t e r a t a s o i l pH o f 6.5 (Warncke and C h r i s t e n s o n , 1980). In g e n e r a l , th e recommended pH fo r f i e l d c ro p s i s 6 .5 , and 6.8 fo r a l f a l f a and leg u m es (C h r iste n s o n e t a l . , 1983). In th e c a se o f mixed p a s tu r e s , i t i s o fte n d e s ir a b le to favor growth o f legu m es; c o n s e q u e n t l y a s o i l pH o f around 6.8 i s recommended. S e v e r a l m ineral i n v e s t i g a t i o n s in Latin America have shown s o i l pH v a lu e s under 6.0 (Sousa, 1978; McDowell e t a l . , 1982; Tejada, 1 98 4). In Ecuador a mean pH v a l u e o f 5.6 was found in th e s o i l o f n a tu ra l p a stu res a t a l t i t u d e s o f around 3600 m (Wilson, 1976). When s o i l pH i s n o t in th e d e s i r e d range fo r a s p e c i f i c c r o p , an amendment i s needed. Low or a c i d i c pH v a l u e s can be c o r r e c t e d w ith th e a d d i t i o n o f c a lc iu m and magnesium o x i d e s , hydroxides or carbonates. This p r a c tic e i s known as lim in g. The m ost common l im in g m a t e r i a l i s c a lc iu m c a r b o n a te or l i m e s t o n e . Other m a t e r ia ls are calciu m oxide or lim e, calcium hydroxide or sla k ed lim e , lim e sto n e s, carb on ate). sla g c a lc iu m and magnesium c a r b o n a t e s or d o l o m i t i c and m a r ls silic a te ), th e s o i l s . n e u t r a l iz e the s o i l . (Jordan e t a l . , lim e sto n e d e p o sits of c a lc iu m B y p ro d u cts o f the ir o n and phosphorus i n d u s t r y , or ( c a lc iu m n e u tr a liz e ( u n c o n s o lid a t e d a lso used when a v a i l a b l e Cement k i l n to d u s t s can be u s e d t o This l a s t byproduct has around 28% calcium 1980), (R o b ertso n n e u t r a l iz in g c a p a c ity are compared w ith 31% or more c a lc iu m in et a l., 1981a), (N oller e t a l . , and a b o u t t h e 1980). same Cement k i l n d u sts a l s o have a v a r i a b l e c o n t e n t o f p o ta s siu m , ranging from 0.40 t o 3.60% ( J o r d a n e t a l . , 1980). I n g e n e r a l , n i t r o g e n , phosp horus, p o tas siu m , s u l f u r , c a l c i u m and magnesium i n s o i l s a r e more a v a i l a b l e f o r p l a n t s a t n e u t r a l or above n e u t r a l pH v a l u e s , w h i l e aluminum, manganese, i r o n , and boron a r e more a v a i l a b l e a t a c i d pH v a l u e s . Zinc i s a v a i l a b l e up t o a pH v a l u e of around 7.0, and copper a t a l m o s t a l l pH v a l u e s , except in very a lk a lin e so ils (C hristenson et a l., 1983). Aluminum and m a n g a n e s e i n h i g h c o n c e n t r a t i o n s a r e t o x i c t o t h e p l a n t s ( T i s d a l e and N e l s o n , 19 75). so il has several ( C hristenson e t a l . , 1) lim in g advantages L iming o r n e u t r a l i z i n g t h e for improved crop p rod uction 1983), i n c l u d i n g : reduces the a v a ila b ility o f a l u m i n u m an d manganese i n t h e s o i l t o l e v e l s t h a t a r e n o t ha rmful t o crops; 2) lim in g in creases the a v a ila b ility of n itro g e n , ph osphorus, p o t a s s i u m , magnesium, c a l c i u m , s u l f u r and molybdenum; 3) l i m e s t o n e s u p p l i e s c a l c i u m t o t h e s o i l and d o l o m i t i c l i m e s t o n e s u p p l i e s c a l c i u m and magnesium; 4) l i m i n g p r o m o t e s f a v o r a b l e m i c r o b i a l a c t i v i t y which r e s u l t s i n an i n c r e a s e d a v a i l a b i l i t y o f s o i l n i t r o g e n and a d e c r e a s e d l o s s o f g aseous n i t r o g e n from t h e s o i l ; 5) lim in g prom otes b e t t e r s o i l s t r u c t u r e and t i l t h due p a r t l y t o i n c r e a s e d m i c r o b i a l a c t i v i t y , p a r t l y t o i n c r e a s e d cro p r e s i d u e s from h i g h e r c r o p y i e l d s and p a r t l y t o chem ical e f f e c t s of d e c r e a s i n g hydrogen ion c o n c e n t r a t i o n and i n c r e a s i n g c a lc iu m and magnesium io n c o n c e n t r a t i o n ; and 6) l i m i n g promotes l o n g e v i t y o f legume s t a n d s , p a r t i c u l a r l y a l f a l f a , due to the high calcium requirement of legumes. I t a lso in c r e a se s n itrogen f i x a t i o n in the r o o ts. N itrogen N i t r o g e n from t h e a i r becomes a v a i l a b l e f o r t h e p l a n t s through f i x a t i o n by R h i z o b i a or o th e r m icro o rg an ism s a tm o sp h e ric f i x a t i o n by b io c h e m ic a l r e d u c t i o n . and Nitrogen is a ls o f i x e d i n t h e form of ammonia, n i t r a t e s or cy an id es by any o f th e v a rio u s i n d u s t r i a l p ro c e s s e s fo r the m anufacture of s y n t h e t i c nitrogen f e r t i l i z e r s In the case of ( T i s d a l e and N e lso n, legum es, nitro g en 1975). fix atio n by R h i z o b i a r e p r e s e n t s t h e main s o u rc e on t h e e le m e n t f o r t h e p l a n t . in a l f a l f a c u l t i v a t i o n , used. Indeed, f o r example, no n i t r o g e n f e r t i l i z e r is To e n s u r e a good n i t r o g e n f i x i n g m i c r o b i a l p o p u l a t i o n , t h e s e e d i s i n o c u l a t e d a t t h e t i m e o f p l a n t i n g ( T e s a r , 1983). When t h e p a s t u r e s a r e mixed g r a s s e s and legumes, t h e legume p r o v i d e s the necessary n itro g e n to the p a stu re. Some a d d i t i o n a l n i t r o g e n comes from t h e manure o f t h e g r a z i n g a n im a l s . T h e r e f o r e , chem ical f e r t i l i z a t i o n w i t h n i t r o g e n i s unnecessary . There i s a l o s s o f c lo v e r from c lo v e r - g r a s s p astures h e a v i ly f e r t i l i z e d w ith n i t r o g e n . T h is i s p o s s i b l y due to c o m p e t i t i o n for moisture and n u t r ie n t s , p a r t i c u l a r l y potassium. According to Donald (1958), c lo v e r i s l o s t because of: 1) i n c r e a s e d r a t e s of n i t r o g e n a p p l i c a t i o n g i v e i n c r e a s e d y i e l d s of g r a s s ; 2) i n c r e a s e d y i e l d s of g r a s s g i v e h ig h e r l e a f a r e a s of g r a s s d i s p o s e d above t h e c l o v e r - l e a f canopy; 3) h ig h er l e a f a re a s above th e c l o v e r reduce th e l i g h t d e n s i t y a t the c l o v e r - l e a f canopy; and 4) reduced l i g h t d e n s i t y a t t h e c l o v e r l e a f canopy c a u se s reduc ed growth o f c l o v e r . In ad dition to p roviding "free" n itrogen to the so il, legumes improve t h e n u t r i t i v e q u a l i t y of t h e p a s t u r e because th e y u s u a l l y have a h i g h e r p r o t e i n c o n t e n t than g r a s s e s and a r e more palatable. Compared t o g r a s s e s , legumes have c h a r a c t e r i s t i c a l l y h igh c o n c e n t r a t i o n s o f c a l c i u m , magnesium, s u l f u r , and f r e q u e n t l y copper. They tend t o be lower i n manganese and z in c th an g r a s s e s (Church and Pond, 1974). Calcium A ll higher p la n t s re q u ire calcium . Legumes i n g e n e r a l e x t r a c t more c a l c i u m from t h e s o i l th an g r a s s e s or c e r e a l s . thousand kg o f a lfa lfa (1.40% c a l c i u m ) Nine from one h e c t a r e t o n s / a c r e ) remove 125 kg of c a l c i u m from th e s o i l . (4 Nine thousand f i v e h u n d r e d kg o f c o r n g r a i n (0,03% c a l c i u m ) from one h e c t a r e (150 b u s h e l s / a c r e ) rem ove 2.85 kg o f c a l c i u m and 10000 kg o f stover (0.30% calcium ) from t h e same crop (4.5 t o n s / a c r e ) remove 30 kg o f c a l c i u m ( R o b e r t s o n e t a l . , 1 9 7 6 a ). i s n o t a common p r o b l e m i n s o i l s . w ith calciu m s a l t s , Calcium d e f i c i e n c y N evertheless, f e r t i l i z a t i o n p a r t i c u l a r l y carbonate, is e s s e n tia l to n e u t r a l i z e t h e s o i l pH, t o m a i n t a i n a s u i t a b l e d e g r e e o f b a s e s a t u r a t i o n of t h e s o i l c o l l o i d s , and t o p r e c i p i t a t e aluminum t h a t i s t o x i c t o p l a n t s ( T i s d a l e and N e l s o n , 1975). of calcium for the so il is f e r t i l i z e r s are calcium s a l t s lim ing. Most o f The main s o u r c e the phosphate (Robertson e t a l . , 1976a). Calcium d e f i c i e n c y can occur in s o i l s in humid r e g i o n s under 10 c o n d i t i o n s i n which r a i n f a l l exceeds e v a p o t r a n s p i r a t i o n fo r most of th e year and where b a ses have been d e p l e t e d and s o i l a c i d i t y h a s d e v e l o p e d (Kamprath and F o y, 19 71). The a c t u a l l e v e l o f c a l c i u m i n s o i l i s n o t i m p o r t a n t a s l o n g t h e pH i s w i t h i n an adequa te range (Robertson e t a l . , 1976a). P l a n t s a b so r b c a lc iu m a s t h e i o n Ca++ i n b a l a n c e w i t h magnesium and p o t a s s i u m . Too much of any o f t h e s e t h r e e e le m e n t s may cause i n s u f f i c i e n c i e s of the o th er two (V itosh e t exchangeable c a lc iu m a l, 1 9 81). and p o t a s s i u m Indeed, in the the so il value is of use d t o d e t e r m i n e t h e need f o r magnesium f e r t i l i z e r ( R o b e r t s o n e t a l . , 197 6a). P l a n t a n a l y s i s c a n be u s e d t o h e l p d e t e r m i n e t h e c a l c i u m s t a tu s of the s o i l . The p e r c e n t o f c a l c i u m i n c o r n and a l f a l f a (Table 1.1, Appendix I) r e p r e s e n t s th e " s u f f i c i e n c y range", which is a le v e l reported esse n tial for high y i e l d s . L e v e l s b e lo w t h o s e im ply th e p o s s i b i l i t y of p r o d u c tio n p ro b lem s, w h ile t h o s e above r e f l e c t e x c e s s i v e l e v e l s and t h e p o s s i b i l i t y of o t h e r n u trie n t d e fic ie n c ie s. These s u f f i c i e n c y lev e ls c a n be i n t e r p r e t e d c o r r e c t l y o n l y when t h e sa m ple s a r e c o l l e c t e d in th e way i n d i c a t e d in the reference tab les. Corn s a m p l e s , for example, a r e c o l l e c t e d from t h e e a r l e a f of i n i t i a l s i l k o f the p l a n t (Robertson e t a l . , 1976a). In the c ase of a l f a l f a , the s u f f i c i e n c y range i s 1.76 t o 3.00% i n t h e top s i x i n c h e s p r i o r t o i n i t i a l flow ering. The c a l c i u m c o n t e n t o f t h e w h o l e p l a n t c u t f o r hay i n e a r l y v e g e t a t i v e s t a t e i s 1.72% (NRC, 1978). Phosphorus P hosp horus, w ith n i t r o g e n and p o t a s s iu m , i s c l a s s e d as a 11 major n u t r i e n t e le m e n t. th ese three n u trien ts S o i l s u s u a l l y r e q u ir e the a d d itio n of for comm ercial production of crops. P h o s p h o r u s d e f i c i e n c y i n s o i l s , p a s t u r e s and a n i m a l s i s one o f t h e m o st common and c r i t i c a l m i n e r a l p r o b l e m s t h r o u g h o u t t h e w o rld (Reid and H o r v a th , 1980; McDowell e t a l . , 1983). The f i r s t e f f e c t o f p h o s p h o r u s d e f i c i e n c y on t h e p l a n t i s d e c r e a s e d r o o t growth, which i n t u r n r e s u l t s i n d e c r e a s e d p l a n t growth and lower y ield s. P l a n t s w ith adequate phosphorus f e r t i l i z a t i o n m ature f a s t e r and i n t h e c a s e o f c e r e a l s h a v e g r e a t e r s t r e n g t h i n t h e stra w . P a s t u r e s i n g e n e r a l have b e t t e r n u t r i t i o n a l q u a l i t y when t h e p h o s p h o r u s s u p p l y from t h e s o i l i s a d e q u a t e ( T i s d a l e and N elson, su lfu r 1975). Phosphorus -and and p o tassium - f e r t i l i z a t i o n , w i t h o u t n i t r o g e n f e r t i l i z a t i o n , o f mixed p a s t u r e s f a v o r th e growth of legumes o v e r th e g r a s s e s . resu lts in b e t t e r n u tritio n a l q u ality : T his u s u a l l y higher p r o te in , d i g e s t i b l e e n erg y, m i n e r a l c o n c e n t r a t i o n and y i e l d (Heady, 1975). Phosphorus a v a i l a b i l i t y depends on the t o t a l con cen tratio n o f th e e le m e n t , pH, o r g a n ic m a t t e r , c l a y c o n t e n t and c l a y s t r u c t u r e , s o i l m o i s t u r e , tem p er a tu r e and a e r a t i o n in th e s o i l (Reid and H o rv a th , 1 9 80 ). su p p lie d as f e r t i l i z e r At low s o i l pH v a l u e s , phosphorus r e a c t s w ith aluminum t o form aluminum orthophosphate, which i s not a v a i l a b l e for the p la n t . so il When the i s n e u t r a l i z e d w it h lim e b e fo r e phosphorus f e r t i l i z a t i o n , aluminum i s p r e c ip it a t e d as aluminum hydroxide (Kamprath and Foy, 197 1). The a d d i t i o n o f o r g a n ic m a t e r i a l s t o m in e r a l s o i l s in c r e a se s the a v a i l a b i l i t y o f phosphorus. S o i l s con tain in g la r g e amounts o f c l a y w i l l f i x more phosphorus than t h o s e c o n t a i n i n g 12 s m a l l amounts. C l a y s of t h e 1:1 typ e r e t a i n more phosphorus than c l a y s o f t h e typ e 2:1. more p h o s p h o r u s N e l s o n , 1975). In g e n e r a l , s o i l s i n warmer c l i m a t e s f i x than s o i l s in c o ld e r clim ates ( T i s d a l e and I n c r e a s i n g s o i l m o i s t u r e and tem p era tu re i n c r e a s e t h e r a t e o f d i f f u s i o n of phosphorus t o th e r o o t system (Reid and H o r v a th , 1980). Recommendations f o r phosphorus f e r t i l i z a t i o n a r e made on the b a s is of the crop considered, organic m atter content of the s o i l , phosphorus c o n t e n t of t h e s o i l and removal of phosphorus by the c ro p (V ito sh and Warncke, 1979). T a b l e s 1.6 and 1.7 (Appendix I) show t h e recommendations f o r phosphorus f e r t i l i z a t i o n made by the E x te n s io n S e r v i c e of M ichigan S t a t e U n i v e r s i t y C hristenson, 19 80). The v alu es (Warncke and c a n be used o n l y when t h e p h o s p h o r u s c o n t e n t o f t h e s o i l h a s been o b t a i n e d by t h e B r a y - 1 e x t r a c t i n g p r o ce d u re (Knudsen, 1980). Phosphate f e r t i l i z e r s a r e m anufactur ed from phospha te rock. The b a s i c phosphate compound i n phosp hate rock i s a p a t i t e . Most of the n a t u r a l l y occurring a p a t i t e i s f l u o r o a p a t i t e or c a lc iu m p hosphate f l u o r i d e . Phosphate rock i s t r e a t e d w ith s u l f u r i c a c i d t o y i e l d o r d i n a r y s u p e r p h o sp h a te w ith 7-9.5% a v a i l a b l e phosphorus and 8-10% s u l f u r a s c a l c i u m s u l f a t e . T r i p l e or c o n c e n tr a te d s u p e r p h o s p h a t e i s m a n u f a c t u r e d by t r e a t i n g p h o s p h a t e r o c k w i t h phosphoric a cid , p h o sp h ates and c o n t a i n s 19 t o 23% phosphorus. a v a ila b le superphosphates, in th e m arket are ammonium p h o s p h a t e s and n i t r i c Among o t h e r am m oniated phosphates. D e f l u o r i n a t e d p h o sp h a te s a r e m a n u f a c t u r e d by h e a t t r e a t m e n t o f phosphate rock, and a r e u s e d f o r anim al feeds ( T i s d a l e and 13 Nelson, 1975). Potassium Potassium i s one o f th e most abundant e le m e n t s i n th e s o i l , b u t t h e f r a c t i o n o f t h e t o t a l p o ta s s iu m i n t h e e x c h a n g e a b le , or p l a n t a v a i l a b l e , form i s u s u a l l y s m a l l . p otassium are high. P l a n t r e q u ir e m e n ts f o r When t h e e l e m e n t i s i n s h o r t s u p p l y , t h e f i r s t symptom i s a r e d u c t i o n i n y i e l d s and t h e q u a l i t y o f t h e crops. There i s a weakening o f t h e st r a w of c e r e a l s and g r a s s e s t h a t a r e th en s u b j e c t t o l o d g i n g , and s t a l k breakage in c orn and sorghum. A u s u a l symptom i n a l f a l f a i s t h e d e c o l o r i z a t i o n of th e lower l e a v e s . This i s because p o tassiu m i s a m obile elem ent which i s t r a n s l o c a t e d t o t h e y o u n g e r m e r i s t e m a t i c t i s s u e s i f a shortage p otassium . occurs. P lan ts d iffer in t h e i r a b ility to use G ra sses a r e b e t t e r a b l e t o s u r v i v e a t low l e v e l s of s o i l p o tassiu m th an c l o v e r s and legumes i n g e n e r a l . T h e r e fo r e t o m a i n t a i n a good legume p o p u l a t i o n i n mixed g r a s s - l e g u m e p a s t u r e s and meadows, i t i s i m p o r t a n t t o p r o v i d e an a d e q u a t e p o t a s s i u m f e r t i l i z a t i o n ( T i s d a l e and N e lso n , 1975). Potassium i n th e s o i l e x i s t s i n fo ur forms: 1) m i n e r a l , or t h e po tassiu m h e l d i n t h e m o l e c u l e s o f f e l d s p a r and mica, which i s u n a v a i l a b l e t o t h e p l a n t ; 2) " d i f f i c u l t l y a v a i l a b l e " , or the p o t a s s i u m i n c l a y s l i k e i l l i t e , v e r m i c u l i t e , and c h l o r i t e ; 3) e x c h a n g e a b l e p o t a s s i u m , h e l d by e l e c t r o s t a t i c f o r c e s , which i s v e r y r e a d i l y e x c h a n g e d from t h e s o l i d p h a s e o f t h e s o l u t i o n by o t h e r c a t i o n s ; and 4) so il to p otassium i n s o l u t i o n , a s the K+ i o n , which i s t h e fo rm t h a t i s a b s o r b e d by t h e r o o t s ( B a rb e r e t a l . , 1971). 14 Potassium a d d ed to the so il as fertiliz er is read ily a v a i l a b l e t o t h e p l a n t a t t h e time o f a p p l i c a t i o n , b u t a f t e r some time t h e p r o c e s s o f " f i x a t i o n " o c c u r s . This i s t h e entra pment of t h e p o t a s s i u m i o n i n b e tw e e n t h e l a y e r s o f 2: 1 t y p e c l a y s . fix e d elem en t i s u n a v a i l a b l e to the p l a n t . The The f a c t o r s t h a t i n f l u e n c e t h e c o n v e r s i o n o f s o i l and ad ded p o t a s s i u m t o l e s s a v a i l a b l e forms a r e t h e f o l l o w i n g ( T i s d a l e and N e lso n , 1975): 1) Type and amount o f c o l l o i d s : more p otas sium th an t h e 1:1 t y p e s . c l a y s o f t h e 2:1 ty pe f i x Independent of the c l a y ty p e , s o i l s w i t h a h i g h e r p e r c e n t a g e o f c l a y w i l l f i x more p o t a s s i u m than sandy s o i l s . 2) T em p eratu re: th ere is ev id en ce t h a t changes in te m p e r a t u r e , such as f r e e z i n g an thawing have some e f f e c t on t h e r e l e a s e of fix ed potassium . The same e f f e c t h a s b een o b s e r v e d with w e t t i n g and d r y i n g o f t h e s o i l . 3) S o i l pH: t h e e f f e c t o f s o i l pH p e r s e on p o t a s s i u m f i x a t i o n i s n o t known. Lim ing o f s o i l s w i t h c l a y s t h a t a r e s a t u r a t e d w ith p o tassiu m r e l e a s e s the p otassium to the s o i l s o l u t i o n by s u b s t i t u t i o n . P o t a s s i u m f e r t i l i z e r added t o s o i l s w i t h c a l c i u m io n s a d sorbed t o t h e c l a y i n t e r c h a n g e s c a l c i u m fo r p o tassiu m on t h e s u r f a c e o f t h e c l a y p a r t i c l e . s t i l l ex ch a n g ea b le . T his p otas sium i s F i x a t i o n of th e exch a n g ea b le po tas sium w i l l depend on t h e amount and typ e of c l a y and t h e degree of po tassium saturation. Potassium f e r t i l i z a t i o n r e c o m m e n d a t i o n s a r e made on t h e b a s i s o f: 1) t h e amount o f t h e e l e m e n t rem oved from t h e s o i l by t h e 1.5 c ro p. Corn s i l a g e remove (56 m e t r i c t o n s / h e c t a r e or 25 t o n s / a c r e ) w i l l 220 kg o f K20 f r o m t h e so il. A lfalfa (11 m e t r i c t o n s / h e c t a r e o r 5 t o n s / a c r e ) w i l l rem ove 250 kg o f K20 from t h e soil (Warncke and C h r i s t e n s o n , 1980). 2) t h e e x c h a n g e a b le amount o f p o tassiu m p r e s e n t i n t h e s o i l as determined by c h em ic al a n a l y s i s ; and 3) the te x t u r e of th e s o i l . Sandy s o i l s require less potassium than s o i l s t h a t have high c o n t e n t s of c l a y . When enough p o t a s s i u m f e r t i l i z e r i s ad ded t o t h e s o i l i t w i l l e v e n t u a l l y s a t u r a t e the c l a y p a r t i c l e s . A l l the e x tr a p o t a s s i u m w i l l t h e n be i n an e x c h a n g e a b l e form t h a t w i l l n o t r e v e r t t o th e f i x e d form. I n some s i t u a t i o n s i t i s d e s i r a b l e to b u i l d up t h e p o t a s s i u m c o n c e n t r a t i o n i n t h e s o i l t o t h e p o i n t of satu ratio n . However , i n s o i l s w i t h h i g h c o n t e n t o f 2:1 t y p e of c l a y , t h e amount needed t o r e a c h s a t u r a t i o n can be so g r e a t i t i s n o t economical t o do so. s o i l more f r e q u e n t l y I n such a c a s e , adding potassium t o the is recommended, not in order to reach s a t u r a t i o n , b u t t o h a v e eno ugh e x c h a n g e a b l e e l e m e n t d u r i n g t h e p e rio d of growth. planting. F o r c o r n , p o t a s s i u m i s ad ded a t t h e t i m e o f I n t h e c a s e o f permanent c ro p s as a l f a l f a , po tassiu m c a n be added a f t e r t h e f i r s t h a r v e s t i n s p r i n g , and a f t e r t h e t h i r d h a r v e s t i n l a t e automn i n M i c h i g a n ( H e l s e l e t a l . , 1984). Recommendations f o r p o t a s s i u m f e r t i l i z a t i o n f o r corn and a l f a l f a made by t h e E x t e n s i o n S e r v i c e o f M i c h i g a n S t a t e U n i v e r s i t y (Warncke and C h r i s t e n s o n , 1980) a r e shown i n T a b l e s 1.6 and 1.7 (Appendix 1) . The main p o t a s s i u m f e r t i l i z e r i s p otassium c h l o r i d e found in 16 u n d e r g r o u n d d e p o s i t s and i n t h e b r i n e s o f d y i n g s e a s and l a k e s . The p otas siu m o r e and the b r i n e s a r e found u s u a l l y as m ix t u r e s of potassium c h lo r id e , sodium c h l o r i d e , other sa lts and c l a y . R e f i n i n g p r o c e s s e s a r e n e c e s s a r y t o o b t a i n c o n c e n t r a t e d or pure p o ta s s iu m c h l o r i d e . Other p o ta s s iu m f e r t i l i z e r s a r e p o ta s s iu m s u l f a t e , p o tas siu m magnesium s u l f a t e , and p o ta s s iu m n i t r a t e . Magnesium The t o t a l magnesium c o n t e n t o f s o i l s i s u s u a l l y h i g h , b u t r a n g e s from 0.1% i n h i g h l y we athe re d , sandy t r o p i c a l s o i l s , t o 4% i n s o i l s of s e m ia r id r e g i o n s (Mortvedt and Cunningham, 1971). As i n t h e c a s e o f p o t a s s i u m , n o t a l l t h e magnesium i n t h e s o i l i s a v a i l a b l e f o r the p l a n t . Magnesium i s absorbed by th e p l a n t s as th e ion Mg++ from th e s o il solution. I t i s adsorbed and f i x e d by t h e c l a y p a r t i c l e s in a way s i m i l a r to t h a t of potassium . The amount o f magnesium abso rbed by t h e p l a n t s depends on t h e amount p r e s e n t , t h e degre e o f s a t u r a t i o n , and the n a t u r e of o t h e r e x c h a n g e a b le io n s ( T i s d a l e and N e l s o n , 1975 ). The M i c h i g a n S t a t e U n i v e r s i t y E x t e n s i o n S e r v i c e (Vitosh e t a l . , 1981) recommends magnesium f e r t i l i z a t i o n i f one o f t h e f o l l o w i n g c r i t e r i a a r e met: 1) t h e e x ch an g eab le magnesium l e v e l i s l e s s than 37 ppm i n m i n e r a l s o i l s and 75 ppm i n o r g a n i c s o i l s ; or 2) when as a p e r c e n t o f t h e t o t a l b a ses (Ca + Mg + K, e x p r e s s e d a s m i l l i e q u i v a l e n t s p e r u n i t o f w e i g h t o f so il), potassium lev e ls e x c e e d magnesium ; o r 3) when s o i l m agnesi um , a s a p e r c e n t o f t h e t o t a l b a s e s , i s l e s s t h a n t h r e e percent. Some a u t h o r s recommend a t l e a s t 10% o f magnesium a s p e r c e n t of the t o t a l b a se s t o p r e v e n t magnesium t e t a n y of a n im a l s 17 f e d magnesium d e f i c i e n t f o r a g e s . S u f f i c i e n c y r a n g e s shown i n t a b l e 1.1 (Appendix I) can be used t o a s s e s s magnesium d e f i c i e n c y i n c o rn and a l f a l f a . Magnesium i s a m o b il e e le m e n t and i s r e a d i l y t r a n s l o c a t e d from o l d e r t o y o u n g e r p l a n t p a r t s i n t h e e v e n t o f d e f i c i e n c y . C o n s e q u e n t l y , symptoms o f t e n a p p e a r f i r s t on t h e l o w e r l e a v e s . I n many s p e c i e s , such as c o rn , the d e fic ie n c y r e s u l t s i n an i n t e r v e i n a l c h l o r o s i s of t h e l e a f , i n which o n l y the v e i n s remain green. I n more advanced s t a g e s t h e l e a f t i s s u e becomes u n if o r m ly p a l e y e l l o w , t h e n brown and n e c r o t i c ( T i s d a l e and N e l s o n , 1975). M agnesium d e ficie n cy can be induced by high potassium f e r t i l i z a t i o n and in a d e q u a t e lim i n g (Vitosh e t a l . , 1981). To c o r r e c t or prevent d eficien cies, a good source of magnesium i s d o l o m i t i c l i m e s t o n e which h a s v a r i a b l e magnesium co n ten ts. This lim e sto n e to m aterial can lim e a c id s o i l s . be used instead When a l k a l i n e of c alcitic so ils need magnesium, s a l t s such a s potassium-magnesium s u l f a t e can be used ( T i s d a l e and N e l s o n , 1975). Sulfur S u l f u r i s a b s o r b e d by t h e r o o t s a l m o s t e x c l u s i v e l y a s t h e su lfate ion, SO4 — • The symptoms o f s u l f u r s im il a r to those of n itro g e n d e fic ie n c y : d e fic ie n cy are uniform c h l o r o s i s of t h e l e a v e s , d e c r e a s e d g r o w t h and g e n e r a l w e a k n e s s o f t h e p l a n t ( T i s d a l e and N e l s o n , 1975). S u l f u r has s e v e r a l f u n c t i o n s i n p l a n t s , among them ( T is d a l e and N e lson , 1975): 1) i t i s re q u ir e d for the s y n t h e s i s of s u l f u r c o n ta in in g 18 amino a c i d s , and f o r p r o t e i n s y n t h e s i s ; 2) i t a c t i v a t e s s e v e r a l enzymes and i t i s a c o n s t i t u e n t of some v i t a m i n s and enzymes; 3) i t i s p r e s e n t i n t h e o i l s o f some p l a n t s a s g a r l i c and o nions and i n c r e a s e s t h e o i l c o n t e n t of p l a n t s l i k e soybeans and flax; 4) it is required for nitro g en fix atio n by l e g u m i n o u s p l a n t s and i s a p a r t o f t h e n i t r o g e n a s e enzyme s y s t e m t h a t i s a s s o c ia te d with t h i s r e a c t i o n . S u lf u r i s a l s o a s s o c ia te d with co ld re s is ta n c e in p l a n t s . The m ost d i r e c t b e n e f i t o f s u l f u r f e r t i l i z a t i o n i n s u l f u r d e f i c i e n t s o i l s i s t h e i n c r e a s e i n y i e l d and q u a l i t y o f t h e crop. I n c r e a s e d p e r s i s t e n c y , w i n t e r h a r d i n e s s and d r o u g h t t o l e r a n c e has been o b se r v e d i n a l f a l f a a f t e r s u l f u r f e r t i l i z a t i o n Fox, 1971). In cereals and g r a s s e s su lfu r (Beaton and fertiliz atio n d e c r e a s e s t h e a c c u m u l a t i o n o f n i t r a t e s , t h a t may be h a r m f u l t o rum in ants . On t h e o t h e r hand, an i n c r e a s e d s u l f u r c o n t e n t i n the p l a n t a f t e r f e r t i l i z a t i o n decreases the nitro g en to s u l f u r r a t i o ( T i s d a l e and N e l s o n , 1 9 75 ). A n i t r o g e n t o s u l f u r r a t i o o f 10 :1 is suggested for e f f i c i e n t u t i l i z a t i o n of n o nprotein n itro g e n (NRC, 1978). G ra s s e s u t i l i z e s o i l s u l f u r b e t t e r than legumes. In g r a s s - le g u m e p a s t u r e s t h e g r a s s e s can a b s o r b th e a v a i l a b l e s u l f a t e a t a f a s t e r r a t e than th e legumes. so il l e v e l of t h i s elem ent is m ain tain ed , U n l e s s an a d e q u a t e th e legumes w i l l d i s a p p e a r from the m i x t u r e ( T i s d a l e and N e l s o n , 1975). A s o i l t e s t l e v e l o f 6 - 7 ppm o f s u l f u r i s c o n s i d e r e d t h e t h r e s h o l d t o d i a g n o s e d e f i c i e n c y in the G r e a t Lakes a r e a . Some 1.9 s o i l s i n M i c h i g a n h a v e s u l f u r c o n c e n t r a t i o n s b e l o w 6 ppm, b u t s u l f u r f e r t i l i z a t i o n has f a i l e d t o i n c r e a s e c ro p y i e l d s w i t h the exception of field beans (R obertson e t a l., 1 9 76 b ). It is p o s s i b l e t h a t c o n ti n u o u s c ropping of high y i e l d i n g v a r i e t i e s w i l l e v e n t u a l l y d e p l e t e t h e a v a i l a b l e s u l f u r i n some s o i l s and th en f e r t i l i z a t i o n w i l l be needed. There a re s e v e r a l s u l f u r c o n ta in in g market. f e r t i l i z e r s on t h e Most o f them a r e s u l f a t e s o f d i f f e r e n t c a t i o n s , and a r e r e a d i l y a v a i l a b l e to the p l a n t . With t h e e x c e p t i o n of ammonium, aluminum, and i r o n s u l f a t e s , s u l f a t e s a l t s have no e f f e c t on s o i l pH. E le m e n t a l s u l f u r i s a good s u l f u r f e r t i l i z e r , b u t needs t o be o x i d i z e d t o s u l f a t e b e f o r e b e i n g a b s o r b e d by t h e r o o t s . v e l o c i t y o f o x i d a t i o n d e p e n d s on t h e p a r t i c l e te m p e r a t u re and m o i s t u r e of t h e s o i l . the so il. Three kg o f c a l c i u m The s i z e and t h e Elemental s u l f u r a c i d i f i e s carbonate are necessary to n e u t r a l i z e one k ilo g r a m o f e l e m e n t a l s u l f u r ( T i s d a l e and N e lso n, 1975). Calcium s u l f a t e or gypsum (around 16% s u l f u r ) , if finely ground w i l l u s u a l l y pro d u ce a q u ic k r e s p o n s e w ith most c ro p s . The same i s t r u e f o r n o r m a l s u p e r p h o s p h a t e t h a t h a s 10-12% o f s u l f u r c o n t e n t (Beaton and Fox, 1971). Sodium Sodium i s e s s e n t i a l f o r t h e g r o w t h o f p l a n t s . c ro p s have d i f f e r e n t r e q u ir e m e n ts f o r t h e e le m e n t. D ifferent The respo n se o f c r o p s t o sodium f e r t i l i z a t i o n i s u s u a l l y d e p e n d e n t on t h e potassium s t a t u s of the s o i l . W h ea t, f o r e x a m p l e , w i l l show i n c r e a s e d y i e l d s i n r e s p o n se t o sodium f e r t i l i z a t i o n i f po tas si um i s low i n t h e s o i l , b u t n o t when p o t a s s i u m i s a d e q u a t e . When 20 sodium n i t r a t e i s u s e d a s a s o u r c e o f n i t r o g e n , t h e sodium i o n h e l p s t o m a i n t a i n t h e pH o f t h e s o i l a t a s u i t a b l e high l e v e l , in c o n t r a s t t o ammonium s o u r c e s whose c o n ti n u o u s use lo wers the s o i l pH. Sodium d i s p e r s e s b o t h c l a y and o r g a n i c m a t t e r . For t h i s r e a s o n , l a r g e q u a n t i t i e s o f sod iu m i n f i n e t e x t u r e d s o i l s a r e undesirable. so il, I n s e m i a r i d r e g i o n s , so dium a c c u m u l a t e s i n t h e i n some c a s e s t o a p o i n t w here p l a n t g r o w t h i s l i m i t e d . Amendment o f t h e s o i l w ith gypsum and s u f f i c i e n t water t o l e a c h o u t t h e d i s p l a c e d so d iu m c a n a l l e v i a t e t h i s c o n d i t i o n ( T is d a l e and N e l s o n , 1975). I n s e v e r a l a r i d and s e m i a r i d r e g i o n s o f t h e w o r l d , t h e p r o b l e m i s n o t o n l y so d i u m , b u t t h e a c c u m u l a t i o n o f to ta l soluble s a lts . This phenomenon i s known as s a l i n i t y of the soil 1982). (Bresler e t a l . , C h l o r in e I t has been d e m o s tr a te d t h a t c h l o r i n e i s e s s e n t i a l f o r p l a n t growth in s e v e r a l s p e c i e s . D e f i c i e n c y o f t h e c h l o r i d e i o n can produce c h l o r o s i s in some a r e a s of t h e p l a n t in some s p e c i e s , and leaf bronzing in o th e r s . In tom ato p l a n t s , c h l o r i n e d e f i c i e n c y i s d e c r e a s e d r o o t growth. the e f f e c t of Corn i s one of the c r o p s s u s c e p t i b l e t o c h l o r i n e d e f i c i e n c y ( T i s d a l e and N e l s o n , 1975). The c h l o r i d e i o n i s h i g h l y s o l u b l e i n w a t e r and l o o s l y h e l d by t h e c l a y p a r t i c l e s , so i t i s e a s i l y l e a c h e d from t h e s u r f a c e h o r i z o n o f s o i l s a f t e r i r r i g a t i o n or r a i n f a l l . fertiliz atio n with potassium m u ria te should Potassium provide enough c h l o r i n e f o r the c r o p s (Mortvedt and Cunningham, 1971). Boron Boron i s indispen sab le for p l a n t s but not for an im als. 21 A l f a l f a i s a c ro p h i g h l y r e s p o n s i v e t o boron f e r t i l i z a t i o n , w h i l e clo v ers a r e medium r e s p o n s i v e and c o r n and g r a s s e s a r e r e s p o n s i v e (Robertson e t a l . , In a lfa lfa , low 1981a). boron d e f i c i e n c y produces a y ello w ish to r e d d i s h - y e l l o w d i s c o l o r a t i o n o f t h e upper l e a v e s , s h o r t nodes and few f l o w e r s . Growing t i p s o f a l f a l f a may d i e , w i t h r e g r o w t h coming a f t e r a new s h o o t i s i n i t i a t e d a t a l o w e r a x i s . Boron d e f i c i e n c y and l e a f h o p p e r damage c a n be c o n f u s e d i n a l f a l f a . L e a f h o p p e r damage shows up a s a V-shaped y e llo w in g of the a f f e c t e d l e a v e s and may appear on any o r a l l p a r t s of t h e p l a n t . The g r o w in g t i p i s u s u a l l y n o r m a l and t h e p l a n t may s u p p o r t abundant flo w e rs . O f t e n , when t h e s o i l i s d r y and p l a n t g r o w t h i s r e t a r d e d , both boron d e f i c i e n c y and l e a f h o p p e r i n j u r y oc cur in t h e same f i e l d . A c u t e b o r o n d e f i c i e n c y i n c o r n a p p e a r s on t h e newly-formed l e a v e s as e l o n g a t e d , w a te r y or t r a n s p a r e n t s t r i p e s . L a t e r , th e l e a v e s become w h ite and d i e . Growing p o i n t s a l s o d i e and, i n s e v e r e c a s e s , s t e r i l i t y i s common. I f e a r s d e v e l o p , they may show corky brown bands a t th e base of the k e r n e l s (Vitosh e t a l . , 1981). In a d d itio n to v isu al diagnosed by s o i l t e s t s . the s o i l sym ptom s, boron s t a t u s c a n be A c o n c e n t r a t i o n o f l e s s th a n 1 ppm when i s e x t r a c t e d w i t h b o i l i n g w a t e r i s an i n d i c a t i o n o f boron d e f i c i e n c y in t h e s o i l . C o r r e l a t i o n s of y i e l d r e s p o n s e s t o boron f e r t i l i z a t i o n based on s o i l t e s t s , however, have been low. P l a n t a n a l y s i s can a l s o be used t o a s s e s s boron d e f i c i e n c i e s or to x icities. The s u f f i c i e n c y r a n g e f o r a l f a l f a ( t o p s i x i n c h e s p r i o r t o i n i t i a l bloom) i s 31-80 ppm. For c o r n , t h e s u f f i c i e n c y 22 range measured in (Robertson e t a l . , the ear leaf at first silk is 4 - 2 5 ppm 1981a). Boron a v a i l a b i l i t y in the s o i l i s g reater when the tex tu re i s sandy than when th e p r o p o r t io n o f c l a y i s h ig h . reduces the a v a i l a b i l i t y o f boron. O v e r lim in g Boron d e f i c i e n c i e s are more m a n i f e s t when th e s o i l i s dry and th e p l a n t can n o t e x t r a c t th e elem ent from i t (T isd a le and N elso n , 1975). T h e r e a r e s e v e r a l compounds and p r e p a r a t i o n s t h a t c a n be used as f e r t i l i z e r to c o r r e c t or p r e v e n t boron d e f i c i e n c i e s . Some of them a r e b o rax, sodium p e n t a b o r a t e and b o r i c a c i d . Boron s a l t s c a n be f u s e d w i t h g l a s s t o p r o d u c e a s l o w r e l e a s e o f t h e s a l t as th e g l a s s d i s s o l v e s . T his m a t e r i a l i s c a l l e d " f r i t " ( T i s d a l e and N e l s o n , 1975). B oron t o x i c i t y u s u a l l y o c c u r s when b o r o n c o n t a i n i n g f e r t i l i z e r s for h ig h ly r e s p o n s iv e s p e c i e s l i k e sugar b e e t s are used a t p la n tin g time f e r t i l i z e r for h ig h ly s e n s i t i v e crops such a s f i e l d b ea n s. T o x i c i t y i s c h a r a c t e r i z e d by y e l l o w i n g o f th e l e a f t i p , i n t e r v e i n a l c h l o r o s i s , and p r o g r e s s iv e scorching o f the l e a f margin (Vitosh e t a l . , 1981). For a l f a l f a , e s p e c i a l l y when grown on c o a r s e t e x t u r e d , a r id s o i l s , boron s h o u ld be a p p l i e d a n n u a lly , but not a t seed in g , at a r a te o f one to two kg/h ectare (H else l e t a l . , 1984). Iron A p l a n t r e q u ir e s a continuous supply of iro n to m ain tain p r o p e r growth (Brown e t a l . , 1972). Iron d eficien cy in s o i l s is r e l a t e d t o high pH v a l u e s such as t h o s e found i n a r i d , c a l c a r e o u s r e g i o n s , a c i d s o i l s w i t h low t o t a l i r o n c o n t e n t , and h i g h s o i l c o n c e n t r a t i o n s o f p h o s p h o r u s ( M o r t v e d t and Cunningham , 1971). I r o n a b s o r p t i o n by t h e p l a n t i s reduced by high c o n c e n t r a t i o n s of manganese, phosphorus and heavy m e t a l s in th e s o i l . highly responsive to iron f e r t i l i z a t i o n , and c o r n a r e medium r e s p o n s i v e G ra sses a r e while a l f a l f a , (Robertson e t a l . , clover 198 1a). M i c h i g a n , i r o n d e f i c i e n c y i s n o t common i n f o r a g e s , In b u t some problems have been o b s e r v e d i n t r e e s , o r n a m e n t a l s and g o l f lawns ( V i t o s h e t a l . , 19 71). S o i l t e s t s h a v e n o t b e e n a good i n d i c a t o r o f e x t r a c t a b l e i r o n ( R o b e r t s o n e t a l . , 1 9 8 1 a , Cox and K a m p ra t h , 1972). Plant a n a l y s i s i s a l s o d i f f i c u l t t o i n t e r p r e t , b u t can be used t o h e l p d i a g n o s e t o x i c i t i e s o r d e f i c i e n c i e s when t h e v a l u e s a r e w e l l above or b e lo w (Appendix I) the su fficien cy (Robertson e t a l . , ranges shown in tab le 1 .2 1981a). V isu a l d e f ic ie n c y symptoms in p la n t s are marked, and show up f i r s t in the young l e a v e s . I n t e r v e i n a l c h l o r o s i s d e v e lo p s f i r s t , and progresses r a p id ly over the e n t i r e l e a f . In se v e r e ca ses the l e a v e s tu rn c o m p l e t e l y w h ite ( T i s d a l e and N e l s o n , 1975). d e fic ie n c y symptoms are v e r y s i m i l a r d e f ic ie n c y (Vitosh e t a l . , Iron t o t h o s e o f manganese 1981). F e r r o u s s u l f a t e i s t h e m o st commonly u s e d s a l t t o c o r r e c t iron deficien cies. I t can be p u t i n t h e s o i l or used as a sp ra y . Among o t h e r i r o n s o u r c e s a r e f e r r i c s u l f a t e , oxide, iron f r i t s . f e r r o u s and f e r r i c I r o n c h e l a t e s (FeEDDHA, FeDTPA and FeEDTA) a r e e f f e c t i v e so u r c e s of i r o n under some c o n d i t i o n s (Mortvedt and Cunningham, 197 1). Under a l k a l i n e sp r a y s a r e recommended (V ito sh e t a l . , s o il con d itio n s, 1981). fo liag e 24 Manganese According to the E xtension S ervice of M ichigan S tate U n i v e r s i t y , manganese i s t h e most common m i c r o n u t r i e n t prob lem i n Michigan s o i l s (Vitosh e t a l . , 1981). P l a n t s r e q u i r e manganese i n s m a l l q u a n t i t i e s ; l a r g e amounts a r e t o x i c ( T i s d a l e and N e l s o n , 1975 ). Manganese d e f i c i e n c y o c c u r s more o f t e n on w e l l - d r a i n e d s o i l s w ith a n e u t r a l or c a l c a r e o u s r e a c t i o n . H o w ev e r, o r g a n i c s o i l s and some m i n e r a l s o i l s w i t h l a r g e q u a n t i t i e s o f o r g a n i c m a t t e r may e x h i b i t symptoms o f d e f i c i e n c y w i t h a s l i g h t l y a c i d pH (Murphy and W a l s h , 197 2). A c id s o i l s w hic h h a v e b e e n l i m e d a r e more l i k e l y t o be manganese d e f i c i e n t th a n n a t u r a l l y n e u t r a l or a l k a l i n e s o i l s ( V i t o s h e t a l . , 1 9 81 ). The m i n e r a l s mag nesi um, and e s p e c i a l l y c a l c i u m i n t e r f e r e w ith manganese a b s o r p t i o n by t h e roots. I r o n ++, b u t n o t i r o n +++, a l s o d e c r e a s e s t h e a b s o r p t i o n of manganese (Moore, 1972). Calcium and magnesium io n s n o t o n l y can p r o d u c e m anganese d e f i c i e n c y by c o m p e t i n g f o r a b s o r p t i o n , b u t a l s o by r a i s i n g t h e s o i l pH. M a n g a n e s e 4"1" i s t h e p r e d o m i n a n t sp ecies in the s o i l s o lu t io n . T h is ion i s v e r y s o l u b l e a t pH 4, b u t w i t h each u n i t i n c r e a s e i n pH, i t s fold (Lindsay, s o l u b i l i t y d e c r e a s e s 100 1972). The s u f f i c i e n c y range fo r m anganese in corn (ear l e a f j u s t b efore s ilk in g ) i s 20-150 ppm, and f o r a l f a l f a (top g r o w th -6 in c h e s t o f l o w e r i n g ) i s 30-10 0 ppm (R ob ertson and L u cas, 1981). In th e p l a n t , manganese i s a r e l a t i v e l y im m obile e le m e n t . symptoms o f d e f ic ie n c y u s u a l l y appear in the younger l e a v e s . The In broad-leaved p la n t s the symptom i n t e r v e i n a l c h l o r o s i s , which a l s o occurs le ss co n sp icu o u sly , i n members o f th e g r a s s fa m ily 25 ( T i s d a l e and N e l s o n , 1 9 75 ). Corn p l a n t s do n o t show marked symptoms, b u t when c om pared w i t h a n o r m a l l e a f , t h e d e f i c i e n t l e a f i s l i g h t e r g ree n and has p a r a l l e l , y e l l o w i s h s t r i p e s (Vitosh e t a l . , 1981). Mangan ese e x c e s s e s o r t o x i c i t y commonly occur in s t r o n g l y a c i d or i n w a t e r l o g g e d s o i l s (Murphy and Walsh, 1972). of manganese t o x i c i t y a r e n o t v e ry s p e c i f i c . f o l l o w e d by n e c r o s i s o f l e a v e s , leaf Severe c h l o r o s i s s p o t s on m a r g i n s , s t u n t i n g o f t h e p l a n t a r e t h e u s u a l symptoms. co n cen tratio n s in p lan ts elem ents, e s p e c i a l l y iron. may i n d u c e Symptoms and High m anga nes e d eficien cies of other Reduction i n t h e number of n o d u l e s on w h i t e c l o v e r r o o t s due t o e x c e s s m a n g a n es e h a s b e e n r e p o r t e d (Mortvedt and Cunningham, 1971). M ang an ese s u l f a t e fertiliz er. is t h e m o st commonly u s e d m an g a n ese O t h e r s o u r c e s o f m an g a n ese a r e o x i d e s , c h l o r i d e s , carbonates, c h e la te s N e l s o n , 1975). (EDTA), and m a n g a n es e f r i t s ( T i s d a l e and I n M i c h i g a n , m ang an ese s u l f a t e and manganous o x i d e h a v e b een e f f e c t i v e t o c o r r e c t d e f i c i e n c i e s . M a n g an ic o xid e i s i n s o l u b l e and has pro v ed t o be i n e f f e c t i v e f o r Michigan so ils. C h e l a t e d m an ga nes e m a t e r i a l s i n g e n e r a l h a v e n o t been s a t i s f a c t o r y on o r g a n i c s o i l s and have been l e s s e f f e c t i v e th an m ang a nes e su lfate on m i n e r a l so ils (V itosh et a l., 1981). Manganese t o x i c i t y i n a c i d s o i l s can be c o r r e c t e d by lim in g t o a pH c l o s e t o n e u t r a l (Lindsay, 1972). When a s o i l m an g an ese t e s t i s a v a i l a b l e a f t e r e x t r a c t i o n w i t h 0.1 N HC1, f e r t i l i z e r c a n be a p p l i e d a t t h e r a t e s shown i n t a b l e 1.8 (Appendix I ) . B r o a d c a s t a p p l i c a t i o n i s n o t recommended 26 b e c a u se o f h ig h f i x a t i o n o f manganese in the s o i l . R e s id u a l carryover o f a v a i l a b l e manganese f e r t i l i z e r i s u s u a l l y low. For t h i s reason, manganese must be a p p lie d every year on a d e f i c i e n t s o i l (Vitosh e t a l , 1981). A l f a l f a , c l o v e r , corn and g r a sse s are crops medium r e sp o n s iv e to manganese f e r t i l i z a t i o n (Robertson and Lucas, 1 98 1 a ). Selenium This e le m e n t i s a p p a r e n t l y n o t needed by p l a n t s , b u t must be present in anim als. forages There a re and c r o p p l a n t s several since is e ssen tial for r e g i o n s i n t h e w o r l d where t h e a v a i l a b l e s e le n iu m l e v e l s in s o i l s a re s u f f i c i e n t l y high to produce f o r a g e s c o n t a i n i n g l e v e l s of t h i s ele m e n t t h a t a r e t o x i c to anim als. T h e r e a r e o t h e r a r e a s t h a t p r o d u c e p l a n t s t h a t do not c o n t a i n enough s e l e n i u m t o meet t h e n u t r i t i o n a l re qu ire m e n ts of anim als (Kubota and A l l o w a y , 197 2). The a v a i l a b i l i t y o f s e l e n i u m t o p l a n t s i s c l o s e l y r e l a t e d t o t h e q u a n t i t y of w a t e r s o lu b le selenium p re s e n t in the s o i l . Selenium a v a i l a b i l i t y i s h ig h er in a l k a l i n e s o i l s where t h e s e l e n a t e s predominate than i n n e u t r a l - t o - s l i g h t l y acid s o i l s . Liming g e n e r a l l y r e s u l t s i n slow r e l e a s e of s e l e n i t e s from t h e i r i r o n complexes and p e rm i ts t h e i r o x id a tio n to th e w ater s o l u b l e s e l e n a t e 197 6). (Beeson and M a t r o n e , The i d e n t i f i c a t i o n and mapping o f s e l e n i u m d e f i c i e n t a r e a s and a r e a s w i t h e x c e s s i v e l e v e l s o f se len iu m has been made on t h e b a s i s o f t h e s e l e n i u m c o n c e n t r a t i o n o f c r o p s grown on th o se s o i l s (Kubota and A llaw ay , 1972). t h i s s u r v e y w ere a l f a l f a p l a n t s . Most of t h e samples fo r A r e a s where more t h a n 80% o f t h e p l a n t s a m p l e s c o n t a i n e d l e s s t h a n 0.05 ppm s e l e n i u m a r e 27 c o n s i d e r e d low i n s e l e n i u m . When more t h a n 80% o f t h e s a m p l e s c o n t a i n e d more t h a n 0 .1 ppm s e l e n i u m , t h e a r e a i s c o n s i d e r e d adequate i n selen iu m . The s t a t e of Michigan has been i d e n t i f i e d as a s e le n iu m d e f i c i e n t a r e a (Kubota and A lla w a y , 1972). In t h e same s o i l , some p l a n t s can a b so r b and accumulate more selen iu m than o t h e r s . E v e n i n s e l e n i f e r o u s s o i l s , c l o v e r and some g r a s s e s do n o t a c c u m u l a t e s e l e n i u m t o l e v e l s t o x i c t o t h e an im als. C e r e a l s , some a s t e r s , and s u n f l o w e r a b s o r b m o d e r a t e q u a n tit ie s of selenium . P lan ts t h a t a b s o r b and a c c u m u l a t e se len iu m r e a d i l y i n c l u d e some s p e c i e s o f A s t r a g a l u s , and s u l f u r acc u m ulating p l a n t s such as t h e C r u c i f e r a e (Beeson and Matrone, 1976). The p r e s e n c e o f s e l e n i u m - a c c u m u l a t o r p l a n t s c o n t a i n i n g more t h a n 50 ppm s e l e n i u m h a s h e l p e d t o i d e n t i f y a r e a s where se len iu m t o x i c i t y i s a problem (Kubota and A llaw ay , 1972). F e r t i l i z a t i o n of s o i l w ith se l e n i u m i s no t p r a c t i c e d in th e Un ited S t a t e s , m a i n l y beca use t h e r e a c t i o n s of se l e n i u m in s o i l s a r e n o t w e l l u n d e r s t o o d ( M o r t v e d t and Cun ningham , 1971). the forages are d e f i c i e n t in selen iu m , When a n i m a l s c a n be f e d a v a r ie ty of selenium supplem ents, or g iv en selenium in je c tio n s t h a t sometimes a l s o c o n t a i n v i t a m i n E (Marczewski e t a l . , 1982). Co b a lt Cobalt has not been demonstrated to be an e s s e n t i a l elem ent fo r p l a n t grow th , b u t th e legum e r o o t n o d u le b a c t e r i a system req uires c o b a lt for the f i x a t i o n o f atmospheric nitrogen . The a v a i l a b l e c o b a lt requirements o f t h i s system c o b a lt are very low. F ie ld ca ses o f c o b a l t d e f i c i e n c i e s a f f e c t i n g legume growth have been r e p o r te d in A u s t r a l i a but n o t in th e U n ite d S t a t e s (Kubota 28 and A lla w a y , 1972). Areas a r e c o n s i d e r e d c o b a l t d e f i c i e n t when t h e e l e m e n t c o n c e n t r a t i o n i n p a s t u r e s i s t o o low t o m ee t t h e req u irem en ts of rum inants. The c o b a l t r e q u i r e m e n t o f d a i r y c a t t l e i s a b o u t 0.10 ppm i n t h e f e e d (NRC, 1978). A survey made in the United S t a t e s by the US P la n t , S o i l and N u tr itio n Laboratory (Kubota and A llaw ay, 1972) o f legumes shows t h a t th e n o r th e r n p a r t o f th e s t a t e o f M ichigan had sa m p le s c o n t a i n i n g from 0.05 t o 0.10 ppm o f c o b a l t . The a u th o r s s t a t e t h a t g r a s s e s g e n e r a l l y c o n t a i n l e s s than 0.10 ppm o f c o b a l t th ro u g h o u t th e U n ite d S ta tes. Among s e v e r a l d ecrease c o b a lt a v a i l a b i l i t y from the s o i l , are th e c l a s s o f c l a y in th e s o i l and s o i l pH. fa cto rs th at the most important Some c l a y s l i k e m uscovite adsorb c o b a l t more s t r o n g ly the o th e rs l i k e b e n to n ite. R aising the s o i l pH from 5.4 t o 6.4 d ecreases the a v a i l a b i l i t y of c o b a lt by h a l f (T isd ale and N e lso n , 1975). C o b a l t i s n o t u s u a l l y ad ded t o f e r t i l i z e r s . In c o b a lt d e f i c i e n t a r e a s , c o b a l t i s s u p p l i e d d i r e c t l y t o th e ruminants in t h e feed ( T i s d a l e and N e lso n , 1975). Molybdenum Molybdenum i s one of the most r e c e n tly recognized e s s e n t i a l p l a n t n u t r i e n t e le m e n t s (R ob ertson e t a l . , 1981 ). Molybdenum fu n ctio n s l a r g e l y in the enzyme systems o f nitrogen f i x a t i o n and n it r a t e red u ctio n . in c o r p o r a t e n itr a te P l a n t s which can n e i t h e r f i x n i t r o g e n nor in to th e ir m e t a b o l i c sy stem b e c a u se o f inadequate molybdenum become n it r o g e n d e f i c i e n t ( V ito s h e t a l . , 1981). Molybdenum d e f i c i e n c i e s in the United S t a t e s occur m ostly on 29 t h e a c i d s a n d y s o i l s o f t h e A t l a n t i c and G u l f C o a s t s , a l t h o u g h r e s p o n s e s t o f e r t i l i z a t i o n w i t h t h i s e l e m e n t h a v e a l s o b e en r e p o r t e d i n C a l i f o r n i a and t h e P a c i f i c Northwe st, Nebraska, and t h e s t a t e s b o r d e r i n g t h e G re at Lakes ( T i s d a l e and N e l s o n , 1976). Using legumes as an in d icato r plant, a map o f molybdenum c o n c e n t r a t i o n i n t h e U n i t e d S t a t e s h a s been p r e p a r e d by Kubota (1976). In g e n e ra l, t h e s o u t h - w e s t e r n s t a t e s had sam ple s w i t h a molybdenum c o n t e n t o f 6 - 8 ppm, t h e n o r t h - w e s t e r n and c e n t r a l s t a t e s 1 . 5 - 3 . 2 ppm, and t h e e a s t e r n s t a t e s 0 . 3 - 1 . 0 ppm. Most o f the ppm o f sam p les m olybdenum , c o lle c te d except surrounding the in M ichigan the lakes: h ad a b o u t so u th -eastern part of b e en sta te In t h i s a r e a t h e median molybdenum c o n c e n t r a t i o n i n le g u m e s was 1.9 ppm. has the t h e s h o r e s o f t h e Saginaw Bay, Lake H u r o n , Lake S t . C l a i r , and Lake E r i e . deficiency 0.4 reported for onions, Molybdenum cabbage, clo v er, a l f a l f a , s p i n a c h , l e t t u c e and c a u l i f l o w e r s grown i n M i c h i g a n ( B e r g e r , 1962). From t h e t o t a l molybdenum c o n c e n t r a t i o n i n s o i l s , o n l y a fractio n is av aila b le to the plant. The a v a i l a b i l i t y of molybdenum i n c r e a s e s l i n e a r l y w i t h i n c r e a s i n g s o i l pH v a l u e s . Heavy a p p l i c a t i o n s o f p h o s p h a t i c f e r t i l i z e r s w i l l i n c r e a s e t h e molybdenum up tak e of p l a n t s . Heavy a p p l i c a t i o n s o f s u l f a t e s , on t h e o t h e r hand, have a d e p r e s s i n g e f f e c t on a p l a n t ' s uptake. On s o i l s w i t h b o r d e r l i n e molybdenum d e f i c i e n c i e s , t h e a p p l i c a t i o n of e x c e s s i v e amounts of s u l f a t e - c o n t a i n i n g f e r t i l i z e r s may induce a molybdenum d e f i c i e n c y in p l a n t s . Under s u c h c o n d i t i o n s the i n c l u s i o n o f molybdenum i n t h e f e r t i l i z e r may be a d v i s a b l e 30 ( T i s d a l e and N e l s o n , 1976). A lfalfa and c l o v e r a r e medium r e s p o n s i v e t o molybdenum fertiliz atio n , w hile grasses (Robertson e t a l . , 1981). and corn are lo w responsive I n c l o v e r , molybdenum d e f i c i e n c y shows up as a g e n e r a l y e l l o w t o g r e e n i s h - y e l l o w f o l i a g e c o l o r , s t u n t i n g and l a c k o f v i g o r . The symptoms a r e s i m i l a r t o t h o s e c a u s e d by n i t r o g e n s t a r v a t i o n ( V ito sh e t a l . , 1981). D e f i c i e n c y symptoms s h o u l d be c o n f i r m e d w i t h p l a n t t i s s u e a n a l y s i s t o compa re w i t h th e s u f f i c i e n c y rang e s shown i n t a b l e 1.2 (Appendix I ) . When molybdenum d e f i c i e n c i e s a r e s u s p e c t e d , l i m i n g t o a c o n v e n i e n t s o i l pH f o r t h e c r o p i n c o n s i d e r a t i o n may i n c r e a s e t h e a v a i l a b i l i t y o f molybdenum. When t h i s i s no t enough, t h e r e a r e s e v e r a l compounds t h a t c a n be a p p l i e d a s a f e r t i l i z e r t o t h e so il, used as f o l i a r s p ra y s or fo r seed t r e a tm e n t. The most commonly u s e d c a r r i e r s o f molybdenum a r e ammonium m o l y b d a t e , molybdenum trio x id e, (R obertson et a l., molybdenum f r i t 1981b). It has and sodium m o l y b d a t e been d e m o n s tra te d in A u s t r a l i a , New Z e a l a n d , and e l s e w h e r e t h a t t h e a p p l i c a t i o n o f molybdenum t o c l o v e r s w i l l in some c a s e s produce y i e l d i n c r e a s e s e q u i v a l e n t t o t h o s e o b t a i n e d from t h e u s e o f s e v e r a l t o n s o f lim estone. Seed t r e a t m e n t i s now p r o b a b l y t h e most common way of c o r r e c t i n g molybdenum d e f i c i e n c i e s elsewhere. molybdenum i n t h e U n i t e d S t a t e s and The seed must be soaked i n a s o l u t i o n c o n t a i n i n g t h e salt (T isdale and N e l s o n , 1976) . S uppliers of molybdenum f o r se ed t r e a t m e n t o f t e n s e l l t h e p r o d u c t in two-ounce (56 g) packages which w i l l t r e a t enough seed f o r fo ur a c r e s (1.6 hectares). For one a c r e (0.40 h e c t a r e s ) , 1 / 2 ounce o f the 31- compound s h o u ld be d i s s o l v e d in t h r e e t a b l e s p o o n s o f w ater and mixed with s u f f i c i e n t seed to p la n t the acre. Using e x c e ss water can c a u s e th e c h e m ic a l t o p e n e t r a t e and i n j u r e th e s e e d embryo. The seed-m olydenum m ix tu r e s h o u ld be mixed t h o r o u g h ly and l e t dry. I t i s a d v i s a b l e t o u se a s u i t a b l e f u n g i c i d e d u s t to h e l p dry th e s e e d ( V it o s h e t a l . , 1981). Zinc Zinc i s e s s e n t i a l f o r p l a n t growth because i t c o n t r o l s t h e s y n t h e s i s o f i n d o l a c e t i c a c i d , which d r a m a t i c a l l y r e g u l a t e s p l a n t growth. Z in c i s a l s o a c t i v e i n many e n z y m a t i c r e a c t i o n s and i s n e c e s s a r y f o r c h l o r o p h y l l s y n t h e s i s and c a r b o h y d r a t e f o r m a t i o n ( V i t o s h e t a l . , 1981). Z in c i s m ost l i k e l y t o be d e f i c i e n t f o r p l a n t s g r o w i n g on s o i l s w ith c a l c a r e o u s s u r f a c e h o r i z o n s or on l e a c h e d , a c i d , sandy soils. Zinc d e f i c i e n c y may a l s o be p r e v a l e n t where th e s o i l i s high in a v a i l a b l e phosphorus. I n te r a c tio n s in v o lv in g zinc, phosphorus and i r o n r e s u l t in poor u t i l i z a t i o n of z in c by p l a n t s (Kubota and A llaw ay , 1972). The a v a i l a b i l i t y o f z in c i s c l o s e l y r e l a t e d t o th e pH l e v e l of t h e s o i l . pH i n M i c h i g a n deficiency . so ils the g reater I n g e n e r a l , t h e h i g h e r the the o p p o rtu n ity for a N e v e r t h e l e s s , some c r o p s grown i n a c i d s o i l s h a v e a l s o responded t o z i n c f e r t i l i z a t i o n i n Michigan (Robertson and L u c a s , 1981). Z in c d e f i c i e n c y i n M i c h i g a n h a s b e en r e p o r t e d in o n i o n s , p o t a t o e s , c a r r o t s , c e l e r y , c o r n , s p i n a c h , l e t t u c e and s o y b e a n s (Berger, 1962). Corn i s h i g h l y r e s p o n s i v e t o z in c f e r t i l i z a t i o n , w h ile a l f a l f a , c l o v e r and g r a s s e s are low r e s p o n s i v e (R obertson and 32 L u cas, 19 81). Zinc d e f i c i e n c y symptoms appear f i r s t on the younger l e a v e s , s t a r t in g with an i n t e r v e i n a l c h l o r o s i s fo llo w e d by a g reat reduction in the ra te o f sh oot growth. In many p la n t s t h i s p rod u ces a symptom known a s " r o s e t t i n g " . In corn and sorghum th e symptom has been c a l l e d "w hite bud" ( T i s d a l e and N e l s o n , 1976). In c o r n , th e d e f i c i e n c y a p p ea rs as a y e l l o w s t r i p i n g o f th e l e a v e s . A reas o f th e l e a f near th e s t a l k may d e v e lo p a g en era l w h it e - t o - y e llo w d i s c o lo r a t io n . In s e v e r e d e f i c i e n c i e s , the p la n t s have shortened internodes and the lower l e a v e s show a red streak about o n e -th ir d o f the way from the l e a f m argin. P l a n t s grow ing i n dark sandy or o r g a n i c s o i l s u s u a l l y show brown or purple nodal t i s s u e s when the s t a l k i s s p l i t . This i s p a r t i c u l a r l y n o t i c e a b l e i n th e low er nodes ( V it o s h e t a l . , 1981). Z in c s u l f a t e i s t h e m o st commonly u s e d s o u r c e o f z i n c f o r f e r t i l i z e r s , b u t o x i d e s , c h l o r i d e s , s u l f i d e s and c a r b o n a t e s o f zinc a re a l s o used. O r g a n i c compounds s u c h a s z i n c c h e l a t e s (zinc EDTA and z in c NTA) a r e a bo u t f i v e tim es more e f f e c t i v e th an e q u i v a l e n t amounts o f z in c found i n o r g a n i c s a l t s 1981). (Vitosh e t a l . , Z in c c a n be a p p l i e d t o t h e s o i l s a t t h e r a t e s shown i n t a b l e 1.9 (Appendix I ) . On h i g h l y r e s p o n s i v e cro p s such as c o rn , 28 k g / h e c t a r e (25 l b / a c r e ) o f z i n c showed good a v a i l a b i l i t y f o r seven years. A l s o , a f t e r s e v e r a l y e a r s o f band f e r t i l i z a t i o n where a t o t a l o f 28 k g / h e c t a r e (25 l b / a c r e ) o f z i n c was u s e d , rates and can be g r e a t l y reduced e l i m i n a t e d (Robertson and Lucas, in 1981b). some instances, even 33 Copper Copper i s e s s e n t i a l f o r p l a n t growth enzymes. and a c t i v a t i o n of many A copper d e f i c i e n c y i n t e r f e r e s w i t h p r o t e i n s y n t h e s i s and c a u s e s a b u i l d u p o f s o l u b l e n i t r o g e n compounds ( V i t o s h e t a l . , 19 81). M ineral s o i l s are considered low i n copper when the t o t a l c o n t e n t i s l e s s t h a n 6 ppm, w h i l e o r g a n i c s o i l s a r e c o n s i d e r e d low i n c o p p e r when t h e y h a v e l e s s t h a n 30 ppm o f t o t a l c o p p e r (Lucas and Knezek, 1 9 72). Most c o p p e r d e ficien t areas are a s s o c i a t e d w ith a high o rg a n ic m atter c o n te n t of the s o i l , but c o p p e r d e f i c i e n c y h a s a l s o b e en fou n d i n m i n e r a l s o i l s i n some co u n tries. A v a i l a b i l i t y o f c o p p e r t o p l a n t s i s d e p e n d e n t on sev eral factors: the presence a lum inum . amount o f o r g a n i c m a t t e r i n t h e s o i l , pH, and of m e t a l l i c ions As a g e n e r a l r u l e , such as iron, manganese, or the higher the o rg an ic m atter c o n t e n t of th e s o i l , t h e l e s s copper i s a v a i l a b l e from t h e t o t a l copper s o i l c o n t e n t . I n some c a s e s copper i s r e t a i n e d so t i g h t l y in the o rg an ic m atter t h a t i t is not p l a n t a v a i l a b l e ; in o th e r cases, p lan ts are ab le to complexes ( T i s d a l e and N e lso n , absorb 1976). copper the organic The s o l u b i l i t y o f copper m i n e r a l s d e c r e a s e s a s t h e pH o f t h e s o i l 1972). from increases (Lindsay, The a b s o l u t e l e v e l o f a m i c r o n u t r i e n t i n t h e r o o t i n g medium o f t h e s o i l may n o t be t h e m o st i m p o r t a n t f a c t o r i n i t s r e l a t i o n to p l a n t growth. More i m p o r t a n t may be t h e amounts of th e e le m e n ts in r e l a t i o n to each o th e r 197 6). In the case of copper, copper a b so rp tio n by p l a n t s ( T i s d a l e and N e l s o n , a lu m in u m i o n s i n t e r f e r e w i t h (Moore, 197 2). High l e v e l s of 34 nitrogen, phosphorus and z in c i n th e s o i l can a c c e n t u a t e copper d e f i c i e n c y in p l a n t s (Lucas and Knezec, 1972). A l f a l f a i s h i g h l y r e s p o n s i v e t o copper f e r t i l i z a t i o n , c o rn, c l o v e r and sorghum a r e medium r e s p o n s i v e , and g r a s s e s a r e low responsive (Robertson e t a l . , 1981) . In the U nited S t a t e s , copper d e f i c i e n c y i s n o t t h e most common m i c r o n u t r i e n t problem i n so ils. In the s t a t e of M ichigan, d e f i c i e n c i e s of copper have b e en r e p o r t e d f o r o n i o n s , s p i n a c h , l e t t u c e , w h e a t , o a t s , carrots and (B e rg e r, 1962). T y p i c a l v i s u a l symptoms o f copper d e f i c i e n c y i n most cro p s are ro settin g of term inal leav es, d i s c o l o r a t i o n o f l e a v e s and f r u i t s 1971). term inal die-back, and ( M o r t v e d t and Cunningham, I n many p l a n t s , copper d e f i c i e n c y shows up as w i l t i n g or l a c k o f t u r g o r and d e v e l o p m e n t o f a b l u i s h - g r e e n s h a d e b e f o r e l e a f t i p s become c h l o r o t i c and d i e . In g r a in , the le a v e s are y e l l o w i s h i n c o l o r and th e l e a f t i p s show a d i s o r d e r s i m i l a r t o f r o s t damage (Vitosh e t a l . , When a d e f i c i e n c y 1981). is U n i v e r s i t y E x te n s i o n S e r v i c e su sp ected , the (Robertson e t a l . , M ichigan S tate 1981) recommends copper f e r t i l i z a t i o n f o r h i g h l y r e s p o n s i v e c ro p s grown on o r g a n i c so ils. (6 Where t h e s o i l t e s t i s l o w , b e lo w 9 ppm, 6.7 k g / h e c t a r e lb /acre) fertiliz e r. of copper recommended a s p a r t of a ba nded On v i r g i n o r g a n i c s o i l s o r where c o p p e r h a s n e v e r b een u s e d on o r g a n i c doubled. are so il, Because copper is the recommended r a t e easily fixed and i s should be not e a s i l y l e a c h e d , f e r t i l i z e r copper t e n d s t o acc umulate i n th e s o i l . For t h i s r e a s o n , no e x t r a f e r t i l i z e r copper i s needed on o r g a n i c s o i l 35 a f t e r a t o t a l o f 22.4 k g / h e c t a r e (20 l b / a c r e ) f o r low r e s p o n s i v e c r o p s and 44.8 k g / h e c t a r e f o r h i g h l y r e s p o n s i v e c r o p s h a s been a p p l i e d , o r t h e s o i l t e s t l e v e l exceeds 20 ppm copper (Robertson e t a l . , 1 9 8 1). S o il Analysis Knowledge o f t h e f e r t i l i t y l e v e l of t h e s o i l f o r optimum p r o d u c t i o n o f c r o p s . is essen tial E lem ental a n a ly s is of s o i l h e lp s to d ia g n o s e n u t r i e n t d e f i c i e n c i e s or t o x i c i t i e s for the plant. I n a d d i t i o n , b a s e d on s o i l a n a l y s i s , t h e s c i e n t i s t can make r e c o m m e n d a t i o n s on t h e amounts o f f e r t i l i z e r n e ede d f o r maximum y i e l d s o f a c r o p , s u g g e s t s o i l management p r a c t i c e s and p r e d ic t resp o n ses to d i f f e r e n t l e v e l s of f e r t i l i z a t i o n . Soil t e s t s e r v i c e s a r e o f f e r e d t o t h e farmer a l m o s t everywhere in t h e w o r l d , e i t h e r by government owned or p r i v a t e l a b o r a t o r i e s . Sampling- A good r e p r e s e n t a t i v e sampling i s th e b a s i s f o r a good s o i l t e s t . A poor sample i s worse than none a t a l l , because i t w i l l produce m is le a d in g v alu es that w ill lead t o wrong recommendations. For g e n e r a l r o t a t i o n c r o p s , s o i l t e s t s s h o u l d be done a t l e a s t once e v e r y t h r e e y e a r s . Where l a r g e amounts of f e r t i l i z e r a r e use d, sa m p le s s h o u l d be take n e v e r y y e a r . Taking sample s o i l s from t h e e n t i r e f ar m i s a good p r a c t i c e . in the o f f season. Knowing t h e so il T h i s c a n be done b e s t test resu lts recommended f e r t i l i z e r m a t e r i a l s r e q u i r e d f o r a l l farm w i l l make t h e e ffic ie n t, m icronutrients use of b o th f e r t i l i z e r p articu larly (Shicluna, when 1983). the and t h e f i e l d s on th e an d l i m e m ore fe rtiliz e r co n tain s 36 S o i l c h a r a c t e r i s t i c s i n a farm a r e u s u a l l y g r e a t l y v a r i e d . A s a m p l e s h o u l d be t a k e n i n e v e r y a r e a t h a t i s from 2 t o 10 hectares (5 t o 10 a c r e s ) i n s i z e . Areas t h a t v a ry i n appearanc e ( c o l o r o f t h e s o i l , f o r exam ple), s l o p e d r a i n a g e , s o i l t y p e s , or p a s t t r e a t m e n t s h o u l d be sampled s e p a r a t e l y . S m all a r e a s t h a t can n ot be t r e a t e d s e p a r a t e l y by lime and f e r t i l i z e r a p p l i c a t i o n s m ight w e l l be o m i t t e d from t h e sam ple. F ifteen to twenty d i f f e r e n t l o c a t i o n s i n a f i e l d s h o u l d be sampled w ith a s o i l tu be a t t h e p lo w d e p t h o f 15 t o 20 cm (6 t o 9 i n c h e s ) i n o r d e r t o make a composite sample. As a l a r g e r amount of f e r t i l i z e r is applied i n the row, c a r e f u l a t t e n t i o n must be g i v e n t o sampling between v i s i b l e rows ( T i s d a l e and N e lso n , 1976). Sa m ple preparation- Once t h e s a m p l e h a s a r r i v e d a t t h e l a b o r a t o r y , i t s h o u l d be d r i e d , g r o u n d and s i e v e d . M oist s o i l s a m p l e s c a n be d r i e d by p l a c i n g t h e op en s a m p l e c o n t a i n e r i n a d ry in g rack or c a b i n e t . I f a l a r g e volume o f m o is t sa m p le s a r e re c eiv e d , a r t i f i c i a l drying is advised. S p e c ia l drying c ab in ets e q u i p p e d w i t h e x h a u s t f a n s e x p e d i t e a i r movement and m o i s t u r e lo ss. If heat is necessary, sh o u l d no t exceed 36° C. th e tem p era tu re of the c a b in e t Samples s h o u l d be c ru shed u n t i l a major p o r t i o n o f t h e s a m p l e w i l l p a s s a 10-mesh (U.S. No. 10, 2 mm s i e v e opening) s i e v e E x tr a ctio n d iffe r e n t (Eik e t a l . , 1980). D i f f e r e n t e x t r a c t i o n p r o c e d u r e s are used in la b o r a to r ie s. In th e same l a b o r a t o r y , d ifferen t e x t r a c t i n g s o l u t i o n s a r e em ployed fo r each m in e r a l or group o f m in era ls. The p r o p o r t i o n o f s o i l sam p le w e ig h t or volum e to e x t r a c t i n g s o l u t i o n volum e and th e tim e o f sh a k in g or s t i r r i n g 37 a l s o d i f f e r s d i f f e r e n t m i n e r a l s or group of m i n e r a l s (Grava, 1980). The c h o ic e o f e x t r a c t i n g s o l u t i o n and method o f e x t r a c t i o n is c r i t i c a l fo r the i n t e r p r e t a t i o n of the r e s u l t s . The c h o i c e depends on t h e c l a s s and ty pe o f s o i l , and, most i m p o r t a n t l y , o f t h e c o r r e l a t i o n o f l a b o r a t o r y a n a l y s i s w ith t h e c ro p r e s p o n s e i n the f i e l d . B ra y (1948) p r o p o s e d t h a t a good s o i l t e s t s h o u l d meet th e f o l l o w i n g t h r e e c r i t e r i a : 1) the e x tr a c t a n t should e x tr a c t a l l or a p r o p o r tio n a te p a r t of t h e a v a i l a b l e form o r forms o f a n u t r i e n t from s o i l s with v a ria b le properties; 2) t h e amount o f n u t r i e n t e x t r a c t e d s h o u l d be measured w ith r e a s o n a b l e acc u ra c y and speed; and 3) t h e amount o f n u t r i e n t e x t r a c t e d s h o u l d be c o r r e l a t e d w i t h t h e growth and r e s p o n se of each c ro p t o t h a t n u t r i e n t under various conditions. There a r e no u n i v e r s a l methods f o r e x t r a c t i o n f o r a l l ty p e s of so ils, different and d i f f e r e n t geographical procedures areas. In should the be follow ed in tro d u ctio n of in the Recommended Chemical S o i l T e s t Pro c ed u re s f o r t h e North C e n t r a l R e g io n o f t h e U n i t e d S t a t e s , Dahnke (1980) s t a t e s : cau tio n to rea d ers of t h i s b u l l e t i n : "A word o f A s o i l t e s t i s o n l y as s u c c e s s f u l and u s a b l e f o r a r e g i o n a s t h e d e g r e e t o w h ich i t i s c o r r e l a t e d and c a l i b r a t e d f o r t h e s o i l s and c r o p s o f t h e a r e a . The p r o c e d u r e s d e s c r i b e d i n t h i s b u l l e t i n a r e e s p e c i a l l y s u i t e d to our r e g io n . Do n o t assume t h a t t h e y w i l l work i n y o u r a r e a w i t h o u t doing t h e n e c e s s a r y r e s e a r c h ." There a r e s e v e r a l c hem ic al methods of a n a l y s i s t h a t can be u s e d f o r e a c h m i n e r a l a f t e r t h e e x t r a c t i o n p r o c e d u r e , and a l l s h o u l d p r o d u c e t h e same r e s u l t s w i t h i n r e a s o n a b l e l i m i t s . c h o i c e depends on f a c t o r s such as c o s t , and s a f e t y . The tim e , e a s e of o p e r a t i o n , Some o f t h e t e c h n i q u e s now em p lo y ed f o r e l e m e n t a l a n a l y s i s a r e u l t r a v i o l e t and v i s i b l e s p e c t r o s c o p y (Cheng and P ratter, 1979), s p e c t r o f l u o r i m e t r y ab so rp tio n (Schenk, and e m i s s i o n s p e c t o p h o t o m e t r y 1979), (C hristian, atom ic 1 9 79 ), p lasm a e m iss io n s p e c t r o p h o t o m e t r y , i n d u c t i v e l y c o u p l e d p l a s m a d i s c h a r g e (Barnes, 1979), and n e u tr o n a c t i v a t i o n a n a l y s i s (Ehmann and J a n g h o r b a n i , 1979). 39 Mineral S ta tu s o f P la n ts and Animal Requirements S o i l - P l a n t and Plant-Animal R e la tio n sh ip s P l a n t s o b t a i n m ost o f t h e i r n u t r i e n t s from th e s o i l . The a v a i l a b i l i t y o f elem en ts in the s o i l s o l u t i o n i s one o f the main f a c t o r s th a t determine the presence and con cen tratio n o f m in era ls in p la n t t i s s u e . The a d d itio n o f a p la n t n u tr ie n t to the s o i l may or may not change th e c o n c e n t r a t i o n o f t h i s n u t r i e n t in th e t i s s u e s o f th e p l a n t s t h a t grow on t h a t s o i l . The c o n c e n t r a t i o n o f a n u t r i e n t e le m e n t i n a p l a n t o f t e n te n d s t o r i s e a lo n g a sig m o id c u r v e as th e a v a i l a b l e s u p p ly o f t h a t e le m e n t in th e s o i l i s in c r e a s e d from a v e r y low l e v e l t o superabundance. Thus, when th e f i r s t increments o f a n u tr ie n t elem ent are added to a d e f i c i e n t s o i l , crop growth may be increased without an ap p re c ia b le in c re a se in the c o n cen tra tio n o f t h i s elem ent in p la n t t i s s u e s . With further a d d i t i o n s o f t h i s e le m e n t t o th e s o i l , both c ro p growth and th e t i s s u e c o n cen tra tio n o f the elem ent in crea se. a d d itio n s o f the e lem en t, With s t i l l further i t s con cen tra tion reaches a " c r i t i c a l v a l u e " , or th e c o n c e n t r a t i o n in th e p l a n t t i s s u e r e q u ir e d fo r optimum growth o f the p la n t. d ifferen t sp ec ies and This c r i t i c a l l e v e l v a r ie s due to v a r ie tie s, and may a l s o vary among d i f f e r e n t temperature, m oisture, and l i g h t c o n d itio n s , as w e l l as with d i f f e r e n t l e v e l s o f supply o f other n u tr ie n ts . A dditions of th e e le m e n t t o th e s o i l above t h o s e n e c e s s a r y t o p r o v i d e th e c r i t i c a l v a l u e o f t i s s u e c o n c e n t r a t i o n s o f t h i s e le m e n t c a u se o n ly minor in c r e a se s or even d ecreases in crop growth, but they may lea d to further in c r e a se s in the concen tration o f the elem ent 40 in th e crop. The e f f e c t o f a d d i t i o n o f a n u t r i e n t f e r t i l i z e r upon t h e c o n c e n t r a t i o n o f t h i s n u t r i e n t i n t h e f e r t i l i z e d c r o p may, t h e r e f o r e , r a n g e from no i n c r e a s e i n t h e n u t r i e n t i n t h e p lan t, even though pronounced increases in crop y i e l d are o b ta in e d , to in c r e a s e s in the c o n c e n tr a tio n of the n u t r i e n t in the c ro p w i t h o u t any i n c r e a s e in c ro p y i e l d (Allaway, 1971). Some elem en ts such as boron are e s s e n t i a l for p la n t s but not fo r a n i m a l s . Some o t h e r s such as s e le n iu m are e s s e n t i a l fo r anim als but not for p la n t s . Furthermore, a h e a lth y crop in which a l l the n u tr ie n t requirements have been met may not be s u f f i c i e n t in term s o f m in e r a l c o m p o s it io n fo r th e growth o f a n im a ls . o th e r c a s e s , In p l a n t s can a ccu m u late c e r t a i n e le m e n t s such as selenium or molybdenum th a t are not harmful for t h e ir growth, but t h a t can be t o x i c t o th e a n im a ls . In o th e r w ords, p l a n t s have d i f f e r e n t requirements than animals for m in erals. N itrogen Nitrogen content fertilizatio n d e fic ie n t of p la n ts in r e l a t i o n to s o i l statu s and A p p lica tio n of nitrogen f e r t i l i z e r s to a n itro g e n so il freq u en tly resu lts i n an i n c r e a s e in the c o n c e n t r a t i o n o f t o t a l p r o t e i n i n t h e c r o p p r o d u c e d , and s i n c e the f e r t i l i z e d crop u s u a l l y produces a h ig h er y i e l d , th e t o t a l p r o t e i n p r o d u c e d p e r h e c t a r e may be s u b s t a n t i a l l y ( A l l a w a y , 1971). increased Under t h e same e n v i r o n m e n t a l c o n d i t i o n s , t h e l i m i t f o r p r o t e i n c o n c e n t r a t i o n i n a c ro p i s t h e g e n e t i c s of t h e plant. I n g e n e r a l legumes c o n t a i n h ig h er p r o t e i n c o n c e n t r a t i o n s th an g r a s s e s or c e r e a l s . The p r o t e i n c o m p o s i t i o n , i n t e r m s o f amino a c i d s , i n th e p l a n t i s a l s o g e n e t i c a l l y c o n t r o l l e d , and i t i s u n l i k e l y i t w i l l be changed by f e r t i l i z a t i o n . The e f f e c t s of n i t r o g e n f e r t i l i z a t i o n on p r o t e i n c o n c e n t r a t i o n and q u a l i t y i n p l a n t s can be summarized as f o l l o w s (Thompson e t a l . , 1) 1960), The amount o f p r o t e i n produced per h e c t a r e of l a n d w i l l be s i g n i f i c a n t l y i n c r e a s e d by u s e o f n i t r o g e n f e r t i l i z e r s on nitrogen d e fic ie n t s o i l s . 2) The c o n c e n t r a t i o n of p r o t e i n w i l l be i n c r e a s e d somewhat under t h i s c o n d i t i o n , b u t n i t r o g e n f e r t i l i z a t i o n w i l l n o t b r i n g t h e p r o t e i n l e v e l o f l o w - p r o t e i n cro ps such as r i c e t o t h e l e v e l found i n wheat o r legumes. 3) The n u t r i t i o n a l q u a l i t y o f t h e p r o t e i n i s g e n e r a l l y u n a f f e c t e d by n i t r o g e n f e r t i l i z a t i o n . P r o t e i n q u a l i t y i n terms of amino a c i d com position i s no t o f p rim a ry importanc e f o r ru m in a n ts , s i n c e t h e microorganisms i n t h e rumen a r e c a p a b l e o f s y n t h e s i z i n g t h e amino a c i d s r e q u i r e d by the a n im a l. N o r m a l l y , 75% or more of t h e n i t r o g e n i n th e p l a n t i s in t h e form o f p r o t e i n . H o w ev e r, a n y t h i n g t h a t i n t e r f e r e s w i t h t h e p r o t e i n s y n t h e s i s p r o c e s s , such as a s h o r t a g e of en ergy w i t h i n t h e p l a n t , may c a u s e an a c c u m u l a t i o n o f n o n p r o t e i n n i t r o g e n compounds. The compounds t h a t a c c u m u l a t e u n de r c o n d i t i o n s o f slowed p r o t e i n s y n t h e s i s i n c l u d e n i t r a t e s , f r e e amino a c i d s , and amides (Allaway, 1971). N itrates in forages- Heavy a p p l i c a t i o n o f n i t r o g e n f e r t i l i z e r o r m anur e and s e v e r e d r o u g h t o r o t h e r f a c t o r s w hich reduce p l a n t m e ta b o lism w i l l tend t o cause some a c c u m u la tio n of nitrates. Under normal c o n d i t i o n s , f o r a g e s and p a s t u r e s do n o t c o n t a i n o v e r 0.5% n i t r a t e s . O c c a s i o n a l l y p l a n t s w i l l c o n t a i n as much a s 5% n i t r a t e s on a d r y b a s i s . lam bsquarter Pigweed (A m a r a n t h u s s p . ) , (Che nopodium s p . ) , ragweed (Ambrosia sp.) and o t h e r weeds may acc um u late v e r y h igh l e v e l s of n i t r a t e b u t g e n e r a l l y com prise a s m a ll p e r c e n t of the d i e t . N itr a te s are norm ally r e d u c e d s u c c e s s f u l l y t o n i t r i t e s , t o n i t r o u s o x i d e and t h e n t o ammonia i n th e rumen. Numerous s t u d i e s i n d i c a t e t h a t c a t t l e can s a f e l y consume n i t r a t e s e q u i v a l e n t t o no more t h a n 2% o f t h e t o t a l d r y m a t t e r of t h e r a t i o n , o r a p p r o x i m a t e ly 44 g o f n i t r a t e per 100 kg of body w eight. If the n itra te co n ten t is s u f f i c i e n t l y h i g h , and c o n v e r s i o n t o ammonia i s s l o w , t h e n a major p a r t o f t h e n i t r a t e i s reduced t o n i t r i t e , and some of the n itrate and n i t r i t e may e n t e r the blood stream . N itrate is e x c r e t e d i n t h e u r i n e b u t n i t r i t e may d i s p l a c e t h e ox yg e n from some of th e h em o g lo b in methemoglobinemia. th eir blood of th e blood re su ltin g in Animals c a n t o l e r a t e some met h e m o g l o b i n i n w ithout harm , and they possess an enzyme, m e t h e m o g l o b i n r e d u c t a s e , f o r c o n v e r t i n g m e t h e m o g l o b i n back t o hemoglobin. Methemoglobin l e v e l s n o r m a l l y must approach 60 t o 90% o f t h e h e m o g l o b i n t o be l e t h a l . C a t t l e fed high l e v e l s of n i t r a t e s o v e r a lo n g p e r i o d of tim e ten d to a d a p t to th e lower o xygen-carrying c ap acity of the blood by i n c r e a s i n g c o n c e n tr a ti o n of e r y t h r o c y te s in the b lo o d . n itrates the Toxic l e v e l s of ( o v e r 2% o f t h e d i e t ) may r e s u l t i n p e a k l e v e l s o f methemoglobin about f o u r h ours a f t e r f e e d i n g . Labored b r e a t h i n g , f r o t h i n g a t t h e mouth, and a brownish t o b l u i s h - g r e y c o l o r of th e non-pigmented s k i n and mucous membranes a r e symptoms of n i t r a t e 43 to x ic ity . P regn an t cows may a b o r t when th e o x y g e n - c a r r y in g c a p a c i t y o f th e b lo o d i s s e r i o u s l y red uced (H illm a n , e t a l . , 1983). Nitrogen s o l u b i l i t y in p l a n t s - feed is r e a d ily s o lu b le . attack ed in the P a r t of the p r o t e i n in the H ighly s o l u b l e p r o t e i n i s q u ic k ly rumen by b a c t e r i a l s i m p l e r compounds and t o ammonia. enzymes and d e g r a d e d t o When t h i s r e l e a s e d ammonia exceeds t h e c a p a c i t y o f rumen b a c t e r i a t o use i t t o make p r o t e i n t h e r e i s an i m m e d ia te l o s s o f p a r t o f t h e d i e t a r y n i t r o g e n v i a excretion in the u r in e . D irect cut grass s ila g e s and h i g h - m o i s t u r e c o rn and sorghum s i l a g e s o f t e n c o n t a i n more th a n 60% of w a t e r - s o l u b l e p r o t e i n , and t h i s i s n o t u t i l i z e d v e r y e f f i c i e n t l y by ru m in a n ts on a l l - s i l a g e d i e t s . Some c o n c e n t r a t e f e e d s have a high p e r c e n t a g e o f s o l u b l e crude p r o t e i n , which makes them l e s s s u i t a b l e f o r f e e d i n g w ith s i l a g e s th a n o t h e r c o n c e n t r a t e s ; e.g., most b y - p r o d u c t f e e d s have more s o l u b l e p r o t e i n th an c o rn g r a i n . On t h e o t h e r h a n d , t h e s o l u b i l i t y o f p r o t e i n i n c o r n o r o t h e r g r a i n s t h a t h a v e b e en f e r m e n t e d i n m o i s t s t o r a g e i s i n c r e a s e d (NRC, 197 8). N itrogen requirements o f dairy c a t t l e - A major component of animal t i s s u e s and organs i s p r o tein . A ll c e l l s s y n t h e s i z e p r o t e i n fo r p a r t or a l l of th e ir w ithout p r o te in s y n th e s is l i f e could not e x i s t . in the animal life c y c l e and P ro te in turnover i s rapid in the c e l l s , e s p e c i a l l y for those in e p i t h e l i a l t i s s u e such as in th e in te stin a l tra ct. C o n s e q u e n t ly , p r o v id in g r e p la c e m e n t p r o t e i n from th e d i e t i s e s s e n t i a l to meet t h e s e t u r n o v e r r e q u ir e m e n ts in a d d i t i o n t o p r o v i d i n g fo r growth and 44 other productive functions. The p e r c e n t of p r o t e i n r e q u i r e d in t h e d i e t i s h i g h e s t f o r young g r o w i n g a n i m a l s . grad u ally I t declin es u n t i l m a t u r i t y when o n l y enough p r o t e i n t o m a i n t a i n body t i s s u e s i s r e q u i r e d . P r o d u c t i v e f u n c t i o n s such a s pregnancy and l a c t a t i o n i n c r e a s e t h e r e q u i r e m e n t s b e c a u s e o f i n c r e a s e d o u t p u t o f p r o t e i n i n p r o d u c t s o f c o n c e p t i o n and i n m i l k and because of an i n c r e a s e d m e t a b o l i c r a t e a s s o c ia te d w ith the p r o d u c t i v e f u n c t i o n (Church and Pond, 1974). I n t h e l a c t a t i n g cow, p r o t e i n i s e x c r e t e d i n m i l k . The p r o t e i n c o n c e n t r a t i o n o f m i l k from H o l s t e i n cows i s around 3.22% ( C e r b u l i s and F a r r e l l , 197 5). A cow p r o d u c i n g 30 kg o f m i l k s e c r e t e s 0.97 kg o f p r o t e i n a d a y . T h a t cow's d i e t m u st r e p l a c e th at protein, urine, h air, m aintenance. as w e l l as r e p l a c e the p r o t e i n l o s t in f e c e s , etc. and a l s o p r o v i d e t h e p r o t e i n r e q u i r e d f o r The NRC (1978) r e p o r t e d t h e p r o t e i n requirem ent f o r a 600 kg (1300 l b ) cow p r o d u c i n g 30 kg (66 l b ) o f m i l k w i t h 3.5% f a t c o n t e n t p e r d a y a t a r o u n d 2.95 kg p r o t e i n p e r d a y . If t h i s cow e a t s 20 kg (45 lb) o f d r y m a t t e r a day, t h e r a t i o n needs t o be 14.75% p r o t e i n t o meet her r e q u ir e m e n ts . N itrogen content of c o n c e n tra tio n s of p r o te in . forages- Forages have v a r i a b l e In a g iven g r a s s , the degree of m a t u r i t y i s t h e main f a c t o r a f f e c t i n g p r o t e i n c o n t e n t . Orchard g r a s s (D a c t y l i s g l o m e r a t a ) f o r e x a m p l e ( E ly e t a l . , 1 9 5 3 ), had 24.8% p r o t e i n when c u t e a r l y in t h e se ason , and 12.4% when c u t a t a l a t e stage of m atu rity . F i r s t c u t , su n c u r e d a l f a l f a hay i n i t s e a r l y v e g e t a t i v e s t a t e has around 24% p r o t e i n . This p r o te in c o n t e n t d e c r e a s e s t o 16% when a l f a l f a i s c u t a t mid-bloom, and to 45 13% when i t i s cut when mature (NRC, 1978). Corn s i l a g e does not change much in c o m p o s itio n w ith m a t u r ity e x c e p t dry m atter con ten t. S i l a g e made from corn c u t a t a s o f t dough s t a g e had 7.4% p r o t e i n , 7.4% when c u t a t a medium-hard dough s t a g e , and 7.3% when c u t a t a t an e a r l y d e n t s t a g e o f m a t u r it y (C o lo v o s e t a l., 1970 ). In M ic h ig a n , d a ta from 1 975-1976 show t h a t corn s i l a g e s had an a v e r a g e o f 8.3% p r o t e i n . S i l a g e made from corn cu t e a r l y in the season had 12% p r o te in and 21% dry m atter, w h ile s i l a g e made from corn c u t l a t e in th e s e a s o n a f t e r th e f i r s t f r o s t s in November had 8.7 p r o te in and 49.2% dry matter (Hillman and Fox, 1977). Nitrogen d e f i c i e n c y i n r u m in a n ts - While f o r nonruminants t h e amino a c i d c o m p ositio n of t h e p r o t e i n i s v e r y i m p o r t a n t , f o r r u m in a n ts b a c t e r i a l s y n t h e s i s p r o v i d e s t h e e s s e n t i a l amino a c i d s t h a t a r e d e f i c i e n t in t h e r a t i o n . Ruminants a r e l i k e l y t o s u f f e r f i r s t from i n s u f f i c i e n t amount o f p r o t e i n i n the d i e t r a t h e r th an s u f f e r i n g from i n s u f f i c i e n t q u a n t i t y or imbalance o f amino a c i d s , or l o w - q u a l i t y p r o t e i n , a s non-rum in ants do. In g e n e r a l, p r o te in d e f i c i e n c y i n r u m i n a n t s h a s t h e same e f f e c t a s i t d o e s i n non­ rum inants. P ro tein d ep riv atio n symptoms are non-specific, r e s e m b l in g t h o s e seen i n p a r t i a l or t o t a l s t a r v a t i o n . The growth o f t h e p r o t e i n d e p l e t e d animal may be g r e a t l y slowed. a ltera tio n s in D e p e n d i n g on t h e the sk eletal Profound t i s s u e s may be e n c o u n t e r e d . s e v e r i t y of the d e f ic ie n c y state, varying deg rees of r e t a r d a t i o n of e p ip h y s e a l or c o s t a l c a r t i l a g e c e l l p r o l i f e r a t i o n w i l l be f o u n d . C a r t i l a g e i s a c r i t i c a l index of t h e n u t r i t i v e s t a t u s o f t h e organism ( F o l l i s , 1958). C a t t l e fed 46 p ro tein d e fic ie n t d ie ts w ill show s l o w g r o w t h , r e d u c e d f e e d i n t a k e and d e c r e a s e d p r o t e i n c o n t e n t i n t h e org an s and s k e l e t a l m uscle. Low a l b u m i n and u r e a i n t h e b l o o d i n d i c a t e p r o t e i n d eficien t d iets. d e ficien t cows. M ilk p ro d u c tio n Growth o f the is decreased fetu s is in im paired protein and body c o n d i t i o n i s d e p re s s e d i n cows fed p r o t e i n d e f i c i e n t d i e t s f o r an extended p e r i o d . I n a d d i t i o n , p r o t e i n d e f i c i e n t a n i m a l s have low immune and t r a n s p o r t p r o t e i n s i n t h e i r blo o d and reduced hormone s e c r e t i o n s t h a t may p r e d i s p o s e them t o i n f e c t i o u s and m e t a b o l i c d i s e a s e s (NRC, 1978). C a t t l e on p a s t u r e a r e n o t l i k e l y t o s u f f e r from s e v e r e p ro te in d eficien cy . D u r i n g a d r y p e r i o d when t h e p a s t u r e s a r e o l d and s c a r c e , however th e p r o t e i n l e v e l o f p a s t u r e g r a s s may be t o o low t o s u s t a i n a good g r o w t h o r m i l k p r o d u c t i o n . R y e g r a s s ( L o l ium m u l t i f l o r u m ) , c o n c e n tra tio n as for ex am p le, can have a p ro tein low a s 4.0% d r y b a s i s (Crampton and H a r r i s , 1969). Mixed p a s t u r e s of legumes and g r a s s e s u s u a l l y have p r o t e i n c o n c e n t r a t i o n s h i g h e r th a n 10%. Corn s i l a g e , with an a v e r a g e of 8.3% p r o t e i n , i s n o t enough t o m e e t t h e p r o t e i n r e q u i r e m e n t s o f h i g h p r o d u c i n g d a i r y cows, w h ic h n e ed a r a t i o n o f a b o u t 15% pro tein part during the first of the lactatio n . R ations c o n t a i n i n g 14% p r o t e i n a r e needed by 100 kg (220 lb) c a l v e s . The p r o t e i n r e q u i r e m e n t d e c r e a s e s f o r 300 kg c a l v e s , r a t i o n s w i t h 11% p r o t e i n (NRC, 1 978). w h ich need Good t o medium q u a l i t y a l f a l f a , 15 t o 20% p r o t e i n , may s a t i s f y th e p r o t e i n re q u ir e m e n ts of most a n im a ls. 47 Calcium Calcium content fertilizatio n - in p l a n t s in r e l a t i o n to s o i l Calcium i s a lw a y s present in status green and p lan ts. U s u a l l y t h e legumes c o n t a i n more c a l c i u m t h a n do g r a s s e s . G ra in c r o p s a r e g e n e r a l l y lower i n c a l c i u m th a n a r e f o r a g e c r o p s , and i s o f t e n n e c e s s a r y t o add a c a l c i u m s u p p l e m e n t t o t h e d i e t s o f cattle t h a t a re being fed r a t i o n s high forage. in g ra in and low i n The c a l c i u m c o n t e n t o f an y on e p l a n t s p e c i e s d o e s n o t c h a n g e v e r y much when c a l c i u m i s ad ded t o t h e s o i l . T herefore, t h e l e v e l o f c a l c i u m i n t h e s o i l h a s few d i r e c t e f f e c t s on t h e n u tr itio n a l q u a lity of p lan ts. But t h e a d d i t i o n o f c a l c i u m , in t h e form of l i m e s t o n e , t o an a c i d s o i l f r e q u e n t l y makes i t e a s i e r t o grow leguminous p l a n t s , l i k e a l f a l f a , which a r e o f t e n h igh in p r o t e i n and e s s e n t i a l m i n e r a l s (U.S. P l a n t , S oil, and N u t r i t i o n Lab. S t a f f , 1965). Calcium con ten t in fo r a g e s- T y p ical calciu m c o n cen tra tio n s i n g r a s s e s r a n g e from 0.4 t o 0.8%, b u t i t c a n be l o w e r t h a n 0.3% l and h ig h er than 1.0 %. A lfa lfa c a lc iu m c o n c e n t r a t i o n s are u s u a l l y between 1.2 and 2.3%, but some samples can be higher than 2.5% or lower than 0.60% (Church and Pond, 1974). In Michigan in 1 9 7 5 - 1 9 7 6 , corn s i l a g e had an a v e r a g e c a lc iu m c o n t e n t o f 0.28% (Hillman and Fox, 1977). Ear corn samples analyzed in Penn S tate from 1969 t o 1973 had an a v e r a g e o f 0.05% c a lc iu m and s h e l l e d corn sa m p le s 0.03% (Adams, 1975). Soybean m eal has a c a lc iu m c on cen tration o f around 0.36% (NRC, 1978). Calcium conten t in forages remains q u ite con sta n t with the stage o f m a t u r ity or w ith the season o f th e y e a r . In th e 48 Southern P l a i n s r e g i o n of t h e U nited S t a t e s , c a l c i u m c o n t e n t of p e r e n n i a l g r a s s e s r a n g e d from 0.33% i n J a n u a r y and A u g u s t t o 0.43% i n A p r i l Calcium (Beeson and Matrone, 1976). r e q u i r e m e n ts o f d a i r y c a t t l e - A 600 kg (1300 lb) cow producing 30 kg (66 lb ) o f m i l k w ith 3.5% f a t c o n t e n t per day r e q u i r e s a b o u t 100 g o f c a l c i u m , o r 0.5% o f t h e d i e t when e a t i n g 20 kg (44 l b ) o f d r y m a t t e r , d a i l y . A 200 kg (440 l b ) H o l s t e i n h e i f e r needs about 21 g c a l c i u m , o r 0.40% of t h e d i e t when e a t i n g 5.2 kg o f d r y m a t t e r , p e r d a y (NRC, 1978). A n i m a l s c onsum in g legumes or mixed p a s t u r e s a r e n o t l i k e l y t o s u f f e r from c a l c i u m deficiency. However, i f the d i e t c o n s i s t m a i n l y o f g r a s s e s , corn s i l a g e and g r a i n , su pp le m e nta ry c a l c i u m may be needed t o meet t h e requirements. C alcium req u irem en ts are calcu lated phosphorus r e q u i r e m e n ts f o r d a i r y c a t t l e . in r e l a t i o n to The r a t i o o f c a l c i u m t o phosphorus i n bone i s about 2:1 i n o l d e r a n im a l s and somewhat l o w e r i n young a n i m a l s . 1.3:1.0. In m ilk th e r a t i o is approxim ately Except fo r p rep artu m r a t i o n s , a high r a t i o of c a lc iu m to phosphorus is f a r l e s s c r i t i c a l fo r rum inants than i t i s for l a b o r a t o r y a n im a l s . However, a c a l c i u m t o phosphorus r a t i o below 1:1 can reduce performance. Growth r a t e and feed u t i l i z a t i o n of c a l v e s have been s a t i s f a c t o r y w ith c a l c i u m t o phosphorus r a t i o s r anging from 1:1 t o 7:1 (NRC, 1978). For l a c t a t i n g cows, c a l c i u m t o p h o s p h o r u s r a t i o s o f 1 : 1 , 1 : 4 , and 8 :1 p r o d u c e d no c h a n g e i n m i l k p r o d u c t i o n (Smith e t a l . , 1 9 66). I n l o n g term e x p e r i m e n t s w ith p r e g n a n t h e i f e r s b e t t e r a b s o r p t i o n o f both e le m e n ts o c c u r r e d w ith a 2:1 c a lc iu m t o phosphorus r a t i o (Manston, 1967). 49 Calcium deficiency phosphorus n u t r i t i o n is in rum inants- A d e q u a t e c a l c i u m and d e p e n d e n t ‘u p o n t h r e e facto rs: a s u f f i c i e n t s u p p l y o f each e l e m e n t , a s u i t a b l e r a t i o between them, and t h e p r e s e n c e o f v i t a m i n D (Maynard and L o o s l i , 196 9). The m o st o b v i o u s symptoms o f s e v e r e c a l c i u m d e f i c i e n c y a re r i c k e t s and o s t e o m a l a c i a . w hich is R i c k e t s i s a d i s e a s e o f t h e growing s k e l e t o n ch aracterized by a d e c r e a s i n g co n cen tratio n of h y d r o x y a p a t i t e i n t h e o r g a n i c m a t r i c e s o f c a r t i l a g e and bone. O s te o m a l a c i a i s r i c k e t s in the a d u l t and, s i n c e c a r t i l a g e growth has ceased, is a sk eletal d isease in ad u lts which is c h a r a c t e r i z e d by a d e c r e a s e d c o n t e n t o f h y d r o x y a p a t i t e i n bone m a t r i x ( F o l l i s , 1958). prevents normal I n young c a l v e s , a c a l c i u m - d e f i c i e n t d i e t bo ne g r o w t h and r e t a r d s g e n e r a l g r o w t h and development. The bones o f a f f e c t e d c a l v e s a r e low i n c a lc iu m and p h o s p h o r u s and f r a c t u r e spontaneously. I n m a t u r e cows, the f e e d i n g o f r a t i o n s low i n c a l c i u m o v e r a long p e r i o d o f time may cause a d ep letio n of calcium and p h o s p h o r u s in the bones, r e s u l t i n g i n f r a g i l e , e a s i l y f r a c t u r e d b o n e s and r e d u c e d m i l k y i e l d (NRC, 1978). With an adeq uate phosphorus i n t a k e (80 t o 100 g / d a y ) , d a i r y cows f e d 200 g c a l c i u m / d a y and v i t a m i n D (300000 IU /day) showed b e t t e r rep ro d u ctiv e r e c e i v i n g 100 g c a l c i u m / d a y . p e r f o r m a n c e t h a n cows The v a r i a b l e s m e a s u r e d i n t h i s experiment were c o m p l e t i o n of u t e r i n e i n v o l u t i o n , days t o f i r s t o v u l a t i o n , and days t o f i r s t p o s t - p a r t u m e s t r u s (Ward, 1971). Milk fever- Dry cows fed e x c e s s i v e amounts of c a l c i u m a re l i k e l y to d e v elo p m ilk fe v e r ( p a rtu rie n t p a re sis) a t c a lv in g . T h i s m e t a b o l i c d i s o r d e r i s c a u s e d by a d i s t u r b a n c e i n c a l c i u m 50 m etabolism m a n i f e s t e d by a marked d ro p i n b l o o d serum c a l c i u m a t p a r t u r i t i o n or soon t h e r e a f t e r (NRC, 1978). Several p re v e n tiv e procedures to a v o id p a r t u r i e n t p a r e s i s have been t r i e d . The f i r s t and most i m p o r t a n t p r a c t i c e t o f o l l o w i s t o p r o v i d e t h e d r y cow w i t h a d i e t w e l l b a l a n c e d i n e n e r g y , p r o t e i n and v i t a m i n s . Abrupt r a t i o n changes and e x c e s s i v e weight i n c r e a s e s sh o u l d be a v o id e d . I f c o rn s i l a g e t h a t i s r e l a t i v e l y high i n energy i s t h e main i n g r e d i e n t of t h e d i e t , i t sh o u l d not be p r o v i d e d ad l i b i t u m t o t h e cows, t o p r e v e n t from becoming ex cessiv ely fa t. Adequate f i b e r t o m a i n t a i n rumen m o t i l i t y s h o u l d be p r o v i d e d (Olson, 1979). C alcium sources- T h e r e a r e s e v e r a l p r o d u c t s t h a t can be used as so u r c e s o f c a l c i u m f o r d a i r y c a t t l e . Limestone (calcium c a r b o n a t e ) h a s a r o u n d 38% c a l c i u m , bone m e a l s from 20 t o 30%, o y s t e r s h e l l f l o u r a r o u n d 36%, m o n o c a l c i u m p h o s p h a t e 16%, and d i c a l c i u m phosphate 22% (Hillman e t a l . , 1983). Cement k i l n d u s t c o n s i s t i n g o f a r o u n d 27% c a l c i u m , c a n a l s o be u s e d a s a c a l c i u m s o u r c e f o r a n im a l s r a t i o n s (Jordan e t a l . , L im estone has been p ro p o se d 1980). as a b u f f e r i n g , or more a c u r a t e l y a s an a l k a l i n i z i n g , a g e n t f o r r u m i n a n t s i n o r d e r t o improve t h e e f f i c i e n c y o f d i g e s t i o n and p r o d u c t i o n (Wheeler and N o l l e r , 1976; W h ee le r, 1980a and b; Wheeler e t a l . , 1981b, c and d; B a s s , 1982). Cement k i l n d u s t s h a v e b e e n u s e d f o r t h e same p u r p o s e ( W h e e l e r , 1979; W h e e l e r and O l t j e n , 1979; Ward e t a l . , 1979; N o l l e r e t a l . , Wheeler e t a l . , 1981a). 1980; Bush e t a l . , 1981; W h e e l e r , 1981; 51 Phosphorus Phosphorus fertilizatio n - c o n t e n t o f p l a n t s i n r e l a t i o n t o s o i l s t a t u s and P h o s p h o r u s i s o f c r i t i c a l i m p o r t a n c e t o many o f th e l i f e p r o c e s s e s o f both p l a n t s and a n im a ls. When th e s o i l i s d e f i c i e n t i n p h o s p h o r u s , c e r t a i n p l a n t s p e c i e s may c o n t a i n t o o l i t t l e of t h i s e l e m e n t t o meet t h e req u ire m e n t o f t h e animal t h a t e a ts the p l a n t 1965). (U.S. P l a n t , S o il, and N u t r i t i o n Lab. S taff, I n g e n e r a l , low c o n c e n t r a t i o n s of a v a i l a b l e phosphorus in the s o i l resu lt in p l a n t s with i n s u f f i c i e n t am ounts o f e le m e n t t o meet th e r e q u i r e m e n ts of a n im a l s . o f phosphorus f e r t i l i z a t i o n the The s u c c e s s f u l use t o c o r r e c t phosphorus d e f i c i e n c y in g r a z i n g a n im a l s i s de pendent upon the s o i l and th e p l a n t s p e c i e s involved. On some s o i l s , a d d i t i o n o f phosphorus f e r t i l i z e r s w i l l no t b r i n g about i n c r e a s e s i n th e phosphorus c o n c e n t r a t i o n s in the p l a n t grown, e v e n t h o u g h s u b s t a n t i a l i n c r e a s e s i n y i e l d may be noted. Where mixed p a s t u r e s c o n t a i n i n g both g r a s s e s and legumes a r e f e r t i l i z e d , t h e i n c r e a s e i n p e r c e n t of legumes in t h e m ix ture resu ltin g from p h o s p h o r u s fertiliz atio n may h a v e im portant e f f e c t s on t h e a n i m a l s g r a z i n g t h e p a s t u r e , i n d e p e n d e n t o f t h e e f f e c t on t h e phosphorus c o n c e n t r a t i o n in th e p a s t u r e p l a n t s . general, In d e c i s i o n s c o nce rn in g use of phosphorus f e r t i l i z e r s a r e b a s e d upon t h e e x p e c t e d r e s p o n s e i n c r o p p r o d u c t i o n . Where l i t t l e or no r es po n se i n p l a n t growth can be e x p e c te d , phosphorus s h o u l d be s u p p l e m e n t e d d i r e c t l y t o t h e a n i m a l s ' d i e t s t o m eet t h e i r r e q u i r e m e n ts (Allaway, 1972). Phosphorus co n c en tr a tio n in fo rag es- T yp ical phosphorus con cen tra tio n in g r a sse s i s 0.2 to 0.3%, but i t can be lower than 52 0.2% and h i g h e r th an 0.4%. I n a l f a l f a , phosphorus c o n c e n t r a t i o n s a r e s i m i l a r t o t h o s e i n g r a s s e s , u s u a l l y 0.2 t o 0.3%, and t h e y c a n be l o w e r t h a n 0.15% and h i g h e r t h a n 0.7% (Church and Pond, 1 974). C o rn s i l a g e s a m p l e s i n M i c h i g a n i n 19 75-1976 had an a v e r a g e 0.29% p h o s p h o r u s c o n t e n t d r y b a s i s 1 9 77 ). E a r c o r n i n P e n n s y l v a n i a , from 1969 t o 1973, had an average of 1975). ( H i l l m a n and F o x , 0.28% p h o s p h o r u s , and s h e l l e d c o r n 0.31% (Adams, Soybean o i l meal has a phosphorus c o n t e n t o f about 0.75% (NRC, 1978). Phosphorus c o n te n t m atu rity and to Southern P l a i n s the in p l a n t s season of region of the is related year. to the p l a n t s ' G rasses from t h e t h e U n i t e d S t a t e s had an a v e r a g e phosphorus c o n t e n t o f 0.34% i n A p r i l , when t h e p l a n t s were young and r a i n f a l l was 72 mm (2.83 i n ) , and 0.10% i n F e b r u a r y when t h e rain fa ll was 26 mm (1.03 in ) and t h e p a s t u r e s were d r y and dormant due t o t h e w i n t e r (Beeson and Matrone, 1976). Phosphorus r e q u i r e m e n ts of d a i r y c a t t l e - A 600 kg (1300 l b ) cow, p r o d u c i n g 30 kg (66 l b ) o f m i l k w i t h 3.5% f a t c o n t e n t a day, r e q u i r e s around 70 g of phosphorus d a i l y . I f t h e dry m a t t e r i n t a k e o f t h i s cow i s 20 kg (44 l b ) , t h e r a t i o n s h o u l d be 0.35% phosphorus. A 200 kg (440 lb ) h e i f e r e a t i n g 5.2 kg o f dry m a t t e r a day r e q u i r e s 14 g o f p h o s p h o r u s o r a b o u t 0.27% o f t h e r a t i o n (NRC, 1978). Phosphorus r e q u ir e m e n ts of l a c t a t i n g d a i r y cows a re n o t u s u a l l y met by f o r a g e s o r g r a i n s a l o n e , so t h e s e a n i m a l s g e n e r a l l y r e q u i r e e x t r a s u p p l e m e n t a t i o n of t h e element. Phosphorus d e f i c i e n c y i n r u m in a n ts- Symptoms of phosphorus d e f i c ie n c y in rum inants are n o n - s p e c i f i c , except perhaps for 53 osteophagia (craving concentrations. for bones) and subnormal blood serum Once t h e serum phosphorus v a l u e s have d e c l i n e d i n a n im a l s fed phosphorus d e f i c i e n t d i e t s , a d e c l i n e i n a p p e t i t e and feed e f f i c i e n c y i s o b s e r v e d . Animals s t a r t showing s i g n s o f d e p ra v e d a p p e t i t e , o r p i c a , c r a v i n g abnorm al m a t e r i a l s such as bones, wood, and s o i l . T h is symptom, however, i s n o t s p e c i f i c t o p h o s p h o r u s d e f i c i e n c y , s i n c e i t h a s b e en o b s e r v e d i n a n i m a l s s u f f e r i n g from l a c k o f sodium and p o tas siu m , and sometimes when p r o t e i n o r e n e r g y a r e d e f i c i e n t i n t h e d i e t (Underwood, 1981). With phosphorus d e f i c i e n c y , low and they become f r a g i l e . t h e m i n e r a l c o n t e n t o f t h e bones i s A p p e t i t e d e c l i n e s , growth r a t e i s r e t a r d e d , and feed u t i l i z a t i o n e f f i c i e n c y i s reduced. phosphorus d e f i c i e n c y , In chronic t h e anim al sometimes becomes s t i f f in the j o i n t s (NRC, 1978). One o f t h e most im p o r t a n t e f f e c t s of phosphorus d e f i c i e n c y i s on r e p r o d u c t i o n . F e r t i l i t y prob lem s were o b s e r v e d i n a d a i r y herd when t h e h e i f e r s were fed a d i e t i n s u f f i c i e n t in phosphorus. The d i e t c o n s i s t e d o f a l f a l f a , pasture. c o r n s i l a g e and l e g u m e - g r a s s I t was e s t i m a t e d t h a t t h e a n i m a l s w ere e a t i n g from 70 t o 80% o f t h e i r p h o s p h o r u s r e q u i r e m e n t . When t h e a n i m a l s were o f f e r e d f r e e c h o ic e d i c a l c i u m p h o s p h a t e , r e p r o d u c t i v e p a ra m eter s i n t h e herd improved. S e r v i c e s p e r c o n c e p ti o n d e cr ea se d from 2.8 t o 1 . 3 , t h e 30 day c o n c e p t i o n r a t e i n c r e a s e d from 33 t o 73%, and th e 60 t o 90 day c o n c e p t i o n r a t e i n c r e a s e d from 36 t o 76%. T heir a v e r a g e b l o o d serum c o n c e n t r a t i o n o f phosphorus i n c r e a s e d from 3.9 mg/100 ml b e f o r e s u p p l e m e n t a t i o n to 6.0 mg/100 ml when d i c a l c i u m p h o s p h a t e was a v a i l a b l e a t a l l t i m e s (Morrow, 1969). 54 In A u s t r a l i a (Scharp, superphosphate to the 1979), drinking ad d itio n of water an i n f e r t i l e of d eflu o rin ated herd i n c r e a s e d t h e f i r s t s e r v i c e p r e g n a n c y r a t e from 36.5 t o 63.2%, t h e mean c a l v i n g t o c o n c e p t i o n i n t e r v a l d e c r e a s e d from 109 days to 85 d a y s and the n u m b e r o f cows c u l l e d i n f e r t i l i t y f e l l from 15 t o 5. each y e ar for Other experiments have f a i l e d to i m p r o v e f e r t i l i t y by p h o s p h o r u s s u p p l e m e n t a t i o n ( C a l l e t a l . , 1978; C a r s t a i r s e t a l . , 1980; C a r s t a i r s e t a l . , 1981; De Boer e t a l . ,1 981). Sources o f p hosp horus- Among s e v e r a l so u r c e s o f phosphorus f o r r u m in a n ts , t h e most commonly used a r e bone m e a l s , monocalcium and d i c a l c i u m phosphates, d e flu o rin ated def lu o r in a te d superphosphate, p h o sp h a te s (Hillman e t a l . , phosphate rock, and m o n o s o d i u m a n d d i s o d i u m 1983). A l l t h e s e s o u r c e s have high phosphorus a v a i l a b i l i t y f o r ru m in ants. The s t a r t i n g m a t e r i a l f o r a lm o s t a l l f ee d ph o sph a tes i s pho sp ha te rock. ch em ically processed T h is m a t e r i a l c o n t a i n s 13 t o 14% p h o s p h o r u s and 3 t o 4% f l u o r i d e (Thompson, 1980 ). Fluoride i s t o x i c t o a n i m a l s ( S u t t i e and K o l s t a d , 1977; H i l l m a n , 1979; S u t t i e , 1980; Ammerman, 1980; Shu p e, 198 0), c a u s i n g d e n t a l and s k e l e t a l l e s i o n s and, i n s e v e r e c a s e s , a d v e r s e l y i n f l u e n c e s t h e p r o d u c t i v e performance of d om estic a n im a l s . Because of t h i s , t h e A s s o c i a t i o n o f American Feed C o n t r o l O f f i c i a l s (AAFCO, 1979) s e t s t a n d a r d s f o r s a f e l e v e l s of f l u o r i d e in fee d p h o s p h a t e s . Since 1952, any p r o d u c t s o l d t o t h e f e e d i n d u s t r y a s " d e f l u o r i n a t e d phosphate" has t o have a phosphorus t o f l u o r i n e r a t i o of a t l e a s t 100:1 (Thompson, 1 9 8 0 ). 55 P o ta ssiu m Po ta ssium c o n te n t of p l a n t s in r e l a t i o n to s o i l s t a tu s fertilizatio n - In r e l a t i o n to other n u trie n ts, and potassium is r e q u i r e d i n f a i r l y l a r g e amounts by both p l a n t s and a n im a l s (U.S. P lan t, S o il, potassium and N u t r i t i o n Lab. S t a f f , in the so il concen tratio n in crops. has a d i r e c t i n c r e a s i n g t h e y i e l d o f t h e c ro p. are used The l e v e l o f e f f e c t on t h e p o t a s s i u m Potassium f e r t i l i z a t i o n in c re a s e s the potassium c o n te n t of the p l a n t , fertiliz er 19 65). to b u t h a s a g r e a t e r e f f e c t on When l a r g e amounts o f n i t r o g e n increase y ield s, large p o t a s s i u m a r e r e m o v e d from t h e s o i l by t h e c r o p . amounts of When t h e s o i l i s f e r t i l i z e d w ith n i t r o g e n w ith o u t p r o p o r t i o n a l i n c r e a s e s in potassium , the potassium c o n te n t of fo rag e s tends to decrease. I n g e n e r a l , h e a v y p o t a s s i u m f e r t i l i z a t i o n d e c r e a s e s magnesium c o n t e n t in p a s t u r e s (B o lto n , 1978; Penny e t a l . , 1980; Penny and Widdowson, 1980). Potassium c o n t e n t i n f o r a g e s - There i s a l a r g e v a r i a t i o n of the p o t a s s i u m c o n t e n t i n p a s t u r e s , due t o p otassiu m f e r t i l i z a t i o n and so il sta tu s. G rasses ty p ic a lly c o n ta in 1.2 t o 2.8% p o ta s siu m , w ith low v a l u e s o f l e s s t h a n 1.0% and high v a l u e s of more t h a n 3.0%. Potassium c o n c e n tra tio n in legumes u s u a l l y r a n g e s from 1.5 t o 2.2%, w i t h v a l u e s fo u n d l o w e r t h a n 0.4% and h i g h e r than 3.0% (Church and Pond, 1974). M ichigan Corn s i l a g e samples in i n 1 9 7 5 - 1 9 7 6 a v e r a g e d 1.04% p o t a s s i u m on d r y m a t t e r b a s i s ( H i l l m a n and F o x , 1 977). Ear c o r n i n P e n n s y l v a n i a , from 1969 t o 1973, had an a v e r a g e o f 0.49% p o ta s siu m , and s h e l l e d corn 0.42% (Adams, 1975). Soybean o i l meal has a po tassiu m c o n t e n t of 56 a b o u t 2.21%. B r e w e r s g r a i n s h a v e a v e r y low p o t a s s i u m c o n t e n t : a b o u t 0.09% o f t h e d r y m a t t e r (NRC, 19 78). Young, v e r y l u s h f o r a g e s i n h i g h l y f e r t i l i z e d s o i l s ( e s p e c i a l l y t h o s e t r e a t e d with p o t a s s i u m ) i n c o o l w e a t h e r may be e x t r e m e l y h i g h i n p o t a s s i u m , o ften about th ree p e rc e n t of the dry m a tte r . P otassium c o n c e n t r a t i o n d e c r e a s e s w i t h a d v a n c i n g m a t u r i t y of f o r a g e s and can be reduced f u r t h e r by l e a c h i n g of mature s t a n d i n g f o r a g e s in humid a r e a s (NRC, 1978). Potassium requirements of dairy c attle- The potassium req u ire m e n t f o r d a i r y cows i s a b o ut 0.8% o f t h e dry m a t t e r in th e r a t i o n (Dennis e t a l . , 1976; Erdman e t a l . , 1980). Other a u t h o r s recommend 0.8 t o 1.0% f o r l a c t a t i n g d a i r y a n i m a l s (Underwood, 1981). A p p a r e n t l y t h e r e q u i r e m e n ts a r e s i m i l a r f o r o t h e r d a i r y cattle (NRC, 1978). Potassium d e f i c i e n c y and t o x i c i t y i n r u m in a n ts r e l a t i v e l y s e v e r e p o ta s s iu m d e f i c i e n c i e s dry m atter of the r a tio n ) Symptoms of (0.06 and 0.15% of the i n l a c t a t i n g cows i n c l u d e a marked d e c re a se in feed i n t a k e , reduced w eight g a in s , d ecreased m ilk production, p ica, l o s s of h a ir g l o s s i n e s s , decreased p l i a b i l i t y of h i d e s , lower plasma and m i l k p o t a s s i u m , and h i g h e r h e m a to c r i t readings. W ith b o r d e r l i n e p o t a s s i u m d e f i c i e n c y (0.45-0.55% o f t h e dry m a t t e r of t h e r a t i o n ) , t h e most n o t i c e a b l e s i g n i s lower feed consumption (NRC, 1978). Excess p otassiu m in the d i e t i s d e t r i m e n t a l fo r a n im als. B u l l c a l v e s fe d 6% p o ta s s iu m added t o t h e d i e t had d e c r e a se d feed i n t a k e and d e c r e a s e d w eight g a i n s . which p r o d u c e d no c l i n i c a l The maximum d i e t a r y potas sium effect was b e tw e e n 2.8 and 7% 57 (Neathery e t a l . , 1980). High l e v e l s of potassium i n th e d i e t of r u m i n a n t s d e c r e a s e magnesium a b s o r p t i o n which c a n r e s u l t in magnesium t e t a n y ( S u t t i e and F i e l d , 1969; F i e l d , 1970a and b; G r e e n e e t a l . , 1 9 8 3 a , b , and c ) . Potassium sources- potassium fo r rum inants The m o st commonly u s e d s o u r c e o f is potassium ch lo rid e, but o th er p o tassium s a l t s such as a c e t a t e , c a r b o n a t e and b i c a r b o n a t e can be used (Neathery e t a l . , 1980). Potassium b i c a r b o n a t e can a l s o be u s e d a s a b u f f e r i n g a g e n t t o p r e v e n t low m i l k f a t syndrome i n l a c t a t i n g d a i r y cows (Emery and Brown, 1961; S t o u t e t a l . , to p r e v e n t l a c t i c a c i d o s i s in beef c a t t l e a llev ia te feedlots (Horn, 1 9 7 9 ), o r t o t h e e f f e c t s o f s h i p p i n g on c a l v e s (Hutchenson e t a l . , 1972), transported to 1984). Sodium Sodium c o n ten t fe r tiliz a tio n - in p l a n t s in r e l a t i o n to s o i l statu s and In sodium d e f i c i e n t s o i l s , sodium f e r t i l i z a t i o n in c r e a se s crop y i e l d s and r a is e s the sodium concen tration o f the p la n t . This e f f e c t i s p a r t i c u l a r l y c le a r when potassium i s a l s o d e f i c i e n t in the s o i l . Sodium conten t in rye g r ass was increased from 0.15 to 0.20%, a s lo n g as 7.5 y e a r s a f t e r th e l a s t sodium a p p l i c a t i o n (B o lto n and Penny, 1978). I t would be d i f f i c u l t , h o w ev er, to add sodium to s o i l s in amounts s u f f i c i e n t t o r a i s e th e so d iu m c o n t e n t o f r e q u ir e m e n ts o f a n i m a l s . f o r a g e s e n o u g h t o m eet t h e so d iu m T h is i s b e c a u se s o i l s h ig h in sodium are v e r y poor s o i l s fo r p l a n t grow th. r e s p o n s i b l e fo r th e low f e r t i l i t y An e x c e s s o f sodium i s and u n d e s i r a b l e p h y s i c a l p r o p e r t i e s o f th e " a l k a l i s o i l s " o f dry r e g i o n s (U.S. P l a n t , 58 S o il, and N u t r i t i o n fe rtiliz a tio n Lab. decreases S taff, the 1965). Heavy potassium sodium c o n c e n t r a t i o n in p l a n t s (Underwood, 1981 ). Sodium content in forages- F o r a g e s , and f e e d s i n g e n e r a l , have low sodium c o n t e n t s . Sunflower (He l i an t h u s sp.) meal i s one o f t h e few f e e d s w i t h a r e l a t i v e l y h i g h so dium c o n t e n t (1.30%) (NRC, 197 8). Legumes i n P e n n s y l v a n i a from 1969 t o 1973 had an a v e r a g e so d iu m c o n c e n t r a t i o n o f 0.024%, g r a s s e s 0.014%, c o r n s i l a g e 0.005%, e a r c o r n 0.007%, and s h e l l e d c o r n 0.003% (Adams, 1975). So y b e a n o i l m e a l h a s a so dium c o n c e n t r a t i o n o f a b o u t 0.31% (NRC, 1978 ). Sodium requirem ents of d airy c attle- The NRC (1978) e s t i m a t e o f t h e sod ium r e q u i r e m e n t o f l a c t a t i n g cows i s 0.18% (0.46% so d iu m c h l o r i d e ) o f t h e d r y m a t t e r i n t h e r a t i o n . For n o n l a c t a t i n g d a i r y c a t t l e t h e e s t i m a t e d sodium r e q u i r e m e n t i s 0.10% (0.25% so d iu m c h l o r i d e ) o f t h e d r y m a t t e r i n t h e r a t i o n (NRC, 19 78). Sodium deficiency and to xicity in ru m in a n ts - d e f i c i e n c y can g r e a t l y d e c r e a s e t h e performance o f c a t t l e . Sodium The d e f i c i e n c y i s c h a r a c t e r i z e d by a d e c l i n e i n sodium c o n c e n t r a t i o n in t h e s a l i v a and u r i n e and an i n c r e a s e i n t h e potas sium l e v e l s in th ese f l u i d s (Loosli, 1978). When a d i e t s e v e r e l y d e f i c i e n t i n sod iu m i s f e d t o d a i r y cows an i n t e n s e c r a v i n g f o r s a l t and p i c a , m a n i f e s t e d by l i c k i n g and c hew ing v a r i o u s o b j e c t s , can o c c u r w i t h i n two weeks. O t h e r symptoms, w h ic h may n o t d e v e l o p f o r s e v e r a l months (the l e n g h t of time take n i s r e l a t e d t o l e v e l of m ilk p ro d u c tio n ), i n c lu d e d ecrea se d or l o s s of a p p e t i t e , 59 u n t h r i f t y haggard a p p e a ra n c e , l u s t e r l e s s eyes, decreased m ilk p ro d u ctio n , growing a n i m a l s , sh iv erin g , death. and r a p i d reduced g a in s ). incoordination, rough h a i r c o a t , l o s s of w eight (or in T e r m i n a l symptoms i n c l u d e weakness, card iac arrythm ia, and With adeq uate s a l t s u p p l e m e n t a t i o n cows r e c o v e r q u i c k l y and c o m p l e t e l y (NRC, 1978). C a t t l e a r e a b l e t o t o l e r a t e a r e l a t i v e l y high l e v e l o f s a l t i n t h e d i e t , e s p e c i a l l y when w a t e r i s r e a d i l y a v a i l a b l e . In c o n t r a s t , t h e s a l t c o n t e n t i n water r e q u i r e d t o produce t o x i c i t y i s much l o w e r t h a n t h e c o n t e n t r e q u i r e d i n f e e d . The amount o f s a l t t h a t can be t o l e r a t e d by l a c t a t i n g d a i r y cows has n o t been c le a r l y established. However, i t i s su g g e s t e d t h a t s a l t (sodium c h l o r i d e ) n o t exceed f i v e p e r c e n t of t h e t o t a l d r y m a t t e r i n t a k e (NRC, 197 8 ). S a l t p o i s o n i n g c a n o c c u r when a n i m a l s de p en d on s a l i n e w a t e r s o u r c e s , o r when a s u d d e n c h a n g e t o s a l i n e w a t e r from f r e s h w ater has o c c u r r e d . Excessive ingestion follow ing a p e rio d of s a l t d e p r i v a t i o n has r e s u l t e d in d e a th s of c a t t l e . P o is o ning has o c c u r r e d as a r e s u l t o f e x c e s s i v e s a l t i n p r e p a r e d fee d. C e n t r a l n e rv o u s system and d i g e s t i v e t r a c t derangement a r e the f e a t u r e s o f a c u t e s a l t p o i s o n i n g i n c a t t l e (S a nd als, Sodium sources- 1578). The m o st common and c h e a p e s t s o u r c e of sodium f o r ru m in ants i s sodium c h l o r i d e , b u t o t h e r s a l t s such as sodium c a r b o n a t e or sodium b i c a r b o n a t e can a l s o be used. Sodium b i c a r b o n a t e i s used a s a b u f f e r i n g a g e n t t o p r e v e n t low m il k f a t synd rome i n d a i r y cows (Emery and Brown, 1961; Emery e t a l . , 1964). in Sodium c h l o r i d e c a n be i n c l u d e d the concentrate form ula a n d /o r fed t o the a n im a l s ad l i b i t u m in a b l o c k of s a l t 60 o r i n g r a n u l a r fo rm i n a m i n e r a l feeder. Cows consume more g r a n u l a r o r l o o s e s a l t t h a n b l o c k s a l t , bu t the i n t a k e s o f b l o c k s a l t a re ad eq u a te t o meet th e needs o f l a c t a t i o n (NRC, 1978). T race m i n e r a l s , such as i o d i n e , z i n c , manganese, i r o n , c o p p e r, c o b a l t , and sometimes se l e n i u m a r e u s u a l l y added t o t h e s a l t f o r d a iry c a ttle or o th e r types of an im als. V oluntary s a l t consumption by c a t t l e i s v a r i a b l e , b u t l a c t a t i n g d a i r y cows have an a v e r a g e c o n s u m p t i o n o f 45 g p e r d a y . Dry cows and h e i f e r s consume from 15 t o 30 g o f s a l t p e r day (Crampton and H a r r i s , 1969 ). T h e s e f i g u r e s s h o u l d be t a k e n i n c o n s i d e r a t i o n when c a l c i u m and phosphorus s o u r c e s a r e added t o s a l t f o r ad l i b i t u m consumption by the a n i m a l s . Magnesium Magnesium c o n c e n t r a t i o n i n p l a n t s i n r e l a t i o n t o s o i l s t a t u s and f e r t i l i z a t i o n - Magnesium f e r t i l i z a t i o n tends t o i n c r e a s e t h e c o n c e n t r a t i o n o f mag nesium i n f o r a g e s . Y ie ld s of re sp o n siv e c r o p s a l s o i n c r e a s e a f t e r magnesium f e r t i l i z a t i o n t o magnesium d eficien t s o ils ( B o l t o n and P e n n y , 1978). On c e r t a i n c o a r s e - t e x t u r e d s o i l s , t h e u s e o f magnesium f e r t i l i z e r s o r d o l o m i t i c lim estone has been c o n c e n tr a tio n in th e effectiv e grass. in T his s u c c e s s f u l on f i n e r t e x t u r e d s o i l s . i n c r e a s i n g t h e magnesium p rac tic e has been less G r a s s e s t e n d t o h a v e low magnesium c o n c e n t r a t i o n s i n p e r i o d s o f a c t i v e growth, e s p e c i a l l y in the sp rin g fertilizatio n (S co tt, 19 72) and after heavy potassium (Allaway, 1971). Magnesium c o n ten t in fo ra g e smore magnesium than do g r a s s e s . Legumes n e a r ly always co n ta in Although the magnesium l e v e l s in 61 p l a n t s can be i n c r e a s e d m o d e r a te ly by add ing magnesium t o the s o i l , the magnesium l e v e l in g r a sse s i s s t i l l below th a t in most le g u m e s , e v e n when th e g r a s s e s a r e grown on a s o i l h ig h in a v a i l a b l e magnesium (U.S. P la n t , S o i l , and N u tr itio n Lab. S t a f f , 1965). Magnesium c o n t e n t in g r a s s e s r a n g e s from 0.12 t o 0.26%, w ith v a l u e s found lo w e r than 0.1% and h ig h e r than 0.3%. In leg u m es th e t y p i c a l magnesium c o n c e n t r a t i o n ra n g e s from 0.3 to 0.4%, w it h v a l u e s found lo w e r than 0.1% and h ig h e r than 0.6% (Church and Pond, 1974). Corn s i l a g e samples in Michigan had an average magnesium c o n ten t o f 0.24% during the years 1975 and 1976 (Hillman and Fox, 1977). In P en nsylvan ia during the years 1969 t o 1 9 7 3 , ear c o rn had a v e r a g e 0.12% magnesium, and s h e l l e d corn a l s o had 0.12% magnesium on a dry m atter b a s i s (Adams, 1975). Soybean o i l meal has an average magnesium con ten t o f 0.30% (NRC, 1978) . Magnesium requirements of dairy c attle- The magnesium re q u i r e m e n t o f d a i r y c a l v e s on a d i e t of m il k r e p l a c e r and c a l f s t a r t e r c o n c e n t r a t e mix i s 0.07% o f t h e d ry m a t t e r of the r a t i o n . Growing h e i f e r s and b u l l s , m a t u r e b u l l s and d r y p r e g n a n t cows r e q u i r e 0.16% magnesium on a d r y m a t t e r b a s i s . The magnesium r e q u i r e m e n t o f l a c t a t i n g d a i r y cows i s 0.20% o f t h e r a t i o n ' s dry m atter. Under c o n d i t i o n s c onducive t o g r a s s t e t a n y (i.e. most of t h e f e e d comes from l u s h , h i g h l y f e r t i l i z e d p a s t u r e s i n c o o l seas on s) i n h ig h p rod u cin g l a c t a t i n g cows, 0.25% o r more d i e t a r y magnesium i s s u g g e s t e d (NRC, 1978). Magnesium d e f i c i e n c y and t o x i c i t y in ruminants- Animals fed magnesium d e f i c i e n t d i e t s show a s t i f f g a i t and gradual l o s s o f 62 condition d eclin e for several weeks, in m ilk y i e l d . w ith o u t l o s s of a p p e t i t e or a T his c o n d itio n c a n be f o l l o w e d by r e c o v e r y i f some form o f magnesium i s p r o v i d e d , o r by t e t a n y and death. T his c o n d it i o n magnesium t e t a n y is u su ally (Underwood, known a s g r a s s 1 9 81). Experim ents t e t a n y or show t h a t m o r t a l i t y i s o f t e n h i g h , e v e n when t h e a n i m a l s a r e r e c e i v i n g d i e t s t h a t a r e o n l y m a r g i n a l l y d e f i c i e n t i n magnesium and where growth o f t h e s u r v i v o r s may approach t h a t o f t h e c o n t r o l a n im a l s . P l a s m a magnesium l e v e l s a r e d e p r e s s e d m a r k e d l y by magnesium d e fic ie n cy (Scott, 1972). Animals showing sumptoms of magnesium t e t a n y s h o u l d be g i v e n p a r e n t e r a l magnesium i m m e d i a t e l y . To p r e v e n t a r e c u r r e n c e o f t h e c o n d i t i o n , a n i m a l s s h o u l d be f e d a d i e t h i g h e r i n mag nesium. U su a lly a fo llo w -u p treatm ent th a t c o n s i s t s of 60 g of magnesium ox ide p e r day f o r a t l e a s t a week, and t h e n w i t h d r a w n g r a d u a l l y , i s g i v e n t o t h e a n i m a l s t h a t had grass tetany (Merck, 1979). Magnesium t o x i c i t y i s not known to be a p r a c t i c a l problem in dairy c a t t l e . Male H o ls t e in c a l v e s s t a r te d showing diarrhea with magnesium (as magnesium o x id e ) l e v e l s h ig h e r than 0.7% o f the d i e t ( Q u illia m e t a l . , 1980 ). In an o th er e x p e r im e n t, H o l s t e i n b u l l c a l v e s had diarrhea but not reduced weight g ain s when fed a d i e t con tain in g 1.0% magnesium as magnesium oxide. L e v e ls o f 2.0 and 4.0% magnesium produced d ia r r h e a and reduced w e ig h t g a i n s (Gentry e t a l . , 197 8). Magnesium magnesium fo r sou rcesrum inan ts The most commonly used s o u r c e o f is magnesium o x i d e . in c lu d e magnesium s u l f a t e and magnesium carbonate. Other sou rces Magnesium in 63 dolomite is poorly utilized (Thompson, 1978). Magnesium o x i d e , a t a l e v e l o f a p p r o x im a t e ly 0.5% o f th e d i e t , a l o n g w ith sodium or p o ta s siu m b i c a r b o n a t e , i s used a s an a l k a l i n i z i n g agent to p reven t low m ilk f a t syndrome in l a c t a t i n g d a ir y cows (Emery e t a l . , 1965; J e s s e e t a l . , 1981 ). Copper and Molybdenum Copper and molybdenum con ten t in p l a n t s in r e l a t i o n to s o i l s t a t u s and f e r t i l i z a t i o n - Copper and molybdenum c o n cen tra tio n in p l a n t s i s r e s p o n s i v e t o f e r t i l i z a t i o n w ith t h e s e two e l e m e n t s . P la n t s p e c ie s vary c o n sid e r a b ly M it c h e ll e t a l . v a r ia tio n s in t h e i r uptake o f co p p er. (1956), quoted by Hodgson e t a l . from 1.7 t o 12.3 ppm o f copper (1962), observed in c l o v e r , w h ile g r a sse s growing with the c lo v e r varied o n ly from 2.0 to 4.3 ppm. In A u s t r a lia and New Zealand the a d d itio n o f copper f e r t i l i z e r to s o i l s has been e f f e c t i v e in meeting the needs o f both the p la n t and th e g r a z in g a n im a l. On some copper d e f i c i e n t s o i l s o f th e United S ta te s a p p lic a t io n s o f copper f e r t i l i z e r s have increased p l a n t growth w it h o u t p r od u cin g a marked change in t h e copper con ten t o f the p l a n t s , and anim als grazing th ese p l a n t s may s t i l l s u f f e r from copper d e f i c i e n c y (U.S. P l a n t , S o i l , and N u t r i t i o n Lab. S t a f f , 1965). k g /h e c ta r e (a b o u t C opper 1 .8 c o n c e n t r a t i o n o f copper fe r tiliz a tio n lb /a c r e ) r e su lte d in le g u m e s , at a ra te in of 2 in c r e a se d g r a s s e s and weeds in a permanent p a s t u r e near A berdeen, E n glan d. The a v e r a g e copper c o n c e n t r a t i o n w it h o u t f e r t i l i z a t i o n was 4.84 ppm, and 5.69 ppm a f t e r copper f e r t i l i z a t i o n (Forbes and Gelman, 1981). Molybdenum con ten t in legumes in the United S t a t e s goes from 64 an a v e r a g e o f 6 ppm i n t h e w e s t t o a r o u n d 0.5 ppm i n t h e E a s t . The p a t t e r n roughly p a r a l l e l s so il c h a n g e s from n e u t r a l to a l k a l i n e ( o f te n c a l c a r e o u s ) s o i l s i n t h e w e ste r n U nited S t a t e s t o p r e d o m i n a n t l y a c i d s o i l s i n t h e e a s t (Kubota, 1976). fertiliz e rs a re m o s t ly used in a c id molybdenum. In a c i d s o i l s molybdenum f e r t i l i z e r becomes r a p i d l y u n a v a ila b le to the p l a n t , so ils that Molybdenum so t h e r e i s l i t t l e are low i n danger of high molybdenum c o n t e n t in f o r a g e s f e r t i l i z e d with t h e e le m e n t under these conditions. There a r e , however, some a c i d s o i l s w ith high m olybdenum c o n c e n t r a t i o n s . When t h e s e molybdenum becomes a v a i l a b l e f o r t h e p l a n t . so ils are lim ed, In these cond itio ns, l e g u m e s i n p a r t i c u l a r , c a n c o n t a i n t o x i c am ounts o f molybdenum (Hodgson e t a l . , 1 9 6 2). Copper and molybdenum c o n t e n t i n f o r a g e s - Copper c o n t e n t in g r a s s e s goes from around 4 t o 8 ppm, w ith v a l u e s found lower than 3 ppm and h i g h e r t h a n 10 ppm. In a l f a l f a , ty p ical copper c o n c e n t r a t i o n s a r e from 6 t o 12 ppm, w ith v a l u e s found lower th an 4 ppm and h ig h e r than 15 ppm (Church and Pond, 197 4). Corn s i l a g e in Michigan in 1975 and 1976 had an average copper conten t o f 9 ppm (Hillman and Fox, 1977). Soybean o i l meal has an average copper c o n t e n t o f around 40 ppm (NRC, 1978). In P e n n s y l v a n i a from 1969 t o 19 73, c orn s i l a g e had an a v e r a g e copper c o n t e n t o f 8.1 ppm. V alu es as low as 2.0 ppm o f copper were a l s o found. In t h e same s t a t e , ear corn had an a v e r a g e o f 4.7 ppm c o p p e r , and s h e l l e d corn 3.6 ppm (Adams, 1975). In B r it i s h Columbia, Canada, legum e hay had 7.2 ppm copper on th e a v e r a g e , g r a s s hay 4.5 ppm, and co rn s i l a g e 4.5 ppm (M iltm ore e t a l . , 1970). In A l b e r t a , 65 Canada, copper c o n t e n t s i n f o r a g e s were h i g h e r : 12 ppm i n g r a s s r o u g h a g e , 11 ppm i n le g u m e r o u g h a g e , and 12 ppm i n g r a s s legum e roughage (Redshaw e t a l . , 1978). Molybdenum i n g r a s s e s ranges from 0.5 t o 3.0 ppm, w i t h v a l u e s fo u n d l o w e r t h a n 0.4 ppm and h i g h e r t h a n 5.0 ppm. In a l f a l f a , molybdenum c o n c e n t r a t i o n s v a r y from 0.5 t o 3.0 ppm, w i t h v a l u e s fo u n d l o w e r t h a n 0.2 ppm and h i g h e r t h a n 5.0 ppm (Church and P o n d, 1 974). calcareo u s, I n some a r e a s , e s p e c i a l l y when t h e s o i l s a r e p astu res can h a v e e x t r e m e l y h i g h m olybdenum c o n c e n t r a t i o n s , r a n g in g from 20 t o 100 ppm (Underwood, 1981). Copper requirements of d airy c a t t l e - Copper req u ir e m e n ts a r e d e p e n d e n t on s e v e r a l f a c t o r s , s u c h a s t h e molybdenum and s u l f a t e i n t a k e o f t h e a n i m a l s and w h e t h e r o r n o t t h e a n i m a l i s grazing. Grazing a n i m a l s seem t o have h i g h e r copper req u ir e m e n ts t h a n n o n g r a z i n g a n i m a l s (NRC, 1 9 7 8 j. Under some c o n d i t i o n s , 4 ppm of copper i n th e d i e t a r e enough t o meet the r e q u i r e m e n ts of dairy c a t t l e , b u t 10 ppm o r more a r e n e e d e d when t h e f o r a g e s c o n t a i n h i g h c o n c e n t r a t i o n s o f molybdenum or o t h e r i n t e r f e r i n g s u b s t a n c e s (NRC, 1 9 78 ). C a t t l e g r a z i n g p a s t u r e s w i t h a r o u n d 10 ppm copper and 1.6 ppm molybdenum showed symptoms of hypocupremia (G i v e n s and H o p k i n s , 1978). S u p p l e m e n t a t i o n o f c o p p e r , t h r o u g h c o p p e r i n j e c t i o n s , t o g r a z i n g H o l s t e i n h e i f e r s w i t h low c o p p e r b lo o d plasm a c o n c e n t r a t i o n s i n c r e a s e d th e l e v e l s of copper in b l o o d a l t h o u g h g r o w t h was n o t a f f e c t e d d u r i n g t h e f o u r - m o n t h p e r i o d o f t h e e xp erim en t (Givens e t a l . , 1981). I n an e f f o r t t o a c c o u n t f o r s u b s t a n c e s t h a t i n t e r f e r e w i t h copper a v a i l a b i l i t y , S u ttle and M c L a u c h la n (1976), in G re at 66 B rita in , developed an e q u a t i o n to c a l c u l a t e tru e copper a v a i l a b i l i t y (TA Cu), as f o l l o w s : l o g TA Cu = - 0 . 0 0 1 9 Mo - 0.0755 S - 0.0131 Mo X S - 1.153 Mo and S i n t h e a b o v e e q u a t i o n a r e t h e c o n c e n t r a t i o n s o f molybdenum (ppm) and s u l f u r ration. (g /k g ) in the dry m a tte r of the The c a l c u l a t e d v a l u e s o f t r u e copper a v a i l a b i l i t y a r e m u l t i p l i e d by the copper c o n t e n t o f t h e r a t i o n and compared with d i e t a r y requirem ents of a v a i l a b l e copper t h a t are as fo llo w s: 0.48 ppm f o r g r o w i n g c a t t l e w i t h l i v e w e i g h t s o f 100 t o 200 kg, 0.42 ppm f o r g r o w i n g c a t t l e w i t h a l i v e w e i g h t o f 400 kg, and 0.41 ppm f o r d a i r y cows (Givens and Hopkins, 1978). T h e r e i s n o t good a g r e e m e n t on w h at i s a s a f e c o p p e r - t o molybdenum r a t i o in the d i e t of ru m in an ts. T his is p r o b a b ly because o t h e r f a c t o r s b e s i d e s molybdenum i n t e r f e r e w i t h c o p p e r m etab o lism , i n c l u d i n g s u l f a t e s and p r o t e i n and whether o r n o t th e a n im als are g ra z in g . G razing an im als a re l i k e l y to have h ig h er c o p p e r r e q u i r e m e n t s t h a n n o n g r a z i n g c a t t l e . Some a u t h o r s h a v e suggested a copper t o m olybdenum r a t i o of 2:1, some 4 : 1 (Underwood, 198 1). Under some c i r c u m s t a n c e s , h y p e r c u p r e m i a has been o b se r v e d even w i t h h i g h e r copper t o molybdenum r a t i o s , such as i n G re a t B r i t a i n w ith a 6.5:1.0 r a t i o ( G i v e n s and H o p k i n s , 1978). Copper deficiency and toxicity in r u m in a n ts- Copper d e f i c i e n c y in ru m in a n ts r e s u l t s i n reduced growth or weight l o s s , u n th riftin ess, deficien cy, observed: and d e c r e a s e d m i l k p r o d u c t i o n . often (but n o t severe diarrhea; in v ariab ly ) the I n an e x t r e m e fo llo w in g ra p id weight l o s s ; are c e s s a t i o n of 67 g r o w t h ; ro u g h h a i r c o a t ; a c h a n g e i n h a i r c o a t c o l o r , which may become f a d e d , b l e a c h e d , g r a y i n g , d i r t y - y e l l o w i s h (for w hite h a i r ) , or brownish (for b l a c k h a i r ) ; a change in h a i r t e x t u r e ; s w e l l i n g a t t h e end o f t h e pasterns; leg bones, e s p e c i a l l y above the f r a g i l e bones o f t e n r e s u l t i n g i n m u l t i p l e f r a c t u r e of r i b s , femur o r humerus; s t i f f j o i n t s t h a t may r e s u l t i n a "pacing g a i t " i n o l d e r c a t t l e ; d e p r e s s e d o r d e l a y e d e s t r u s and r e d u c e d r e p r o d u c t i o n ; d i f f i c u l t y i n c a l v i n g and r e t a i n e d p l a c e n t a ; birth of c a l v e s w ith c o n g e n i t a l r i c k e t s ; " f a l l i n g d i s e a s e " or sudden d e a t h due t o a c u t e h e a r t f a i l u r e ; and a n e m i a . Som etim es t h e b l a c k h a i r a r o u n d t h e e y e s l o s e s p i g m e n t and d e v e l o p s a g r a y s p e c t a c l e d appe ara nce t h a t i s a p p a r e n t l y i s s p e c i f i c f o r copper deficiency . With i n a d e q u a t e c o p p e r i n t a k e , p e r f o r m a n c e may be s u b n o r m a l when t h e r e a r e no o b v i o u s d e f i c i e n c y symptoms o t h e r th an n o n s p e c i f i c u n t h r i f t i n e s s (NRC, 1978). A c c o r d i n g t o Ward (1978), c o p p e r d e f i c i e n c i e s a r e produced by fo u r c l a s s e s of f e e d s : above 100 ppm; 2) less; 3) 1) high molybdenum f e e d s , generally low copper t o molybdenum r a t i o f e e d s : 2:1 or c o p p e r d e f i c i e n t f e e d s , b e l o w 5 ppm; and 4) p r o t e i n f e e d s , t h o s e 20 t o 30% p r o t e i n i n f r e s h f o r a g e form. high The a u th o r s p e c u l a t e s t h a t t h e l a t t e r s i t u a t i o n p r o b a b l y r e s u l t s from h i g h e r l e v e l s of s u l f i d e produced from s u l f u r amino a c i d s d u rin g rumen f e r m e n t a t i o n . Sheep are v e r y s u s c e p t i b l e t o copper p o i s o n i n g and h o r s e s r e l a t i v e l y t o l e r a n t t o high copper l e v e l s in the d i e t . B o v in es, in g e n e r a l , can t o l e r a t e h ig h e r amounts o f copper than sh eep w i t h o u t s h o w in g s i g n s o f t o x i c i t y . The amount o f c o p p e r 68 n e c e s s a r y t o c a u s e p o i s o n i n g d e p e n d s a l s o on t h e r e l a t i o n o f copper t o i n t e r f e r i n g s u b s t a n c e s such as molybdenum and s u l f a t e s . I t i s e s t i m a t e d t h a t c a t t l e can s a f e l y t o l e r a t e 70-100 ppm copper c o n t i n u o u s l y and h i g h e r l e v e l s f o r s h o r t p e r i o d s s u c h a s a few weeks (NRC, 1978). When e x c e s s i v e copper is c o nsum ed, c a ttle are a b le to a c c u m u l a t e e x t r e m e l y h i g h am o un ts i n t h e l i v e r b e f o r e o b v i o u s symptoms o f t o x i c i t y a p p e a r . The t o x i c i t y symptoms a r e due t o t h e sudden l i b e r a t i o n of l a r g e amounts o f copper from t h e l i v e r t o t h e b lo od c a u sin g a h e m o l y t i c c r i s i s . by c o n s i d e r a b l e h em olysis, This i s c h a r a c t e r i z e d j a u n d i c e , m ethem oglobinem ia, h e m o g l o b i n u r i a , g e n e r a l i z e d i c t e r u s , w i d e s p r e a d n e c r o s i s , and o f t e n d e a t h (NRC, 1978). C h r o n i c c o p p e r p o i s o n i n g may o c c u r i n f ar m a n i m a l s from n a t u r a l g r a z i n g c o n d i t i o n s where t h e c o p p e r c o n t e n t s herbage are e x c e s s iv e , in the o r a r e n o r m a l b u t a b n o r m a l l y low molybdenum and s u l p h u r c o n c e n t r a t i o n s ; from e x c e s s i v e consumption o f c o p p e r - c o n t a i n i n g s a l t l i c k s ; or from t h e unwise use o f copper d r e n c h e s (Underwood, 19 81). Copper sources- Cupric s u l f a t e , form CuS04.5H20 c o n t a i n i n g 25% c o p p er , u s u a l l y the pentahydrate i s t h e most commonly used form o f c o p p e r s u p p l e m e n t f o r r u m i n a n t s . Most t r a c e m i n e r a l s a l t s c a r r y c o pper, b u t u s u a l l y a t th e low l e v e l o f about 0.03% of the s a l t m ixture. In copper d e f i c i e n t a r e a s , s h o u l d c o n t a i n 0.5 t o 1.0% c u p r i c s u l f a t e which i s e q u i v a l e n t t o 0.125 t o 0.25% co pper. s a l t lic k s (Underwood, 1977); I f t h e d i e t of th e d a i r y cow i n a h y p o t h e t i c a l copper d e f i c i e n t a r e a c o n t a i n s 5 ppm 69 c o p p e r , and t h e cow i s e a t i n g 20 kg (44 l b ) o f d r y m a t t e r a d a y , a d a i l y i n t a k e o f 45 g of a t r a c e m i n e r a l s a l t with 0.25% c o pp er, w i l l r a i s e i t s copper i n t a k e i n t h e t o t a l d i e t t o an e q u i v a l e n t o f around 10 ppm c opper. T h is i n t a k e i s p r o b a b l y a dequate under m o st c i r c u m s t a n c e s . O t h e r c o p p e r c o n t a i n i n g compounds t h a t c a n be u s e d f o r ru m in ants i n c l u d e c u p r i c c a r b o n a t e , c u p r i c c h l o r i d e and c u p r i c n itrate, b u t copper i n t h e s e forms i s g e n e r a l l y l e s s a v a i l a b l e f o r t h e anim al (Ammerman and M i l l e r , 1978). I n j e c t a b l e forms of copper used f o r copper d e f i c i e n c y t h e r a p y a r e copper g l y c i n a t e , copper c a l c i u m e d e t a t e gluconate ( e t h y l e n e d i a m i n e t e t r a a c e t a t e ) , and copper (Underwood 1977). Copper f e r t i l i z a t i o n o f p a s t u r e s w i t h 5 t o 7 kg o f c o p p e r s u l f a t e p e r h e c t a r e (4 t o 6 l b / a c r e ) r a i s e s t h e copper c o n t e n t i n t h e f o r a g e s t o l e v e l s h i g h enough t o p r e v e n t d e f i c i e n c i e s . In sane a r e a s s i g n i f i c a n t i n c r e a s e s i n t o t a l herbage p r o d u c t i o n a r e c o i n c i d e n t a l l y a c h i e v e d (Underwood, 1977). Sulphur S u lp h u r content fertilizatio n - in p la n ts in r e l a t i o n to s o i l status and S u l f u r i s e s s e n t i a l f o r both p l a n t s and a n im a l s . S u l f u r d e f i c i e n c y i n p l a n t s i s e s p e c i a l l y common i n t h e g r a y wooded s o i l s o f c o o l , tem perate re g io n s . Many o f t h e s o i l s d e v e l o p e d from v o l c a n i c m a t e r i a l s i n n o r t h e r n C a l i f o r n i a and in t h e P a c i f i c Northwest a r e d e f i c i e n t i n s u l f u r (U.S. P l a n t , and use N u tritio n Lab. S taff, 1965). The of S oil, o rd in ary s u p e r p h o s p h a te , which c o n t a i n s 11-12% s u l f u r , p r o b a b l y a v o i d e d su lfu r d eficien cies in th e se a re a s . T rip le or c o n c e n t r a t e d 70 s u p e r p h o s p h a te , i n c o n t r a s t , has a l m o s t no s u l f u r (0 t o 1%), and i t i s p o s s i b l e t h a t i t s use may r e s u l t in s u l f u r d e f i c i e n c i e s in s u s c e p t i b l e c r o p s such as legumes. When s u l f u r f e r t i l i z e r s a r e a d d ed t o a s u l f u r - d e f i c i e n t so il, in creased crop y ield s and in creased to ta l su lfu r co n ce n tra tio n in the p l a n t norm ally r e s u l t . I n c r e a s e s in p r o t e i n c o n cen tratio n are a l s o f re q u e n tly observed. But t h e r a t i o o f the s u l f u r amino a c i d s t o o t h e r amino a c i d s w i t h i n th e t r u e p r o t e i n f r a c t i o n i s g e n e r a l l y unchanged. S u l f a t e , l i k e n i t r a t e , may acc umulate i n p l a n t t i s s u e s under c e r t a i n c o n d i t i o n s , b u t u n l i k e n i t r a t e e x c e s s s u l f a t e s i n p l a n t s a r e n o t t o x i c f o r th e anim al. The o n l y c o n c e r n w i t h h i g h l e v e l s o f s u l f a t e in fo rag e s for r u m i n a n t s i s i n t h e c a s e o f c o p p e r d e f i c i e n c y p r o d u c e d by h i g h l e v e l s o f molybdenum. S u l f a t e s can enhance th e d e f i c i e n c y . I n o r g a n i c s u l f u r , l i k e s u l f a t e , c a n be u s e d by t h e b a c t e r i a i n t h e rumen o f a n i m a l s t o p r o d u c e s u l f u r c o n t a i n i n g amino a c i d s . So, e v e n when a h i g h l e v e l o f s u l f a t e i s p r e s e n t i n f o r a g e s , i t u s u a l l y o n ly im proves the n u t r i t i o n a l q u a l i t y of the fo rag e (Allaway, 1971). S u lfu r con ten t in fo ra g es- T y p ic a l s u l f u r c o n t e n t in g r a s s e s g o e s from 0.15 t o 0.25%, w ith v a l u e s found low er than 0.1% and h ig h e r than 0.3%. In a l f a l f a the s u l f u r c o n t e n t i s h igh er, t y p i c a l l y ranging t y p i c a l l y from 0.3 to 0.4%, with v a lu e s found low er than 0.2% and h ig h e r 1974). than 0.7% (Church and Pond, Corn s i l a g e i s r e l a t i v e l y low in s u l f u r . 1975-1976, In Michigan in corn s i l a g e samples had an average s u lfu r conten t of 0.11% (H illm a n and F ox, 1 977). In P e n n s y l v a n ia from 1969 to 71 1973, t h e a v e r a g e s u l f u r c o n t e n t o f e ar c o rn was 0.13%, and 0.14% f o r s h e l l e d c o rn (Adams, 1975). Soybean o i l meal has an a v e r a g e o f 0.49% s u l f u r (NRC, 1978). Sulfur requirements of d a iry c a t t l e - U n l i k e nonr um in ants, w hic h t h a t h a v e a s p e c i f i c r e q u i r e m e n t f o r s u l f u r c o n t a i n i n g amino a c i d s , r u m i n a n t s c a n make u s e o f i n o r g a n i c s u l f u r i n t h e ration. B a c t e r i a and p r o t o z o a i n t h e rumen c a n s y n t h e s i z e t h e s u l f u r - c o n t a i n i n g amino a c i d s r e q u i r e d by th e ruminant s t a r t i n g from i n o r g a n i c s u l f u r . in relatio n n itro g en to the to s u l f u r S u l f u r r e q u i r e m e n ts a r e o f t e n c a l c u l a t e d nitro g en ratio co n cen tratio n of 10:1 t o appropriate for d airy c a t t l e . in the d i e t . 12:1 i s s u g g e s t e d A as The e s t i m a t e d s u l f u r re q u ir e m e n t f o r l a c t a t i n g d a i r y cows i s 0.20% i n t h e a v e r a g e d i e t ; t h a t f o r n o n l a c t a t i n g d a i r y c a t t l e i s c a l c u l a t e d from the minimum p r o t e i n re q u ir e m e n t with a n i t r o g e n t o s u l f u r r a t i o of 12:1 (NRC, 1978). Sulfur deficiency and toxicity in r u m in a n ts- In the p r a c t i c a l f e e d i n g o f d a i r y c a t t l e , a s u l f u r d e f i c i e n c y i s m ost lik ely t o o c c u r when c o n s i d e r a b l e ad ded n o n p r o t e i n n i t r o g e n and/or corn s i l a g e a re fed (NRC, 197 8 ). In th e s e c a se s the d e f i c i e n c y i s n o t s e v e r e , s i n c e th e o t h e r i n g r e d i e n t s o f t h e d i e t p r o v i d e scsne s u l f u r f o r t h e anim al. S u l f u r d e f i c i e n c y symptoms i n d a i r y c a t t l e a r e no t s p e c i f i c , e s p e c i a l l y when t h e d e f i c i e n c y i s no t s e v e r e . S u l f u r i s e s s e n t i a l f o r t h e th e s y n t h e s i s of m i c r o b i a l p r o t e i n , and th u s fo r optimum f e r m e n t a t i o n o f s u b s t r a t e s ( Q u i s p e , 198 2). d i s r u p t e d w ith s u l f u r d e f i c i e n t d i e t s . dry m atter d i g e s t i b i l i t y , Rumen m e t a b o l i s m i s This r e s u l t s i n d e c r e a s e d decreased dry m atter intak e, and 72 decreased m ilk production of d a iry c a t t l e 1 9 7 3 a , b and c ) . (Bouchard and Conrad, The r e q u i r e m e n t s o f t h e a n i m a l f o r i n o r g a n i c su lfu r, and t h e e f f e c t s o f a d e f i c i e n c y a r e n o t w e l l (Foil is , 1958). known The maximum amount of s u l f u r t h a t can be t o l e r a t e d by c a t t l e i s not w e ll defined. I t i s su g g e ste d t h a t t h e maximum s h o u l d be l i m i t e d t o a b o u t 0.35% p e r c e n t o f t h e d i e t w i t h no more t h a n 0.20% coming from added s u l f a t e s u l f u r . can to lerate a higher lev el of i n g r e d i e n t s th an from added s u l f a t e Sulfur sources- Apparently, d a iry c a t t l e su lfu r from n atu ral feed (NRC, 1978). S e v e r a l s o u r c e s , such as sodium s u l f a t e , p o t a s s i u m s u l f a t e , magnesium s u l f a t e , ammonium s u l f a t e , and c a l c i u m s u l f a t e , a r e e f f e c t i v e in meeting t h e s u l f u r re q u i r e m e n t of rum inants. efficien tly E l e m e n t a l s u l f u r i s a l s o u t i l i z e d b u t much l e s s (NRC, 1978). Iron Iron content fertilizers- in plants in r e l a t i o n to soil statu s and I r o n u p t a k e by t h e p l a n t from t h e s o i l d e p e n d s t o l a r g e e x t e n t on t h e p l a n t s p e c i e s and v a r i e t y . A l f a l f a and c o rn , f o r exam ple, t a k e more i r o n from t h e s o i l th a n soybeans, and w i l l pr oduce good y i e l d s i n s o i l s t h a t a r e i r o n d e f i c i e n t f o r soybeans (T isd ale et a l., 1985). In iron d e fic ie n t so ils, iron f e r t i l i z a t i o n i s l i k e l y t o i n c r e a s e c ro p y i e l d s , b u t n o t t h e ir o n c o n c e n t r a t i o n in t h e p l a n t (Allaway, 1971). Iron content of forages- Iron l e v e l s in forages are u s u a lly high enough t o meet t h e re q u ir e m e n ts of d a i r y a n i m a l s . Typical i r o n c o n c e n t r a t i o n i n g r a s s e s i s 50-100 ppm, w i t h v a l u e s found 73 than 45 ppm and h ig h e r than 200 ppm. lo w e r A lfa lfa 's ir o n co n c en tr a tio n ranges from 50 to 200 ppm, with v a lu e s found lower th an 30 ppm and h ig h e r than 300 ppm (Church and Pond, 1974). Corn s i l a g e in M ich igan in 1975 and 1976 hadan a v e r a g e o f 214 ppm ir o n i n th e dry m a tte r (H illm a n and Pox, 19 77). Ear corn in P en n sy lv a n ia from 1969 to 1973 had an average o f 94 ppm ir o n , and s h e l l e d co rn 69 ppm (Adams, 1975). Soybean o i l m eal has an average iron con ten t o f 130 ppm (NRC, 1978). Iron requirements of d a ir y c a t t l e - An i r o n l e v e l o f 100 ppm i n t h e d r y d i e t s h o u l d be adeq uate f o r a l l needs o f c a l v e s up to t h r e e m o n th s o f a g e ; c attle (NRC, 19 78). w i t h 50 ppm s u f f i c i e n t f o r o t h e r d a i r y About 30 t o 40 ppm i n the d iet in the p r o d u c t i o n of v e a l w i l l p r o v i d e s u f f i c i e n t i r o n t o p r e v e n t l o s s o f p e r f o r m a n c e from a s e v e r e d e f i c i e n c y and s t i l l m a i n t a i n t h e p a l e v e a l c o l o r ( M i l l e r , 1981). Iron deficiency and toxicity in rum in a n ts- Since most f o r a g e s have a d e q u a te l e v e l s of i r o n , i r o n d e f i c i e n c y seldom o c c u r s i n d a i r y c a t t l e u n l e s s as a r e s u l t of s e v e r e l o s s o f blood cau se d by p a r a s i t i c i n f e s t a t i o n s or d i s e a s e . Young a n im a l s a r e s u s c e p t i b l e t o i r o n d e f i c i e n c y when they a r e fed e x c l u s i v e l y on m ilk t h a t i s low i n i r o n c o n t e n t o f abo ut 0.5 m g / l i t e r (NRC, 1978). Cows m i l k h a s an i r o n (Thomas, 1970). Even though some f e e d s c o n t a i n a h ig h p e r c e n t a g e o f i r o n , t o x i c i t y d oes n o t appear t o be an im p o rtan t p roblem f o r d a i r y c a ttle . The e f f e c t s o f ir o n t o x i c i t y , which are n ot s p e c i f i c , in c lu d e lower feed in ta k e, le s s e n e d weight g a in s , and lower m ilk p r o d u c t io n . L im ite d d a ta s u g g e s t t h a t s o l u b l e ir o n compounds 74 such as s u l f a t e s a r e more t o x i c than i r o n i n n a t u r a l f e e d s t u f f s (M iller, 1981 ). It is believed that cattle g en erally can t o l e r a t e 1000 ppm d i e t a r y i r o n under most c o n d i t i o n s , e s p e c i a l l y i f the iron is from n a t u r a l fee d s o u r c e s and adequ a te l e v e l s other m inerals a r e s u p p l i e d (NRC, Iron sources- such as ferrous 1978). The a v a i l a b i l i t y compounds v a r i e s enormously. su lfate of of iro n in d i f f e r e n t G e n e r a l l y i r o n i n s o l u b l e compounds and ferric citrate are much more a v a i l a b l e t o c a t t l e th an i n f e r r i c ox ide or i r o n p h y t a t e ( M i l l e r , 1981). Feed g ra d e interm ediate ferrous a v aila b ility carb o n ates range from (Ammerman and M i l l e r , low 1978). to An im p o rta n t source of i r o n , as w e ll as of o th e r m in e r a ls i s s o i l . S o i l i n t a k e o f g r a z i n g a n i m a l s can be a s h i g h a s 10% o f t h e d r y m a t t e r i n t a k e , and ev en h i g h e r under some c o n d i t i o n s such as high s t o c k i n g r a t e or a r a i n y seas on (Healy, 1974). Manganese Manganese fertilizatio n - content in p la n ts in r e l a t i o n to s o i l As i n t h e c a s e o f i r o n , m an ga n es e status and co ntent in p l a n t s i s g e n e r a l l y n o t r e s p o n s i v e t o manganese f e r t i l i z a t i o n . I n m an ga n es e d e f i c i e n t s o i l s , and w i t h c r o p s s e n s i t i v e t o low l e v e l s o f a v a i l a b l e m an ganese i n t h e s o i l s u c h a s a l f a l f a and s o y b e a n s , m an g a n es e f e r t i l i z a t i o n w i l l p r o b a b l y i n c r e a s e t h e y i e l d o f t h e c r o p b u t w i l l h a v e l i t t l e e f f e c t on t h e m ang an ese c o n t e n t o f t h e p l a n t (Allaway, M anganese content 1971). in forages- v a r i a b i l i t y i n t h e i r manganese c o n t e n t . Fo rages show a g r e a t G ra ss es have a manganese c o n c e n t r a t i o n ran g in g from 40 t o 200 ppm, w i t h v a l u e s found lower 75 than 30 ppm and h ig h e r than 250 ppm. T y p i c a l c o n c e n t r a t i o n in a l f a l f a r a n g e s from 25 t o 45 ppm, but v a l u e s low er than 20 ppm and h ig h e r than 100 ppm are a l s o found (Church and Pond, 1974). A vera ge manganese c o n c e n t r a t i o n in corn s i l a g e i n M ich igan in 19 7 5 - 1 9 7 6 was 33 ppm (H illm a n and Fox, 197 7). Ear corn in P e n n s y l v a n ia from 1969 t o 1973 had a manganese c o n t e n t o f 7.3 ppm, and s h e l l e d c o rn 4.8 ppm (Adams, 1975). Soybean o i l m eal has an average manganese conten t o f 31 ppm (NRC, 1978). Manganese r e q u i r e m e n ts of dairy c attle- The su g g e ste d m an g a n ese d i e t a r y r e q u i r e m e n t i s 40 ppm i n t h e d i e t on a d r y m a t t e r b a s i s (NRC, 1978). in the d iet se e m t o High l e v e l s of c a l c i u m and phosphorus in te rfe re w i t h manganese a b s o r p tio n , i n c r e a s i n g the re q u ir e m e n t f o r i t i n t h e d i e t . Some a u t h o r s have recommended an i n c r e a s e o f t h e m ang a n es e c o n t e n t i n t h e d i e t t o 70-95 ppm t o ta k e c a r e of reduced manganese a b s o r p t i o n caused by high calcium in tak e (H id iro g lo u , 1979); how ever, th is recommendation i s s t i l l c o n t r o v e r s i a l . Manganese deficiency is d e f i c i e n c y and t o x i c i t y i n rum inants- linked reduced to silen t heats, Manganese conception, a b o r t i o n s , reduced b i r t h w e ig h t, i n c r e a s e d p e r c e n t a g e of m ale o f f s p r i n g , p a r a l y s i s , and s k e l e t a l damage i n d a i r y cows ( P u l s , 1981). Symptoms o f e x p e r i m e n t a l m a n g a n es e d e f i c i e n c y a r e w e l l documented (Underwood, 1977 and 1981; M i l l e r , 1981; H i d i r o g l o u , 1979; Thomas, 1 9 7 0 ), b u t s e v e r e d e f i c i e n c i e s do n o t seem t o be p r e v a l e n t w ith p r a c t i c a l d iets. It is very p o s s ib le th at b o r d e r l i n e d e f i c i e n c i e s w i t h n o n s p e c i f i c s i g n s a r e w idespread, e s p e c i a l l y i n a n i m a l s whose d i e t s a r e b a s e d on c o r n s i l a g e and 76 corn. T h e s e d i e t s a r e v e r y l i k e l y t o c o n t a i n l e s s t h a n 40 ppm manganese, t h e e s t i m a t e d req u ire m e n t. Manganese s o u r c e s - Manganese s u l f a t e , c h l o r i d e , c a r b o n a t e , d i o x i d e , and p o tas siu m permanganate a r e a l l v e ry a v a i l a b l e forms o f manganese f o r ru m in ants (Ammerman and M i l l e r , 1978), and can be i n c l u d e d i n t r a c e m i n e r a l s a l t s and r a t i o n s . Zinc Zinc con ten t fe r tiliz a tio n - in p la n ts A number o f con ten t o f natu ral fe e d s . a c id s o i l . p la n ts. in r e l a t i o n to general fa cto rs so il statu s a ffect th e and z in c Zinc i s more a v a i l a b l e to p la n t s in an Thus, l im i n g te n d s t o lo w er t h e z in c c o n t e n t o f th e S in c e l im i n g u s u a l l y i n c r e a s e s crop p r o d u c t i o n , z in c con ten t may be lower on some o f the b e tte r managed farms. Often the zin c con ten t o f forage p la n ts d e c li n e s somewhat with m aturity o f th e p l a n t . co n ten t is L ik e w ise , lo w e r some in fo r m a tio n s u g g e s t s t h a t th e in a dry c l i m a t e (M ille r , 1979). Z in c f e r t i l i z a t i o n , h o w ev e r, i s e x p e c t e d t o have a b ig g e r e f f e c t on y i e l d o f th e f o r a g e than on i t s z in c c o n c e n t r a t i o n (A lla w a y , 1971). Zinc con ten t in fo rag es- In g e n e r a l, are good s o u r c e s o f z i n c ( M i l l e r , 19 79). high p r o te in feed s G r a s se s have a z in c c o n c e n t r a t i o n ra n g in g from 20-80 ppm, w ith v a l u e s found low er th a n 15 ppm and h ig h e r than 100 ppm. A lfa lfa 's z in c con cen tration ranges from 12 to 35 ppm, with v a lu e s found lower than 10 ppm and h ig h e r than 50 ppm (Church and Pond, 1974). During the years o f 1975 and 1976, corn s i l a g e in Michigan had an average zin c con ten t o f 37 ppm (Hillman and Fox, 1977). Ear corn in P en n sylv an ia from 1969 to 1973 had an average zin c con ten t of 77 27 ppm, and s h e l l e d c o r n an a v e r a g e o f 25 ppm (Adams, 197 5). Soybean o i l m e a l h a s an a v e r a g e z i n c c o n t e n t o f 48 ppm (NRC, 1978). Z inc r e q u ir e m e n ts of d a ir y c a ttle - The estim ated zinc requirement for dairy c a t t l e i s 40 ppm in the d i e t . The t o x i c i t y th r esh o ld i s estim ated to range from 500 to 1500 ppm. According t o M i l l e r (19 7 9), th e req u ire m en t o f 40 ppm o f z i n c in th e d i e t p rov id es a modest margin of s a f e t y , s in c e in some c a s e s anim als consuming d i e t s w ith 40 ppm or more o f z i n c have improved t h e i r perform ance a f t e r z in c s u p p le m e n t a t io n . N e v e r th e le ss , i t is b e l i e v e d th a t t h i s l e v e l i s adequate for normal c a t t l e under most or a l l p r a c t i c a l feed in g c o n d itio n s ( M i l le r , 1979). Zinc d e f ic ie n c y and t o x i c i t y in ruminants- Weak hoof horn w ith i n c r e a s e d s u s c e p t i b i l i t y t o i n t e r d i g i t a l d e r m a tit is , fo o t r o t , and reduced c o n c e p t i o n r a t e a r e some o f th e symptoms o f zin c d e f ic ie n c y in c a t t l e . The e f f e c t o f the d e f ic ie n c y i s more se v e r e on male f e r t i l i t y than on fem ale f e r t i l i t y . m a tu r a tio n i s s e v e r e l y a f f e c t e d . in c lu d e reduced g r o w th p a r a k e r a to sis (P u ls, 1981). r a te, Spermatozoan V ery common symptoms a l s o reduced feed in ta k e , and As with s e v e r a l o f the other m ineral d e f i c i e n c i e s , a s e v e r e z in c d e f i c i e n c y d o e s n o t appear t o be a m ajor p r a c t i c a l p r o b le m in g e n e t i c a l l y normal ru m in an ts. However, th e e x t e n t o f b o r d e r l i n e d e f i c i e n c i e s in p r a c t i c a l s it u a t i o n s i s u n certa in . A key r ea so n fo r t h i s u n c e r t a i n t y i s the la ck of good d ia g n o s t ic procedures for d e te c tin g a b o r d e r lin e d e f i c i e n c y , e s p e c i a l l y under f i e l d c o n d itio n s ( M i l l e r , 1970 and 1979) . 78 Zinc t o x i c i t y i n c a t t l e i s uncommon due t o t h e h igh l e v e l s n e c e s s a r y t o produce p o i s o n i n g : a t l e a s t 500 ppm o f z in c i n t h e d i e t (NRC, 197 8 ). Zinc sources- Zinc oxide i s the most commonly used s o u rc e o f z i n c f o r t h e f o r m u l a t i o n o f t r a c e m i n e r a l s a l t s and r a t i o n s f o r r um in a n ts. Zinc s u l f a t e and zin c c h l o r i d e a r e a l s o r e a d i l y a v a i l a b l e s o u r c e s of z in c ( M i l l e r , 1979). C o b a lt C ob alt c o n ten t fe r tiliz a tio n - in p l a n t s in r e l a t i o n t o so il statu s and Both p l a n t s and animals require c o b a l t for t h e ir normal f u n c t i o n . The n i t r i f y i n g b a c t e r i a in th e n o d u le s o f legumes require c o b a l t for adequate nitrogen f i x a t i o n (Kubota and A llaw ay, 1972). crops such as fe r tiliz a tio n There i s a l s o some ev id en ce th at other nonlegume co tto n have (T isd a le e t a l . , h ig h er y ie ld s 1985 ). a fter c o b a lt The "amount o f c o b a l t required for optim al p l a n t growth i s n e v e r t h e le s s very s m a l l , and in some areas o f the world the concen tration o f c o b a l t in fo ra ges i s not s u f f i c i e n t to meet the requirements o f anim als (Hodgson e t a l., 1 9 62 ). In th e U n ite d S t a t e s th e low er A t l a n t i c C o a s t a l P la i n i s a ge n e ra l region o f e x c e e d in g ly low s o i l c o b a l t . Some sandy s o i l s o f g l a c i a t e d r e g i o n s in th e N o r t h e a s t and in the Great Lakes s t a t e s are a l s o low in c o b a lt . Forages grown in the r e g i o n s m en tioned h a ve a c o b a l t c o n c e n t r a t i o n to o low t o meet a n im a l's r e q u ir e m e n ts (Kubota and A l l a w a y , 1972). Even though c o b a l t f e r t i l i z a t i o n i s l i k e l y to in crea se c o b a lt conten t o f the crop s, the use o f c o b a l t f e r t i l i z e r s i s not a common p r a c tic e to c o r r e c t d e f i c i e n c i e s for anim als (Kubota and A llaw ay, 1972). 79 C obalt content of forages- Legumes g e n e r a l l y c o n t a i n more c o b a l t than do g r a s s e s , b u t ev en legumes a r e d e f i c i e n t i n c o b a l t for g razin g an im als i n some a r e a s N u t r i t i o n Lab. S t a f f , 1965). (U.S. P l a n t , S o il, a nd G r a s s e s and a l f a l f a t y p i c a l l y have a c o b a l t c o n t e n t o f 0.08-0.25 ppm i n t h e d ry m a t t e r , w ith v a l u e s fo u n d h i g h e r t h a n 0.30 ppm, and i n d e f i c i e n t a r e a s , l o w e r t h a n 0.08 ppm (Church and Pond, 197 4 ). Corn s i l a g e h a s an a v e r a g e c o b a l t c o n c e n t r a t i o n o f 0.06 ppm, s h e l l e d c o r n 0.04 ppm, and soybean o i l meal 0.10 ppm (NRC, 1978). C obalt requirements of d a iry c a t t l e component o f v itam in microorganism s. B12, which is C o b a l t i s an e s s e n t i a l syn th esized by ru m e n The minimum c o b a l t re q u ir e m e n t of d a i r y c a t t l e i s a b o u t 0.10 ppm (NRC, 1978). C o b a l t d i f i c i e n c y and t o x i c i t y i n r u m in a n ts- G enerally, a c o b a l t d e f i c i e n c y becomes e v i d e n t o n l y a f t e r a n im als have been on a d e f i c i e n t d i e t f o r a c o n s i d e r a b l e t i m e , and t h e n p r o g r e s s e s s l o w l y a s v i t a m i n B12 s t o r e s i n l i v e r and o t h e r t i s s u e s a r e depleted. C a t t l e do n o t s t o r e s i g n i f i c a n t amounts of c o b a l t i n u s a b l e forms; t h u s v i t a m i n B12 s y n t h e s i s d e c l i n e s v e ry q u i c k l y when d i e t a r y c o b a l t i s in ad e q u ate (NRC, 1978). The most co n sp icu o u s e a r l y f e a t u r e o f a c o b a l t d e f i c i e n c y i s decreased a p p etite and feed con su m p tio n resu ltin g in l i s t l e s s n e s s , r e t a r d e d growth or weight l o s s , and d e c r e a s e d m il k production. O t h e r symptoms, e s p e c i a l l y w i t h an e x t r e m e and ex te n d ed d e f i c i e n c y , can i n c l u d e e m a c ia tio n or w a stin g of th e m u s c u l a t u r e , p a l e n e s s of t h e s k i n and raucous membranes, m usc ular in c o o rd in a tio n , a stum bling g a i t , ro u g h h a i r c o a t , and h i g h 80 m o r t a l i t y r a t e among c a l v e s (NRC, 1978). The p o s s i b i l i t y o f l i v e s t o c k po iso n in g caused by an e x c e s s of c o b a l t in the n a t u r a l herbage of f e e d s t u f f s remote (Young, 1979). is ex trem ely C a l v e s fed e x c e s s i v e c o b a l t show reduced a p p e t i t e , l e s s g ro w th , d e c r e a s e d w a ter c o n su m p tio n , rough h a i r c o a t , l a c k o f m u s c u l a r c o o r d i n a t i o n , i n c r e a s e d h e m o g l o b i n and packed c e l l volume, and e l e v a t e d l i v e r c o b a l t compared t o c o n t r o l a n im a l s . lev el; Ten ppm i n t h e d ry d i e t i s g e n e r a l l y a cc ep ted as a s a f e h o w e v e r , t h e r e i s no e v i d e n c e t o i n d i c a t e t h a t 20 ppm would produce any a d v e r s e e f f e c t s (NRC, 1978). C o b a lt sou rces- The c a r b o n a t e , c h lo r id e , s u l f a t e and n itr a te forms o f c o b a l t h ave been proposed a s s a t i s f a c t o r y d ie ta r y sou rces of th e m in e ra l. B ecause o f its d e sir a b le p h y s i c a l c h a r a c t e r i s t i c s , c o b a l t c a r b o n a te i s f r e q u e n t l y th e c o b a lt source o f c h o ice in the feed industry. C ob alt p e l l e t s are u s u a l l y made w it h c o b a l t o x id e and c l a y (Ammerman and M i l l e r , 1978). T h e r e a r e s e v e r a l ways o f t r e a t i n g o r p r e v e n t i n g c o b a l t deficien cy in rum inants. D renching w ith c o b a l t c h l o r i d e or s u l f a t e i s e f f e c t i v e f o r a b o u t 3 weeks. B u l l e t s or p e l l e t s of c o b a l t i c o x id e g i v e n o r a l l y t h a t lo dg e i n t h e r e t i c u l o - r u m e n a r e e f f e c t i v e for a t l e a s t 3 years. T reatm ent of t h e p a s t u r e w ith 1 t o 5 kg o f c o b a l t s u l f a t e p e r h e c t a r e i s e f f e c t i v e f o r a t l e a s t one y e a r . be u s e d : m o st Subcutaneous i n j e c t i o n of hydroxycobalamine can a l s o 2 mg i n i t i a l l y and t h e n 1 mg p e r month. common p r a c t i c e to prevent co b alt By f a r , t h e deficien cy is the i n c o r p o r a t i o n of c o b a l t i n th e fo rm u la s of t r a c e m i n e r a l s a l t s a t 81 a r a t e o f 0.004 t o 0.01% o f t h e s a l t p r a c tic e is follo w ed ( P u l s , 1981) . This l a s t e v e n when t h e r e i s no e v i d e n c e o f c o b a l t d e f i c i e n c y i n t h e unsupplemented r a t i o n s (Underwood, 1981). Selenium S elen iu m content fertilizatio n - in p la n ts in r e l a t i o n to s o i l s ta tu s and Selenium i s a p p a r e n t l y n o t needed by p l a n t s . But i t m u st be p r e s e n t i n p l a n t s s i n c e i t i s e s s e n t i a l f o r a n i m a l s . P l a n t s d i f f e r i n t h e i r uptake of a v a i l a b l e s e le n iu m accord ing to s p e c i e s , s t a g e o f g r o w t h , and t h e s e a s o n . C e r t a i n s p e c i e s of A s t r a g a l u s a b s o r b more se l e n i u m than do o t h e r p l a n t s growing in the same m u sta r d , so il. P lan ts such as the cru cifers (ca b bage and f o r example) and onions which r e q u i r e l a r g e amounts of s u l f u r a b s o r b i n t e r m e d i a t e a m o u nts o f s e l e n i u m . G r a s s e s and g r a i n c r o p s a b s o r b l o w - t o - m o d e r a t e amounts o f se l e n i u m ( T is d a l e e t a l . , 1 9 8 5). F o r t h e m o st p a r t , s e l e n i u m - a c c u m u l a t o r p l a n t s a r e n o t ones t h a t a r e p r e f e r r e d by g r a z i n g a n im a l s . However, the s e l e n i u m t a k e n by t h e s e p l a n t s and r e t u r n e d t o t h e s o i l in t h e i r o r g a n i c r e s i d u e s i s much more a v a i l a b l e t o t h e common c r o p and p a s t u r e p l a n t s th an o t h e r se l e n i u m compounds. T h e r e f o r e , a c y c l e o f p l a n t s u c c e s s i o n i n which s e v e r a l y e a r s ' growth o f s e l e n i u m a c c u m u la to r p l a n t s i s f o l l o w e d by t h e growing o f fo r ag e g r a s s e s and c e r e a l s can r e s u l t in t o x i c l e v e l s of s e l e n i u m i n t h e common f o r a g e s and c e r e a l s 1 9 65 ). (U.S. P l a n t , S o i l , and N u t r i t i o n Lab. S t a f f , Selenium c o n c e n tr a tio n selenium f e r t i l i z a t i o n . in forages is responsive to S e le n ite s are p re fe rre d to s e le n a te s b e c a u s e t h e y a r e s l o w e r a c t i n g and t h u s l e s s l i k e l y t o p r o d u c e e x c e s s i v e l e v e l s of s e l e n i u m in p l a n t s th an t h e r a p i d l y a v a i l a b l e 82 s e l e n a te s (Tisdale e t a l . , 1985). Selenium f e r t i l i z a t i o n i s n o t , however, a common method t o p r o v i d e se l e n i u m t o a n i m a l s d e f i c i e n t in the m ineral. Selenium content of forages- The se l e n i u m c o n c e n t r a t i o n i n f o r a g e s and g r a i n i s d e p e n d e n t on t h e s e l e n i u m l e v e l s i n t h e so il. A s u r v e y c a r r i e d o u t i n 1957 showed t h a t f o r a g e s ( m a i n l y a lfa lfa ) from some selenium . areas in A pproxim ately the U nited 80% o f the S tates are low in sam ples of the a re a su rro u n d in g t h e G r e a t Lakes c o n t a i n e d l e s s t h a n 0.05 ppm s e le n iu m (Kubota and A lla w a y , 1972). In some o t h e r a r e a s in t h e c e n t e r o f t h e c o u n t r y t h e s e l e n i u m c o n t e n t i n t h e f o r a g e s s a m p l e d was h i g h e r t h a n 0.1 ppm. F i n a l l y i n some l o c a l i z e d s p o t s i n S o u t h Dakota, North Dakota, and Wyoming, s e l e n i u m - a c c u m u l a t o r p l a n t s were fo u n d w i t h c o n c e n t r a t i o n s h i g h e r t h a n 50 ppm (Kubota and A llaw ay, 1972). Selenium d o c u m e n te d , requirements of d a iry c a t t l e the re q u ire m e n t approxim ately 0.1 ppm, the for selenium exact lev el c h e m i c a l form o f s e l e n i u m and t h e enhancing f a c t o r s lip id s, proteins, in the d i e t , amino acids, Although n o t w e l l by r u m i n a n t s depending is upon t h e l e v e l s of i n t e r f e r i n g or i n c l u d i n g v i t a m i n E, s u l f u r , and several m icroelem ents (NRC, 1978) . Selenium d e f i c i e n c y and t o x i c i t y - Acute se l e n i u m d e f i c i e n c y can cause w hite musc le d i s e a s e , d i a r r h e a , muscle s t i f f n e s s , and o c c a s i o n a l l y recumbency, p a r t i c u l a r l y i n p a r t u r i e n t cows ( s i m i l a r t o m i l k f e v e r s y n d r o m e ). Sudden d e a t h due t o c a r d i a c f a i l u r e w i t h no p r i o r s i c k n e s s c a n a l s o be c a u s e d by a c u t e s e l e n i u m 83 deficiency. M a r g i n a l se l e n i u m d e f i c i e n c y can r e s u l t in r e t a i n e d p l a c e n t a s , a b o r t i o n s , r e d u c e d f e r t i l i t y , d e c r e a s e d growth r a t e and d e c r e a s e d immune r e s p o n s e ( P u l s , 1981). Selenium t o x i c i t y , which o c c u r s under p r a c t i c a l c o n d i t i o n s in s e v e r a l a re a s of th e w o rld , is o f te n c l a s s i f i e d as a cu te or c h r o n i c a l k a l i d i s e a s e . The l o w e s t t o x i c l e v e l i s a p p r o x i m a t e ly 3 t o 5 ppm, t h e e x a c t amount d e p e n d i n g upon t h e p r o t e i n , s u l f u r , and a r s e n i c l e v e l s (higher amounts of each reduce the t o x i c i t y ) o f t h e d i e t and on t h e c h e m i c a l form o f s e l e n i u m . A pparently, th e n a t u r a l l y o c c u r r i n g o r g a n i c s e l e n i u m of p l a n t s i s much more t o x i c t h a n t h e i n o r g a n i c form. The range between the req u irem en t and t o x i c l e v e l s i s 30 t o 5 0 - f o l d . c h a r a c t e r i z e d by d u l l n e s s , labored resp iratio n , respiratory fa ilu re . Acute s e le n iu m p o i s o n in g i s s lig h t atax ia, diarrhea, lethargy, r a p i d weak p u l s e , and d e a t h due t o Signs o f c h r o n i c se l e n i u m t o x i c i t y ( a l k a l i d ise ase ) in c lu d e lam eness, lo s s of v i t a l i t y , lo s s of a p p e t i t e , em aciation, neph ritis, loss of sore f e e t, h air from t h e tail, liv e r c irrh o sis, and deformed, c ra cked and e l o n g a t e d hoofs (NRC, 1978) . Selenium sources- Sodium s e l e n i t e and sodium s e l e n a t e a r e good s o u r c e s of se l e n i u m f o r rum in ants . Sin c e 1979, t h e Food and Drug A d m i n i s t r a t i o n has g r a n t e d a p p r o v a l f o r o r a l s u p p l e m e n ta t io n t o s h e e p , d a i r y and b e e f c a t t l e dairy c a t t l e , (Ammerman e t a l . , 198 0). Fo r s e l e n i u m can be added t o a l e v e l n o t t o exceed 0.1 ppm s e l e n i u m i n t h e com plete r a t i o n (Marckzewski, 1982). The most u s u a l and c o n v e n i e n t way t o a d m i n i s t e r se l e n i u m t o d a i r y a n im a l s i s through th e t r a c e m i n e r a l s a l t or m i n e r a l mix. Selenium s a l t s 84 ( s e l e n a t e o r s e l e n i t e ) can be i n c l u d e i n t h e t r a c e m i n e r a l s a l t f o r m u l a t i o n a t a r a t e o f 25 t o 75 ppm o f s e l e n i u m and f e d f r e e c h o ic e or 40 g per day p e r mature cow ( P u l s , 1981). O ccasionally, selenium in jectio n s a n im a l s under c e r t a i n c o n d i t i o n s . are recommended f o r Newborn c a l v e s may r e c e i v e a s i n g l e i n j e c t i o n o f 5 mg o f s e l e n i u m f o r t h e p r e v e n t i o n o f white musc le d i s e a s e . Cows may be i n j e c t e d with a commercial p r o d u c t t h r e e weeks p r e p a r tu m , and a g a i n a f t e r c a l v i n g . may be g i v e n ev en when the d i e t These i n j e c t i o n s c o n t a i n s t h e recommended amounts o f added s e l e n i u m (Marckzewski, 1982). Iodine Iodine content fertilizatio n - in p la n ts in r e l a t i o n to s o i l status and I o d i n e i s r e q u i r e d by a n im a l s b u t not by p l a n t s . Even so, p l a n t s w i l l acc um u late a p p r e c i a b l e amounts of i o d i n e in t h e i r t i s s u e s i f i t i s p r e s e n t i n an a v a i l a b l e form i n t h e s o i l , and io d in e from p l a n t s i s one o f t h e i m p o r t a n t s o u r c e s o f io d in e in anim al r a t i o n s . P l a n t s low i n i o d i n e a r e m o st o f t e n fou nd growing on g e o l o g i c a l l y young s o i l s and i n a r e a s o f low r a i n f a l l . I t appears t h a t the c y c le of io d in e in n a tu r e in v o lv es the v a p o r i z a t i o n o f i o d i n e compounds from t h e s e a , t h e i r t r a n s p o r t i n l a n d by w i n d , and t h e i r d e p o s i t i o n on l a n d by r a i n f a l l (U.S. P l a n t , S o i l , and N u t r i t i o n Lab. S t a f f , 1965). Iodine extrem ely content v ariab le, in and feedsit Iodine c o n te n t in forag es is d e p e n d s n o t o n l y on t h e iodine c o n c e n t r a t i o n i n t h e s o i l b u t a l s o on t h e p l a n t s p e c i e s and se ason of t h e y e ar (Underwood, 1981). A l f a l f a hay samples had an a v e r a g e i o d i n e c o n t e n t o f 0.82 ppm and c o r n s i l a g e 0.52 ppm i n 85 Illin o is. average Hay and c o r n s i l a g e s a m p l e s from M a r y l a n d had an iro d in e c o n te n t of (Hemken e t a l . , 197 2). se a a r e r i c h 1.87 and 1.64 ppm, resp ectiv ely A l l e d i b l e m a t e r i a l s o b t a i n e d from t h e i n i o d i n e , compared with s i m i l a r m a t e r i a l s o b t a i n e d from f r e s h water or from t h e l a n d . The e d i b l e f l e s h of s e a - f i s h and s h e l l - f i s h may c o n t a i n 0.3 t o 3.0 ppm i o d i n e on a f r e s h b a s i s , compa red w i t h 0.02 t o 0.04 ppm f o r f r e s h w a t e r - f i s h and with i n t e r m e d i a t e v a l u e s f o r f i s h which spend p a r t o f t h e i r l i f e i n t h e s e a and p a r t i n f r e s h w a t e r (Underwood, 1981). P astures, and c r o p s i n g e n e r a l , grown a t h i g h a l t i t u d e s t e n d t o be low i n iod in e, and en d em ic g o i t e r h a s b e e n o b s e r v e d i n t h o s e a r e a s (Kubota and A lla w a y , 1972). Iodine r e q u i r e m e n ts of dairy cattle - The i o d i n e req u ire m e n t o f l a c t a t i n g cows and dry p r e g n a n t cows i s 0.50 ppm, and i s 0.25 ppm f o r b u l l s , h e i f e r s and c a l v e s . I f the d i e t c o n t a i n s a s much a s 25% o f s t r o n g l y g o i t r o g e n i c f e e d on a d r y basis, i o d i n e p r o v i d e d s h o u l d be i n c r e a s e d by two times or more (NRC, 1978). Iodine deficiency and d e fic ie n c y in d a iry c a t t l e stillb irth , toxicity resu lts a b o r t i o n s and h a i r l e s s in ru m in a n ts- Io d in e in re p r o d u c tiv e f a i l u r e , o r weak young. Another symptom i s su p p r e s s e d e s t r u s w i t h r e s u l t a n t i n f e r t i l i t y 1981). (Puls, One o f f i r s t symptoms o b s e r v e d i s an e n l a r g e m e n t o f t h e t h y r o i d g l a n d s ( g o i t e r ) i n s l a u g h t e r e d c a t t l e or newborn c a l v e s (NRC, 1978). I o d i n e d e f i c i e n c y c a n be c a u s e d n o t o n l y by low i o d i n e co ntent in the d iet, but also by c h e m i c a l s in feeds that 86 likely to occur (Miller, 1974). G enerally the p e r c e n t a g e o f magnesium a b s o r b e d m a t e r i a l l y a f f e c t e d by t h e amount consumed. is not L ik ew ise, magnesium c o n t e n t o f t i s s u e s i s n o t e l e v a t e d with e x ce ss i n t a k e . Rather, h o m e o s t a s i s i s m a i n t a i n e d by t h e e x c r e t i o n o f e x c e s s magnesium v ia urine. More t h a n a t r a c e o f magnesium i n u r i n e i n d i c a t e s a d e q u a t e magnesium t o m e e t t h e a n i m a l ' s n e e d s . urine magnesium in d icates eith er V e r y low u r i n e a d eficien cy or a b arely a d eq u a te i n t a k e ( M i l l e r , 1974). A n a l y s i s o f f o r a g e f o r magnesium, n i t r o g e n and p o tas siu m can a id in d ia g n o s in g th e l i k e l i h o o d of a g r a s s te ta n y problem ; however, these are far less reliab le than u rin e and se ru m magnesium a n a l y s e s ( M i l l e r , 1974). Sodium, P o ta ssium and C h l o r in e Normal c o n c e n t r a t i o n s i n b lood serum a r e around 300 mg/100 ml f o r s o d i u m , 14 t o 18 mg/100 ml f o r p o t a s s i u m , and a r o u n d 360 mg/100 ml f o r c h l o r i n e (Ch u rch, 197 6). Serum c o n c e n t r a t i o n o f t h e s e t h r e e e l e m e n t s i s n o t a good i n d i c a t o r o f t h e a d e q u a c y o f t h e d i e t or t h e n u t r i t i o n a l s t a t u s o f t h e an im al ( M i l l e r , 1974). I n humans, se ru m sodium i s p a t h o l o g i c a l l y d e h y d ra tio n , sod iu m in to x ic a tio n , increased in ad re n o co rtica l h y p erfunctioning, c o r tic o s te r o id therapy, b rain in ju ry , b rain hemorrhage and e n c e p h a l i t i s . I t i s d e c r e a s e d by s e v e r e sw eating w i t h o u t a d e q u a t e sodium i n t a k e , by l o s s o f d i g e s t i v e ju ices (through d i a r r h e a or v o m it i n g ) , and because of b u r n s , e xpansion of the e x t r a c e l l u l a r pneum onia, severe flu id renal due t o w a te r tu b u lar in ju ry , in to x ic atio n or ad ren o co rtical 87 i n t e r f e r e w i t h i o d i n e a b s o r p t i o n by t h e a n i m a l . C ru ciferous p l a n t s c o n t a i n v a r i a b l e amounts o f g o i t r o g e n s o f t h e g o i t r i n type which i n t e r f e r e w i t h t h e p r o c e s s o f hormonogenesis in th e t h y r o i d gland. Many p a s t u r e p l a n t s , such a s c l o v e r , c o n t a i n cyano g e n etic g l y c o s i d e s t h a t a r e g o i t r o g e n i c (Underwood, 1981). Soybean o i l meal i s m i l d l y g o i t r o g e n i c (Hemken, 1970). I o d i n e p o i s o n i n g c a n r e s u l t from e x c e s s i v e i o d i n e i n t a k e , e s p e c i a l l y from medicated f e e d s . (EDDI) is E th y len ed iam in e d ih y d rio d id e s o m e t i m e s add ed t o t h e r a t i o n in excess of io d in e d i e t a r y r e q u i r e m e n t s t o p r e v e n t f o o t r o t and s o f t t i s s u e lumpy jaw, and a s an e x p e c t o r a n t i n t r e a t m e n t o f m i l d r e s p i r a t o r y in fectio n s. Signs of iodine to x icity include lacrim ation, c o r y z a , c o n j u n c t i v i t i s , c o u g h i n g , h a i r l o s s , and e x o p h t h a l m u s ( H i l l m a n and C u r t i s , 1980). O t h e r symptoms o b s e r v e d i n c a l v e s a r e b r o n c h o p n e u m o n i a and squamous m e t a p l a s i a o f t h e t r a c h e a l epithelium . The t h y r o i d s o f t h e a n im a ls s u f f e r i n g from t o x i c i t y had l a r g e f o l l i c l e s , a f l a t e p i t h e l i u m , and l a r g e amou nt s o f co llo id (Mangkoewidjojo e t a l . , 1980). Iod ine sources- Sodium and p o ta s siu m io d id e are w e l l u t i l i z e d a s s o u r c e s o f o f i o d i n e but l a c k p h y s i c a l s t a b i l i t y . C alciu m i o d a t e , d i i o d o d it h y m o l and pentacalcium orthoperiodate are l e s s water s o l u b l e , have greater p h y sic a l s t a b i l i t y and are sim ila r t o so d iu m and p o t a s s i u m io d id e in a v a i l a b i l i t y . D i i o d o s a l i c y l i c a c id i s r e a d i l y absorb ed by rum inants but i s excreted with l i t t l e r e l e a s e of iodine from the c y c l i c str u c tu r e. I n j e c t a b l e forms o f io d ize d o i l s have been e f f e c t i v e in supplying s u p p le m e n t a l io d in e to sh ee p (Ammerman and M i l l e r , 1978). 88 E t h y l e n e d i a m i n e d i h y d r i o d i d e can a l s o be u s e d a s a s o u r c e o f io d i n e ( M i l l e r and Swanson, 1973). T rac e m i n e r a l s a l t s u s u a l l y c o n t a i n 0.007 t o 0.01% i o d i n e (NRC, 1978). P lan t A n aly sis Plant analysis for soil fertility evaluation- Plant a n a l y s e s a r e b a s e d on t h e p r e m i s e t h a t t h e amount o f a g i v e n elem ent in p articu lar a plan t is an i n d i c a t i o n o f t h e s u p p l y o f n u t r i e n t and a s s u c h is d i r e c tl y q u a n t i t y of the n u t r i e n t in the s o i l . elem ent w i l l lim it the p l a n t 's related th at to the S i n c e a s h o r t a g e o f an growth, other e l e m e n t s may a c c u m u l a t e i n t h e c e l l s a p and show h i g h t e s t s , r e g a r d l e s s o f supply. F o r e x a m p l e , i f c o r n i s low i n n i t r a t e , t h e p h o s p h o r u s t e s t may show h i g h . adequate nitrogen T h i s i s no i n d i c a t i o n , h o w e v e r , t h a t i f were s u p p l i e d p h o s p h o r u s w o u ld be a d e q u a t e analysis fertility . provides some u n i q u e to th e corn (T isdale e t a l . , advantages to the supply 1975). evaluate of P lant so il The n u t r i e n t c o n t e n t o f t h e p l a n t i s a r e f l e c t i o n of the s o i l ' s a v a i l a b l e n u t r ie n t s t a t u s : the p l a n t 's a b i l i t y to ab so r b a n u t r i e n t i n t h e e s t a b l i s h e d environm ent i s r e f l e c t e d by the p l a n t n u t r i e n t c o n c e n t r a t i o n a t any one time. By comparison, a s o i l t e s t does n o t always p r o v i d e a measure of t h e s o i l - p l a n t in te rac tio n . On the other hand, so il tests for some m i c r o n u t r i e n t s a re e i t h e r n o n e x i s t e n t or no t w i d e l y adap ted for u n i v e r s a l use Sampling- (Jones, 1972). As a g e n e ra l p r i n c i p l e for any type of sampling, sa m p le s for p l a n t a n a l y s i s s h o u ld be r e p r e s e n t a t i v e o f th e p op u la tio n of p la n t s in the f i e l d under study. There are s e v e r a l 89 c riteria t o m eet i n o r d e r t o i n t e r p r e t t h e r e s u l t s o f p l a n t analyses. P l a n t a n a l y s i s l a b o r a t o r i e s p r o v i d e i n s t r u c t i o n s on t h e p l a n t p a r t t o s e l e c t , number o f p a r t s t o c o l l e c t , number o f p lan ts to sam ple, and t im e o f s a m p l i n g (Jones, 1 9 72 ). The C o o p e r a t iv e E x te n s io n S e r v i c e of M ichigan S t a t e U n i v e r s i t y p r o v i d e s g u i d e s on t h e p a r t o f t h e p l a n t t o s a m p l e , sam pling, tim e of and t h e a c c e p t a b l e o r s u f f i c i e n c y n u t r i e n t r a n g e s r e q u i r e d fo r high p r o d u c tio n of s e v e r a l c ro p s (V ito sh e t a l . , 1981). Dust or so il co n tam in atio n can change the m in eral c o n c e n t r a t i o n o f t h e s a m p l e , e s p e c i a l l y i t s i r o n and m an ga nese content. When t h e p a r t s o f t h e p l a n t s a m p l e h a v e b e en c l o s e t o t h e ground and t h e r e i s s o i l c o n t a m i n a ti o n , o r when t h e r e i s too much d u s t on t h e l e a v e s , washing of the sa m ple s may be n e c e s s a r y . There i s no g e n e r a l agreement on which washing p r o c e d u r e s h o u l d be used. Some l a b o r a t o r i e s recommend such means as h y d r o c h l o r i c a c i d s o l u t i o n s , d e t e r g e n t s , EDTA, wiping o f smooth l e a v e s with a damp c l o t h , or com binations of th e s e methods. When a c i d s , d e t e r g e n t s o r o t h e r s o l u t i o n s a r e u se d t o wash t h e s a m p l e s , r i n s i n g w i t h d i s t i l l e d o r d e i o n i z e d w a t e r m u st f o l l o w ( J o n e s , 197 2). I n c o n t r a s t , when f o r a g e s a r e a n a l y z e d t o a s s e s s t h e n u t r i t i o n a l s t a t u s of a n im a l s s o i l or d u s t c o n ta m i n a ti o n sh o u l d n o t be removed i n o r d e r t o p r o v i d e a b e t t e r id e a of what th e an im al i s consuming. D ry in g , g r i n d i n g and a s h i n g - p r e f e r a b l y i n a f o r c e d a i r oven. drying a re p r e fe rre d Fresh sa m ple s s h o u l d be d r i e d R e l a t i v e l y low t e m p e r a t u r e s f o r (45 t o 60° C) t o a v o i d v o l a t i l i z a t i o n o f 90 o r g a n i c compounds. cu ttin g faces S tain less in m i l l s used p o s s i b i l i t y o f c o n ta m i n a ti o n . steel s c r e e n s and t o o l steel to g rin d sam ples red u ce the The mesh s i z e o f th e s i e v e chosen i s u s u a l l y 1 mm, which a c h i e v e s good homogenization of t h e sample ( J o n e s , 1972; F i c k e t a l . , 197 9). The a s h i n g p ro c e d u r e of th e sample i s chosen in view of t h e m ineral t o be a n a l y z e d . Dry a s h i n g is necessary for boron a n a l y s i s s i n c e t h i s e l e m e n t i s v o l a t i l i z e d d u r i n g wet a s h i n g ( J o n e s , 1972 ). Wet a s h i n g i s u s e d f o r t h e a n a l y s i s o f e l e m e n t s t h a t a r e v o l a t i l e a t h ig h te m p e r a t u r e s such as s e le n iu m . Dry a s h i n g p r o v i d e s good p r e c i s i o n and i s an e a s y , r a p i d d i g e s t i o n m eth od r e q u i r i n g m inim al a n a l y s t a t t e n t i o n . b e n e f i t i s t h a t t h i s method i s r e l a t i v e l y co n tam ination. An a d d i t i o n a l f r e e from r e a g e n t V a r i o u s d i g e s t i o n r e a g e n t s a r e u s e d f o r wet ashing in clu d in g n i t r i c , p erchloric, s u lfu ric , h y d r o f l u o r i c and h y d r o c h l o r i c a c i d s , and hydrogen p e ro x i d e . The main a d v a n t a g e of th is ele m e n tal m ethod is v o latiliza tio n tem perature. th at because elim in ates the d ig estio n takes place lo ss by a t a low I t s m ain d i s a d v a n t a g e s a r e t h a t i t i s s u b j e c t t o rea g en t contamination, atten tio n it i s t e d i o u s and r e q u i r e s c a r e f u l o p e r a t o r ( P e r k i n , 1 982). S p e c i a l c a r e s h o u l d be t a k e n when p e r c h l o r i c a c i d i s used i n t h e r e a c t i o n m i x t u r e , s i n c e t h i s a c i d forms e x p l o s i v e m ix t u r e s w ith o r g a n i c m a t t e r . I n t h i s c a s e the s a m p l e s h o u l d be p r e d i g e s t e d f i r s t w i t h o t h e r a c i d s u n t i l t h e organic m atter is oxidized com pletely. A nalytical av aila b le techniques- S ev eral a n a l y t i c a l techniques are for m in eral a n a ly s is . The d i f f e r e n t m e t h o d s t a k e 91 a d v a n t a g e o f t h e p h y s i c a l and c h e m i c a l c h a r a c t e r i s t i c s o f t h e elem ent or e lem en ts an aly zed . In s e v e r a l l a b o r a t o r i e s atom ic a b s o r p t i o n and e m i s s i o n t e c h n i q u e s a r e t h e method o f c h o i c e (U llrey, 1977). Several e l e m e n t s c a n be a n a l y z e d w i t h t h e p r e p a r a t i o n by atomic a b s o r p t i o n . The method i s and to sen sitiv e low c o n c e n t r a t i o n s e le m e n t s such a s ph o sphorus, s u l f u r , d iffic u lt to measure (Perkin, same s a m p l e fast, accurate 1 976). Some n i t r o g e n , and s e l e n i u m a r e by a t o m i c a b s o r p t i o n . P h o s p h o r u s commonly a n a l y z e d by c o l o r i m e t r i c p r o c e d u r e s (Fick e t a l . , is 1978). N i t r o g e n i s d e t e r m i n e d by t h e K j e l d h a l p r o c e d u r e , and s e l e n i u m c a n be a n a l y z e d f l u o r i m e t r i c a l l y ( W h e t te r and U l l r e y , 1978) . S u l f u r can be a n a l y z e d i n d i r e c t l y th rough atomic a b s o r p t i o n , by m easu rin g barium a f t e r th e p r e c i p i t a t i o n o f th e s u l f a t e s w ith barium c h l o r i d e Several (P e rkin , 1982). elem ents can be d e t e r m i n e d a t o n c e by p l a s m a e m iss io n s p e c t r o p h o t o m e t r y , i n d u c t i v e l y c o u p le d plas ma d i s c h a r g e ( B a r n e s , 1 9 7 9 ) , and n e u t r o n a c t i v a t i o n (Ehmann and J a n g h o r b a n i , 19 79). These methods are fast and s e n s i t i v e . T heir d i s a d v a n t a g e i s t h e h ig h c o s t o f t h e i n s t r u m e n t s a c q u i r e d . main 92 Blood M i n e r a l s and D e f i c i e n c i e s D ia g n o sis C l i n i c a l and p a t h o l o g i c a l o b s e r v a t i o n s o f t h e a n i m a l a r e e s s e n tia l d iag n o stic to o ls for a l l m i n e r a l d e f i c i e n c i e s and t o x i c i t i e s , a l t h o u g h t h e i r v a l u e v a r i e s w i t h t h e e l e m e n t and with the s e v e r i t y of the d e fic ie n c y or t o x i c i t y in q u e s tio n . M ild m in e ral d e f i c ie n c i e s or ex ce sse s a re e s p e c i a l l y d i f f i c u l t to i d e n t i f y b e c a u s e t h e i r e f f e c t s on t h e a n i m a l a r e f r e q u e n t l y i n d i s t i n g u i s h a b l e from t h o s e r e s u l t i n g fr o m s e m i s t a r v a t i o n o r underfeeding, from p r o t e i n p a rasitism . A d ep re ssio n d eficien cy in or from ap p etite , w ith in te stin a l resu ltin g u n d e r n u t r i t i o n , i s a common symptom o f a l l m i n e r a l d e f i c i e n c i e s , as it is w ith d e f i c i e n c i e s of o th er esse n tia l n u trien ts (Underwood, 1981). When t a k e n i n c o n j u n c t i o n w i t h c l i n i c a l and p a t h o l o g i c a l o b s e r v a t i o n s , a p p r o p r i a t e c h em ic al a n a l y s i s and b i o l o g i c a l a s s a y s o f t i s s u e s and f l u i d s of a n i m a l s a r e v a l u a b l e a i d s i n t h e e a r l y d e t e c t i o n of m i n e r a l a b n o r m a l i t i e s i n l i v e s t o c k . v alu ab le in d istin g u ish in g b e tw e e n various They a r e a l s o functional and s t r u c t u r a l d i s o r d e r s of m i n e r a l o r i g i n , t h e c a u s e s o f which a r e d i f f i c u l t t o i d e n t i f y on t h e b a s i s o f c l i n i c a l e v i d e n c e a l o n e . The d i a g n o s t i c s i g n i f i c a n c e o f s u c h b i o c h e m i c a l d a t a a r i s e s p r i m a r i l y from t h e f a c t t h a t a d i e t a r y d e f i c i e n c y o f a m i n e r a l i s sooner or l a t e r r e f l e c t e d in subnorm al c o n c e n t r a t i o n s of the m i n e r a l in c e r t a i n t i s s u e s and f l u i d s (Underwood, 1981). The ch oice o f t i s s u e or f l u i d for a n a l y s is v a r ie s with the mineral under i n v e s t i g a t io n . o b v io u s a d v a n ta g e s b e c a u se B lood, u rin e , s a l i v a and hair have of th e ir a c c e ssib ility w ith o u t 93 s a c r i f i c e o f th e a n im a l. d iffic u ltie s , a lt h o u g h Body t i s s u e sa m p lin g p r e s e n t s more s im p le techniques are now a v a i l a b l e . liv e r and ta il bone b io p s y Whole b lood , blood serum or plasma i s more employed for s t u d ie s in m ineral n u t r it io n than any other t i s s u e or f l u i d o f th e body b e c a u se i t i n v a r i a b l y r e f l e c t s , in some asp ect o f i t s com position, the mineral s t a t u s o f the animal, and can be obtained e a s i l y and and fr e q u e n tly without harm to or d e a th o f th e a n im a l. I t can a l s o be r e a d i l y t r a n s p o r t e d and s t o r e d fo r su b s e q u e n t a t t e n t i o n . The normal v a l u e s or normal range o f c o n c e n t r a t i o n s in th e b lo o d o f h e a l t h y farm a n im a ls c o n s u m in g sa tisfa c to r y d ie ts are known f o r m o st o f th e n u t r i t i o n a l l y important m in e ra ls, making p o s s i b l e comparison with v a l u e s found in th e b lo o d o f d o m e s tic l i v e s t o c k under stu d y (Underwood, 1981). The m i n e r a l c o n c e n t r a t i o n i n b lood i s , high i n d i v i d u a l mechanisms. other anim al however, s u b j e c t t o v a r i a t i o n and t o t h e c o n t r o l o f h o m e o s t a t i c I n c o n t r a s t t o t h e m i n e r a l c o n t e n t i n f o r a g e s and feeds, which vary to a great e x ten t, tissu e c o n c e n t r a t i o n s o f f u n c t i o n a l forms o f e s s e n t i a l t r a c e e le m e n t s i s u s u a l l y m a in ta in e d w i t h i n narrow l i m i t s ( M i l l e r , 1975). E x p e r i m e n t a l l y , some m i n e r a l d e f i c i e n c i e s can be r e l a t i v e l y easy to i d e n t i f y . How ev er, u n d e r f i e l d c o n d i t i o n s , d i a g n o s i n g e v e n a c u t e d e f i c i e n c i e s i s f r e q u e n t l y n o t e a s y , and b o r d e r l i n e d e f i c i e n c i e s a r e f a r more d i f f i c u l t t o d e t e c t . a f f e c t so many a n i m a l s , Because th ey b o r d e r l i n e d e f i c i e n c i e s a r e o f much g r e a t e r importance ( M i l l e r , 1974). To diagnose n u t r i t i o n a l mineral problems, a l l the a v a i l a b l e 94 i n f o r m a t i o n s h o u l d be c o n s i d e r e d . T h is in clu d es anim al perf o rm ance, feed i n t a k e , c l i n i c a l and p a t h o l o g i c a l o b s e r v a t i o n s , s o i l a n a l y s i s , f o r a g e and f e e d a n a l y s i s , and t i s s u e a n a l y s i s . Even t h e n , d i a g n o s i s i s o f t e n d i f f i c u l t ( M i l l e r , 1974). Calcium and Phosphorus C a l c i u m and p h o s p h o r u s c o n c e n t r a t i o n i n b l o o d and i n t h e a n im a l's m etab o lism is c o n tro lle d by t h e in te rac tio n of p a r a t h y r o i d hormone and c a l c i t o n i n w ith t h e a c t i v e m e t a b o l i t e of v i t a m i n D3, 1 , 2 5 - d i h y d r o x y c h o l e c a l c i f e r o l (Underwood, 1981). The h o m e o s ta ti c or p h y s i o l o g i c a l mechanisms r e g u l a t i n g serum c a l c i u m a r e more e f f e c t i v e than those m inerals 1974). (M iller, f o r p h o s p h o r u s o r m o st o t h e r When t h e r e is a failu re of the h o m e o s ta ti c mechanism, such as i n m il k f e v e r , serum c a l c i u m g e t s v e r y low. Normal serum c a l c i u m c o n c e n t r a t i o n i s about 10 mg/100 m l , w i t h a r a n g e o f 9 t o 12 mg/100 ml (C hu rch , 1 976). When a cow i s a f f e c t e d by m i l k f e v e r , se ru m c a l c i u m l e v e l s d r o p t o 3 t o 7 mg/100 m l, t h e a v e r a g e being 5 mg/100 m l. Signs u s u a l l y appear when t h e serum c a l c i u m f a l l s t o 7 mg/100 ml o r l o w e r (Merck, 1979). Normal phospho rus b lood serum c o n c e n t r a t i o n i n a d u l t c a t t l e i s 4 t o 6 mg/100 m l , and somewhat h i g h e r , 6 -8 mg/100 m l , i n v e r y young a n im a l s (Underwood, 1981). According t o Underwood (1981), t h e f i r s t known r e s p o n se t o a d i e t a r y d e f i c i e n c y of phosphorus i s a f a l l i n t h e i n o r g a n i c ph osphate l e v e l o f t h e blood plasma and a w ith d r aw a l of c a l c i u m and phosphorus from r e s e r v e s i n t h e bones. Accompanying t h i s d e c l i n e i s a r i s e i n pl asma ph o sp h a tas e and a s m a l l r i s e i n se rum c a l c i u m c o n c e n t r a t i o n s , t o 13 o r 14 mg/100 95 ml. A f t e r a few weeks o r months on a p h o s p h o r u s - d e f i c i e n t d i e t , the con cen tratio n s f a l l t o 2-3 mg/100 m l, and c o n c e n t r a t i o n s of 1-2 mg/100 ml have been r e c o r d e d i n m i l k i n g cows s u f f e r i n g from severe deficiency (Underwood, 1981). C a l c i u m and p h o s p h o r u s d e f i c i e n c i e s c a n be d i a g n o s e d by b l o o d a n a l y s i s co m b in ed w i t h f e e d a n a l y s i s and o b s e r v a t i o n o f c lin ical and p a t h o l o g i c a l signs. A d e fic ie n c y of calcium , phosphorus, o r v i t a m i n D can r e s u l t i n bone d e m i n e r a l i z a t i o n , and t h u s i n a d e c r e a s e o f a s h i n t h e bon e. I f bones a re a v a i l a b l e f o r a n a l y s i s , t h e r e f o r e , bone ash v a l u e s can a l s o be used t o h e l p d iag n o s e d e f i c i e n c i e s ( M i l l e r , 1974). Magnesium The n o r m a l c o n c e n t r a t i o n o f magnesium i n b l o o d se rum o f c attle is around 1.8 t o 3.0 mg/100 ml (Church, 1 976). Low c o n c e n t r a t i o n o f magnesium i n p a s t u r e s r e s u l t s i n a d e c l i n e o f serum magnesium. potassium and T h i s may a l s o be w o r s e n e d by h i g h l e v e l s o f n itro g en in the p astu re, a b s o r p t i o n from t h e g u t i s th en impaired. b e c a u s e magnesium T h is c o n d i t i o n i s more l i k e l y t o occur a t t h e b egin ning o f s p r i n g when th e p a s t u r e s a r e growing r a p i d l y . drops. As hypomagnesemia d e v e l o p s , t h e serum magnesium U s u a l l y when t h e se rum magnesium i s b e l o w 1.0 o r 1.5 mg/100 m l , c l i n i c a l symptoms o f magnesium t e t a n y a r e o b s e r v e d (Merck, 1979 ). S u b n o r m a l se rum c a l c i u m (5 t o 8 mg/100 ml) i s u s u a l l y a l s o c h a r a c t e r i s t i c o f magnesium t e t a n y (Merck, 1979). Serum magnesium a n a l y s i s i s one o f b e s t i n d i c a t o r s o f the magnesium s t a t u s o f c a t t l e . Low serum magnesium in a s u b s t a n t ia l p r o p o r t io n o f th e a n im a ls s u g g e s t s t h a t a t e t a n y o u tb re a k i s 96 insufficiency agents, (Addison's d i s e a s e ) , m ed icatio n with d i u r e t i c and d i a b e t i c k e t o s i s (Geigy, 1975). The se ru m c h l o r i d e lev el i n humans increased a f t e r p r o tr a c te d dehydration, a cid o sis (L ightw ood and A l b r i g h t a lk a lo sis, after co rtico stero id s. head in ju ries is p a th o lo g ically i n r e n a l h y p e rc h l o r e m ic ty p es), in resp irato ry and d u rin g tr e a tm e n t w ith I t i s d e c r e a s e d by s e v e r e s w e a t i n g w i t h o u t ad eq u a te c h l o r i n e i n t a k e , by l o s s o f d i g e s t i v e j u i c e s ( e s p e c i a l l y g a stric ju ice), flu id , by b u r n s , by e x p a n s i o n o f t h e e x t r a c e l l u l a r by i n i n j u r y t o t h e r e n a l t u b u l e s , in su fficien cy , in a d re n o c o r tic a l because of m ed ica tio n w ith c e r t a i n d iu retic a g e n t s , i n r e s p i r a t o r y a c i d o s i s and o c c a s i o n a l l y i n d i a b e t i c k e t o s i s accompanied by d i u r e s i s The se rum p o t a s s i u m .in cre ased by r a p i d h em olysis, (Geigy, lev el 1975). i n humans i s p a t h o l o g i c a l l y in fu s io n of potassium s a l t s , by a c u t e tissu e breakdow n, in in m assive ad ren o co rtical i n s u f f i c i e n c y , by r e n a l f a i l u r e accompanied by o l i g u r i a or a n u r i a and by u n t r e a t e d d iab e tic k eto sis. It is p a th o lo g ic a lly d e c r e a s e d by in a d e q u a t e potassium i n t a k e or a b s o r p t i o n , by l o s s o f d i g e s t i v e j u i c e s , i n a d r e n o c o r t i c a l h y p e r f u n c i o n i n g due t o hyperaldosteronism therapy), (C ushing's syn d ro m e), or co rtico ste ro id by kidney d i s e a s e accompanied by p o l y u r i a , because of m e d i c a t i o n w i t h d i u r e t i c a g e n t s , by r e n a l t u b u l a r a c i d o s i s , by F a n c o n i's sy n d r o m e , and by d i a b e t i c k e to sis during in su lin t r e a t m e n t (Geigy, 1975) . Changes o f sodium, c h l o r i d e and po tas siu m c o n c e n t r a t i o n s i n r um in ants due t o p a t h o l o g i c a l metab olism a r e no t w e l l documented. 97 I t i s exp ected , n e v e r t h e l e s s , th a t th ese changes would be s im ila r to those observed in humans. Serum sodium, p o ta s s iu m and c h l o r i d e a r e no t good i n d i c a t o r s o f t h e n u t r i t i o n a l s t a t u s o f r u m in a nts. The a n a l y s e s of s a l i v a and fee d f o r sodium and p o tas siu m l e v e l s a r e more u s e f u l measures o f t h e s t a t u s o f t h e s e two m i n e r a l s in c a t t l e . Due t o wide v a r i a t i o n s , h a i r , u r i n e and f e c a l sodium h ave low r e l i a b i l i t y as a d i a g n o s t i c measure ( M i l l e r , 1974). Iron Normal iron c o n c e n tra tio n ug/100 ml (Church, 1976). i n b l o o d se rum i s a r o u n d 150 I r o n o c c u r s i n b l o o d a s hemoglobin i n t h e e r y t h r o c y t e s and a s t r a n s f e r r i n i n t h e p l a s m a i n a r a t i o o f n e a r l y 1000:1. The l e v e l s of hemoglobin in t h e b lo o d v a ry w ith n u t r i t i o n a l l e v e l , pregancy and l a c t a t i o n s t a t u s , a l t i t u d e , h e alth of th e anim al (Underwood, and 1977). For e x a m p le , th e h e m a t o c r i t v a l u e of sh eep kept i n a h y p o b a ri c chamber f o r 32 days a t 348 mm Hg o f p r e s s u r e ( e q u i v a l e n t t o 6200 m of a l t i t u d e ) , rose t o 37.3 c om pared w i t h t h e m e a s u r e d v a l u e o f 27.1 f o r c o n t r o l a n i m a l s k e p t a t a p r e s s u r e o f 6 2 0 -64 0 mm Hg ( P h i l l i p s , 1969). Serum i r o n c o n c e n t r a t i o n in s t e e r s m a i n t a i n e d a t an a l t i t u d e of around 3000 m was 1123 ug/100 ml (Wilson, 1975). Blood a n a l y s i s i s n o t a good i n d i c a t o r of t h e i r o n s t a t u s of anim als, e s p e c i a l l y f o r ru m in ants which a r e u n l i k e l y to s u f f e r from s e v e r e i r o n d e f i c i e n c y . C a l v e s fed e x c l u s i v e l y on m i l k f o r s e v e r a l weeks may d e v e l o p i r o n d e f i c i e n c y a n em ia (NRC, 1978). N evertheless, sen sitiv e low h e m o g l o b i n and h e m a t o c r i t v a l u e s a r e n o t i n d ic a to r s of the e a r l y sta g e s of iro n d e fic ie n c y 98 because they d ep leted . do n o t T heir occur use u n til storage is m ainly lim ite d c o n f i r m a t i o n of a c u te i r o n d e f i c i e n c y iron is sev erely to d ia g n o s is (M iller, 1974). and Analysis o f t h e d i e t may be o f v a l u e i n d i a g n o s in g i r o n d e f i c i e n c y b e fo r e c l i n i c a l symptoms ap p ear. Zinc The normal o r adeq uate serum z in c l e v e l i n c a t t l e i s 70 t o 140 ug/100 m l, t h e d e f i c i e n t l e v e l i s 20 t o 40 ug/100 m l, t h e low b o r d e r l i n e l e v e l i s 50 t o 60 u g / 1 0 0 m l , and t h e t o x i c l e v e l i s 520 t o 7500 u g / 1 0 0 ml ( P u l s , 1 981). Plasm a zin c is quickly reduced in an im als fed a s e v e r e l y d e f i c i e n t d i e t . How ever, i n d i v i d u a l v a r i a b i l i t y o f plasma z in c l e v e l s i s h igh compared to d i f f e r e n c e s c a u s e d by a m a r g i n a l d e f i c i e n c y , factors and d i s e a s e s affect these lev els, and many o t h e r so a b o r d e r l i n e d e f i c i e n c y h a s much l e s s e f f e c t on t h e l e v e l s o f p l a s m a z i n c (M iller, 1974). S ince nonspecific, c lin ica l sy m p t o m s o f b o r d e r l i n e d e f i c i e n c y a r e and g i v e n t h e i n d i v i d u a l v a r i a b i l i t y i n plas ma or se ru m z i n c ( M i l l e r , 1 9 7 4 ) , p r o b a b l y t h e b e s t way t o d i a g n o s e a d e f i c i e n c y i s through a n a l y s i s o f t h e d i e t , combined w ith blood a n a l y s i s and o b s e r v a t i o n of c l i n i c a l symptoms. Copper Adequate copper l e v e l s i n blood serum i n c a t t l e a r e i n the range o f 80 t o 150 ug/100 m l, d e f i c i e n t l e v e l s a r e 6 t o 70 ug/100 m l, m a r g i n a l o r b o r d e r l i n e d e f i c i e n t l e v e l s a re 55 t o 80 ug/100 m l , h i g h l e v e l s a r e 250 t o 400 u g / 1 0 0 m l , and t o x i c l e v e l s a r e 400 t o 1100 ug/100 ml ( P u l s , 1981). Copper p o i s o n i n g c a u se s th e 99 c o n c e n tr a ti o n of copper in th e liv e r and b l o o d t o i n c r e a s e . Blood serum copper c o n c e n t r a t i o n s of 500 t o 2000 ug/100 ml have been o b s e r v e d d u r in g th e h e m o l y t ic c r i s i s of copper p o is o n in g (Merck, 1979). Since the liv er is a n a ly s is of the l i v e r the organ where c o p p e r is stored, i s a good i n d i c a t o r o f c o p p e r s t a t u s . However, because o f t h e c o m p a r a t i v e e a s e i n t a k i n g sa m p le s, blood p lasm a copper i s o f t e n t h e measurement used. A b e t t e r measure of copper s t a t u s i s c e r u l o p l a s m i n a c t i v i t y i n serum ( M i l l e r , 1974). As w ith th e o t h e r m i n e r a l s , d i a g n o s i s o f copper s t a t u s i s b e t t e r made by a c o m b in a tio n o f o b s e r v i n g c l i n i c a l symptoms, animal performance, and response to supplem entation, and taking biochem ical measurements. C o b a lt According to P u l s (1981), a d e q u a t e c o b a l t b l o o d se rum i n r u m i n a n t s i s 0.04 t o 0.06 u g / 1 0 0 m l , m a r g i n a l o r b o r d e r l i n e d e f i c i e n t i s 0.025 t o 0.035 u g / 1 0 0 m l , and d e f i c i e n t i s 0.004 t o 0.02 ug/100 ml. Measurement o f c o b a l t in serum i s d i f f i c u l t due t o t h e low c o n c e n t r a t i o n s p r e s e n t . B a r f o o t and P r i t c h a r d (1980) r e p o r t a wide v a r i a t i o n o f human serum c o b a l t v a l u e s depending on the t e c h n iq u e used. ug/100 ml. The v a l u e s r e p o r t e d range from 0.003 t o 110 Using f l a m e l e s s atomic a b s o r p t i o n s p e c tr o p h o to m e tr y t h e a u t h o r s m e a s u r e d an a v e r a g e o f 0.12 t o 0.20 u g / 1 0 0 ml i n se ru m o f h e a l t h y a d u l t human b e i n g s . McAdam and O ' D e l l (1982), a l s o u s i n g atomic a b s o r p t i o n , measured c o b a l t and o t h e r m i n e r a l s in the plasm a of g estatio n . d airy cows during a whole lactatio n and At t h e f o u r t h week a f t e r c a l v i n g p l a s m a c o b a l t was 100 b e tw e e n 8 and 9 u g / 1 0 0 m l; t h e n i t d r o p p e d t o v a l u e s b e t w e e n 5 and 6 u g / 1 0 0 ml i n t h e t e n t h t o t h e 2 2 t h week, and r o s e a g a i n t o v a l u e s between 7 and 8 ug/100 ml from t h e 28th t o 46th week. The se rum c o b a l t v a l u e s were s i m i l a r f o r young cows ( f i r s t - c a l f h e i f e r s ) and mature cows (two or more c a l v i n g s ) , and f o r a n im a ls f e d p l a i n s a l t and t r a c e m i n e r a l s a l t c o n t a i n i n g 0.007 c o b a l t . The g e n e r a l a v e r a g e f o r a l l t r e a t m e n t s t h r o u g h o u t l a c t a t i o n was 7.6 u g / 1 0 0 m l . Due t o t h e a n a l y t i c a l d i f f i c u l t i e s and t h e v a r i a t i o n of the v a l u e s r e p o r t e d , se ru m a n a l y s i s i s p e r h a p s n o t t h e b e s t way t o d i a g n o s e c o b a l t d e f i c i e n c i e s in c a t t l e . The a n a l y s e s o f v i t a m i n B12 i n b l o o d , liv e r and rumen f l u i d d e te rm in e c o b a l t s t a t u s . c a n be good m e t h o d s t o Since c o b a l t d e f i c i e n c y i s a r e g i o n a l problem , c o b a l t a n a l y s i s i n t h e s o i l and i n p a s t u r e s i s a h e l p f u l guide t o t h e a n i m a l ' s c o b a l t s t a t u s ( M i l l e r , 1974). Manganese Normal manganese l e v e l s in b lood serum o f c a t t l e a r e around 2 t o 3 u g / 1 0 0 ml (Ch u rch, 1976). Puls (1981) c o n s i d e r s 0.5 u g / 1 0 0 ml a m a r g i n a l o r b o r d e r l i n e m ang an ese c o n c e n t r a t i o n i n b lo o d serum, and 0.6 t o 3.0 ug/100 ml a dequate . The m a n g a n es e c o n t e n t o f m o st body t i s s u e s i s r e m a r k a b l y resistan t to change b ecause of redu ction occurs a n im a l s ( M i l l e r , in the 1974). liv e r, low i n t a k e . bone, H ow eve r, some and h a i r o f d e f i c i e n t M onitorin g feed l e v e l s seems t o be t h e b e s t d i a g n o s t i c a i d f o r d e t e r m i n i n g m an g a n ese s t a t u s i n c a t t l e ( P u l s , 1981). 101 Selenium The c o n c e n t r a t i o n of s e l e n i u m in an a n i m a l 's blood i s a good in d ic a to r of e ith e r s e l e n i u m d e f i c i e n c y or a d e q u a c y . Blood plas ma l e v e l s o f 1 t o 5 ug/100 ml i n d i c a t e se len iu m d e f i c i e n c y ; s e l e n i u m s h o u l d be added t o t h e d i e t . u g / 1 0 0 ml i s d e s i r a b l e . A b lood l e v e l o f about 10 B l o o d l e v e l s o f a b o u t 20 u g / 1 0 0 ml o r h i g h e r i n d i c a t e t h a t t h e a n i m a l i s r e c e i v i n g t o o much s e l e n i u m and t h a t a t o x i c s i t u a t i o n may e x i s t (Marczewski e t a l , 1982). A n a l y s i s o f g l u t a t h i o n e p e r o x i d a s e and m e a s u r e m e n t o f t h e selenium c o n te n t of t h e d i e t c a n a l s o be used t o e s t a b l i s h s e l e n i u m s t a t u s and t h e a d e q u a c y o f t h e d i e t f o r t h e t h e a n i m a l (M iller, 1974). Iodine A dequate io d in e co n ten t in b lo o d serum o f c a t t l e is c o n s i d e r e d t o be 15 t o 40 u g / 1 0 0 m l , d e f i c i e n t t o be 3 t o 10 ug/100 m l, e x c e s s i v e t o be 90 t o 300, and c h r o n i c a l l y t o x i c t o be 200 t o 1500 ug/100 ml ( P u ls , 1981). Feed i o d i n e i s n o t w i d e l y u s e d i n d i a g n o s i n g a d e f i c i e n c y p r o b l e m , e s p e c i a l l y when g o i t r o g e n s a r e i n c l u d e d i n t h e d i e t . P r o b a b l y t h e b e s t d i a g n o s t i c h e l p i s a k n o w le d g e o f t h e a r e a , since iodine d e fic ie n c y is a problem in lo calized regions. I o d i n e d e f i c i e n t a r e a s a r e known f o r most p a r t s of t h e w o r l d , and a r e mapped w ith t h e h e l p o f c l i n i c a l o b s e r v a t i o n s and s t a t i s t i c s o f g o i t e r o c c u r r e n c e , e s p e c i a l l y i n humans (NRC, 1970). Blood A n a l y s i s Blood i s t h e most w i d e ly used t i s s u e f o r s t u d i e s in m i n e r a l nutrition. I t r e f l e c t s t h e m i n e r a l s t a t u s o f t h e a n i m a l , and can 102 be o b t a i n e d f r e q u e n t l y and e a s i l y w i t h o u t harm t o t h e a n i m a l (Underwood, 1 9 8 1). The normal values or normal range of c o n c e n t r a t i o n s i n t h e b l o o d se ru m o r p l a s m a o f h e a l t h y f ar m a n i m a l s c on su m ing s a t i s f a c t o r y d i e t s a r e known f o r m o st o f t h e n u t r i t i o n a l l y i m p o r t a n t m i n e r a l s f o r comparison w ith t h o s e i n the b lo o d o f a n im a l s under s t u d y (Church, 1976; P u l s , 1981; Underwood 1977 and 1981) . Most o f t h e b l o o d m i n e r a l a n a l y s i s a r e made i n p l a s m a o r s e r u m , and t h e r e s u l t s a r e e q u i v a l e n t . C a r e m u st be t a k e n t o a void hemolysis o f red blood c e l l s (Fick e t a l . , 1979). A v a rie ty of a n a l y t i c a l te c h n iq u e s a re used fo r d e t e r m i n a t i o n of m i n e r a l s i n b lo od . the The most commonly used a re flame atomic a b s o r p t i o n f o r most o f t h e m i n e r a l s , c o l o r i m e t r y f o r phospho rus, and f l u o r i m e t r y f o r se len iu m . Since manganese l e v e l s i n plas ma or serum a r e below t h e d e t e c t i o n l i m i t s o f flam e .atomic a b s o r p t i o n , f l a m e l e s s a t o m i c a b s o r p t i o n i s u se d i n t h i s c a s e ( U l l r e y , 1977). F l a m e l e s s atomic a b s o r p t i o n can a l s o be used to d ete rm in e c o b a l t (Barfoot and P r i t c h a r d , 1980). Techniques t h a t p e r m i t t h e d e t e r m i n a t i o n o f s e v e r a l e le m e n t s a t once a r e used i n some l a b o r a t o r i e s . These i n c l u d e n e u tr o n a c t i v a t i o n (Ehmann and J a n g h o r b a n i , 1979); p l a s m a e m i s s i o n , and i n d u c t i v e l y c o u p l e d plas ma d i s c h a r g e s p e c t r o p h o t o m e t r y (Barnes, 1979). 103 G a s t r o i n t e s t i n a l P a r a s i t i s m i n D airy C a t t l e A knowledge of the degree of parasite in festatio n is necessary to diagnose m ineral or n u t r i t i o n a l d e f i c ie n c i e s in c a t t l e , since symptoms of p a r a s i t i s m can o f t e n be c on fused w ith n u t r i t i o n a l problem s (Underwood, 1981). P a r a s itiz e d anim als, for e x a m p l e , a r e e i t h e r more s u s c e p t i b l e t o c o p p e r d e f i c i e n c y , o r c o p p e r d e f i c i e n t a n i m a l s a r e more s u s c e p t i b l e ( P u l s , 1981). to p a ra s itis m Anemia, e m a c i a t i o n , poor h a i r c o n d i t i o n , and o t h e r symptoms due t o p a r a s i t i s m can be c o n f u s e d w i t h c o p p e r , i r o n o r o t h e r m i n e r a l d e f i c i e n c i e s or t o x i c i t i e s . be t r u e : The c o n t r a r y can a l s o symptoms o f m i n e r a l d e f i c i e n c i e s can be a t t r i b u t e d t o parasitism . The m o st common sto m ac h worms o f c a t t l e a r e Haemonchus p l a c e i , O s t e r t a g i a o s t e r t a g i and T r i c h o s t r o n g i l u s a x e i . species belong tr e m a t o d e s , to the class of the nematodes. These Among t h e F a s c i o l a h e p a t i c a i s t h e most i m p o r t a n t p a r a s i t e o f d o m e s t i c r u m i n a n t s and t h e m ost common c a u s e o f l i v e r fluke d i s e a s e i n t h e U n i t e d S t a t e s and o t h e r t e m p e r a t e a r e a s o f t h e w o rld . The p r o t o z o a n s E im eria z u e r n i i and E im eria b o v i s a r e th e s p e c i e s o f c o c c i d i a most o f t e n a s s o c i a t e d w ith c l i n i c a l c a s e s o f co c c id io sis in c a t t l e (Merck, 1979). Nematodes I n 198 0, t h e r e w ere a p p r o x i m a t e l y 10.9 m i l l i o n d a i r y cows and 4.2 m i l l i o n d a i r y r ep la ce m e n t h e i f e r s in t h e U n ite d S t a t e s . A l t h o u g h s u r v e y s show a h i g h p r e v a l e n c e o f n e m a to d e i n f e c t i o n n a t i o n w i d e i n a d u l t d a i r y cows, m o st show low worm b u r d e n s and egg c o u n t s o f l e s s t h a n 10 e p g . The q u e s t i o n o f w h e t h e r l o w - 104 l e v e l nematode i n f e c t i o n s reduce m i l k p r o d u c t i o n i n c o m m e r c i a l d a i r y cows i s c o n t r o v e r s i a l . The e f f e c t s o f p a r a s i t i s m in a d u l t cows appear t o depend p a r t l y on r e g i o n a l d i f f e r e n c e s in p a s t u r e v e r s u s d r y l o t management . t h a t both c l i n i c a l T h e r e i s more c o n s i s t e n t a g r e e m e n t and s u b c l i n i c a l p arasitism resu lt in s u b s t a n t i a l economic l o s s e s in th e r a i s i n g of d a i r y re p la c e m e n t h eifers. H eavy worm b u r d e n s and h i g h egg c o u n t v a l u e s c a n be found i n p a s t u r e d d a i r y c a l v e s and y e a r l i n g s which may approach the l e v e l s fo u n d i n h e a v i l y p a r a s i t i z e d young b e e f a n i m a l s . A n th e lm in tic c o n t r o l of t h i s c ateg o ry of anim als r e s u l t s in i m p r o v e d w e i g h t g a i n , and t h e r e i s e v i d e n c e t h a t d a i r y h e i f e r s p r o t e c t e d from s u b c l i n i c a l p a r a s i t i s m may produce s i g n i f i c a n t l y more m i l k i n t h e i r f i r s t l a c t a t i o n compared t o u n t r e a t e d c o n t r o l a n i m a l s (American Assoc. V et. P a t h o l o g i s t s , 1983). Trematodes In c a ttle , the liv e r flu k es F ascio la h ep atica and F a s c i o l o i d e s magna a r e r e s p o n s i b l e f o r t h e condemnation of 1 t o 1.5 m i l l i o n liv e rs annually at slaughter inspections. In a d d itio n to th ese l o s s e s , re p o rts in c re a s in g ly in d ic a te th a t i n d i r e c t l o s s e s due t o f a s c i o l a s i s d u rin g t h e a n i m a l 's growth and p r o d u c t i o n p h a s e s may be f a r g r e a t e r . I n d ire c t lo s s e s include r e d u c t i o n i n a v e r a g e d a i l y weight g a in and lower fee d c o n v e r s i o n r a t i o s in the f e e d l o t , reduced m i l k p r o d u c t i o n in d a i r y c a t t l e , and r e d u c e d h e r d p e r f o r m a n c e i n c o w - c a l f o p e r a t i o n s (American Assoc. V et. P a t h o l o g i s t s , 1983). Protozoa C o c c i d i o s i s due t o E i m e r i a s p . i s a common d i s e a s e o f t h e 105 g a s t r o i n t e s t i n a l t r a c t o f r u m in a n ts . are t h e m o st p a t h o g e n i c o f the E im eria z u r n i i and Eh b o v i s 14 s p e c i e s fou nd i n c a t t l e . V i r t u a l l y e v e r y a n im al becomes i n f e c t e d with one or more E im eria sp e cie s during i t s l i f e t i m e . The d i s e a s e i s i n s i d i o u s and i s o f t e n d i a g n o s e d o n l y a f t e r t h e a n i m a l show c l i n i c a l s i g n s o f d i a r r h e a , d e b i l i t a t i o n , or r e f u s a l o f feed. C o c c i d i o s i s i s most c l i n i c a l l y i m p o r t a n t in f e e d l o t s , among young d a i r y a n i m a l s , and i n o t h e r s i t u a t i o n s whe re y o u n g , u n e x p o s e d s t o c k a r e p l a c e d i n c o n ta m in a te d , confined areas (American Assoc. Vet. P a t h o l o g i s t s , 1983) . Control The m o s t w i d e l y chemotherapy. in c a t t l e : used m easure of p a r a s i t e At p r e s e n t , is 6 a n t h e l m i n t i c s a r e approved f o r use th iab en d azo le, p h e n o t h i a z i n e and m o r a n t e l . c o n tro l lev am iso le, co umaphos, haloxon, T h ia b e n d a z o l e ( s o l d under th e brand names of T h ia b en , B o v i z o l e , P o l i v a l , e tc .) and l e v a m i s o l e ( a l s o known a s T e t r a m i s o l e , R i p e r c o l , L e v a s o l e , T r a m i s o l , e t c . ) h a v e high d e g re e s o f e f f i c a c y a g a i n s t a d u l t g a s t r o i n t e s t i n a l nematodes and some l a r v a e , and t h e y a r e t h e most w i d e ly used. com parable in e f f ic a c y . Levam isol is also M o r a n te l i s activ e against lungworms. M i l k from cows t r e a t e d w ith coumaphos does no t have to be w i t h d r a w n fro m s a l e ; h o w e v e r , m i l k from cows t r e a t e d w i t h o t h e r a n t h e l m i n t i c s m ust be w i t h d r a w n f o r a s p e c i f i e d p e r i o d a f t e r th e cows a r e t r e a t e d . New a n t h e l m i n t i c s r e c e n t l y approved o r i n t h e p r o c e s s o f a p p r o v a l by t h e FDA a r e t h e b e n z i m i d a z o l e d e r i v a t i v e s a l b e n d a z o l e , f e n b e n d a z o l e , and o x f e n d a z o l e , and i v e r m e c t i n (American Assoc. V et. P a t h o l o g i s t s , 1983). 106 There i s no f l u k i c i d a l drug a v a i l a b l e i n t h e U n ited S t a t e s t h a t i s f u l l y approve d f o r use in l i v e s t o c k by t h e Food and Drug A d m inistration. At one t i m e , h e x a c h l o r o e t h a n e was w i d e l y use d o n c e o r t w i c e a y e a r f o r c o n t r o l o f f a s c i o l a s i s i n c a t t l e and sm all ru m in an ts. h ex ach lo ro eth an e D eclared was rem oved a p o ten tial from the carcin o g en , m arket in 1979. A l b e n d a z o l e , a b r o a d - s p e c t r u m a n t h e l m i n t i c s t i l l bein g t e s t e d , was s u b s e q u e n t l y approved f o r emergency use a g a i n s t and E\ magna i n c a t t l e and sheep. l i m i t the p o t e n t i a l e c o n o m ic l o s s e s . hepatica R e s t r i c t i o n s on use , however, e f f e c t i v e n e s s of t h i s drug in reducing I t i s n o t f o r use i n l a c t a t i n g a n i m a l s , t h e w i t h d r a w a l p e r i o d i s 180 d a y s , i t i s n o t f o r u s e i n t h e f i r s t 45 days o f g e s t a t i o n , and i t can o n l y be o b t a i n e d from v e t e r i n a r i a n s who a r e responsible for m aintaining p r e - and p o s t t r e a t m e n t reports. Albendazole is e ff ic a c io u s a g a in st a d u l t h epatica in c a t t l e and sh e ep , b u t a l i k e h e x a c h lo r o e th a n e has l i t t l e e f f e c t on i m m a tu r e f l u k e s (American A s s o c . V e t . P a t h o l o g i s t s , 1 9 83 ). In o t h e r c o u n t r i e s , however, t h e r e a r e s e v e r a l f l u k i c i d e s a v a i l a b l e for c a t t l e in clu d in g rafoxanide, b r o t i a n i d e and n i t r o x y n i l . These compounds can a l s o k i l l immature f l u k e s (Merck, 1979). C o ccid io sis can be p r e v e n t e d c o n d i t i o n s when a n i m a l s , c on fin em en t. by m a i n t a i n i n g s a n i t a r y e s p e c i a l l y th e young, are kept in The prim ary u s e f u l n e s s of a n t i c o c c i d i a l drugs i s t o a r r e s t f u r t h e r s p r e a d of i n f e c t i o n among a n im a l s . C ertain s u lf a d rug s and amprolium a r e the o n l y drugs p r e s e n t l y approved f o r use (American Assoc. Vet. P a t h o l o g i s t s , 1983). Chemotherapy k i l l s a d u l t worms and i s e f f e c t i v e in t r e a t i n g 107 c l i n i c a l l y a f f e c t e d a n i m a l s , b u t i t does no t n e c e s s a r i l y p r o v i d e lo n g -te rm R einfectio n b e n efits may o c c u r Optimum p r e v e n t i v e several of p re v e n tin g natu rally . the in te rv al grazing co n tam in atio n . b e tw e e n c o n t r o l programs i n v o l v e approaches: anth elm intics, in p astu re m anagement, treatm ents. i n t e g r a t i o n of strateg ic u se of and use o f t h e h o s t ' s a b i l i t y t o a c q u i r e immunity The s t r a t e g y is (American Assoc. Vet. P a t h o l o g i s t s , 1983): 1) t o p r e v e n t t h e b u i l d u p of dangerous numbers o f i n f e c t i v e s t a g e s on p a s t u r e s by re ducing c o n ta m i n a ti o n with f e c a l eggs or la r v a e a t c r i t i c a l periods; 2) t o r e d u c e a c q u i s i t i o n o f i n f e c t i o n s by a n t i c i p a t i n g p e r i o d s d u r i n g which l a r g e numbers of l a r v a e a r e l i k e l y t o occur; and 3) t o remove s u s c e p t i b l e a n im a ls from h e a v i l y contaminated p a stu re before these periods. The e s s e n t i a l r e q u i r e m e n t of i n t e g r a t e d , p r e v e n t i v e c o n t r o l is the p r o v i s i o n of "safe" p a s tu re fo r s u s c e p t i b l e anim als a t a p p r o p r i a t e tim es (American Assoc. Vet. P a t h o l o g i s t s , 1983). D ia g n o sis The c l i n i c a l sig n s asso ciated w ith g astro in testin al p a r a s i t i s m a r e s h a r e d with many d i s e a s e s and c o n d i t i o n s ; however, p r e s u m p t i v e d i a g n o s i s b a s e d on h i s t o r y and sypmtoms i s o f t e n j u s t i f i e d and i n f e c t i o n can u s u a l l y be confirmed by t h e pr e s e n c e o f eggs i n f e c a l m a t t e r . I n e v a l u a t i n g t h e c l i n i c a l importance o f f e c a l e x am in a tio n i t i s im p o r tan t t o c o n s i d e r t h a t th e number o f e g g s p e r gram o f f e c e s i s n o t an a c c u r a t e i n d i c a t i o n o f t h e 108 number o f a d u l t worms. N e g a t i v e c o u n t s can be found d e s p i t e t h e p r e s e n c e of a l a r g e number o f immature worms, due t o s u p p r e s s i o n o f egg p r o d u c t i o n by immune r e a c t i o n o r p r e v i o u s a n t h e l m i n t i c treatm en t and v a ria tio n d i f f e r e n t worms. in the egg -p ro ducin g c a p a c ity of On t h e o t h e r hand, eggs i s d i f f i c u l t and i m p r a c t i c a l . the m ost d irect m ethod of s p e c if ic i d e n t i f i c a t i o n of Postmortem ex am in a tio n s a r e id en tify in g and q u a n titiz in g g a s t r o i n t e s t i n a l p a r a s i t i s m s (Merck, 1979). At p r e s e n t t h e r e a r e no immunologic t e c h n iq u e s a v a i l a b l e f o r p r a c t i c a l use in antemortem a sse ss m e n t of t h e e x t e n t o f nematode p arasitism . plasm a pepsinogen tests for d iag n o sis of o s t e r t a g i a s i s have been used e s s e n t i a l l y as a s u r v e y m o n ito rin g to o l, b u t s u c h t e s t s a r e m o st u s e f u l when a n i m a l s a r e b e i n g t e s t e d r e p e a t e d l y o v e r an e x t e n d e d p e r i o d . in d icates that sero lo g ic al procedures Recent e x p e rie n c e may h a v e value for d i a g n o s i s o f F. h e p a t i c a and F. magna i n f e c t i o n s , com pa red w i t h t im e c onsum in g fecal exam inations. There are no r e l i a b l e antemortem p a r a s i t o l o g i c d i a g n o s t i c methods f o r c e s t o d e s or th e im p o rtan t protozoans Pathologists, 1983). in an im als (Am erican A ssoc. V et. MATERIALS AND METHODS S a m p l e s were t a k e n from t h r e e f a r m s i n e a c h o f f i v e m i l k p r o d u c i n g r e g i o n s a r o u n d Riobamba ( a l t i t u d e 2,754 m, 1 ° 40' S, 78° 39' W) t h e c a p i t a l o f t h e Ch im bo ra zo p r o v i n c e i n E c u a d o r . The r e g i o n s s a m p l e d w ere t h e most i m p o r t a n t i n m i l k p r o d u c t i o n f o r t h e c i t y , and r a n g e d i n a l t i t u d e fro m a r o u n d 3 ,0 0 0 m (9,8 40 ft) t o 4000 m ( 1 3,12 0 f t ) . The r e g i o n s c h o s e n c o r r e s p o n d t o d i f f e r e n t g e o l o g i c a l f o r m a t i o n s on t h e s l o p e s o f t h e Ande s. Average t e m p e r a t u r e s i n t h e r e g i o n s range from 6 t o 11° C (43 t o 52° F) t h r o u g h o u t t h e y e a r . F r o s t i n t h e m o r n i n g s i s common a t these a lt i tu d e s . mm (40 i ) . 1979). P r e c i p i t a t i o n ranges from 400 mm (16 i) t o 1200 The d r y s e a s o n l a s t s from J u l y t o S e p t e m b e r (Ter&n, Most o f t h e farms had some form of i r r i g a t i o n a t th e time t h e sam p le s were t a k e n ( J u l y t o September 1982). One d a i r y farm i n t h e U nited S t a t e s , l o c a t e d in Shiawasee coun ty i n t h e S t a t e of M i c h i g a n , was a l s o s a m p l e d f o r c o m p a r i s o n w i t h t h e f a r m s i n Ecuador. T a b l e 1 shows t h e names of t h e r e g i o n s , t h e i r a l t i t u d e above s e a l e v e l , and t h e i r approximate g e o g r a p h i c a l c o o r d i n a t e s . B l o o d se ru m s a m p l e s were t a k e n on e a c h farm from t h e t a i l v e i n or a r t e r y o f 10 a d u l t m i l k i n g cows and 10 a n im a l s under one y ear of age. A p p r o x i m a t e l y 30 ml o f b l o o d were c o l l e c t e d from each an im al i n t e s t t u b e s w i t h o u t c o a g u l a n t . Blood sam p le s were l e f t s t a n d i n g a t room t e m p e r a t u r e from 4 t o 10 h o u r s p r i o r t o centrifugation. The t e s t t u b e s with b lood were t h e n c a r r i e d to t h e l a b o r a t o r y where t h e y were c e n t r i f u g e d and t h e b l o o d s e ru m was separated. Blood serum 109 was stored frozen in p lastic no T able 1. A l t i t u d e above se a l e v e l and approximate g e o g r a p h i c a l coordinates o f f i v e r e g i o n s from t h e Chimborazo p r o v i n c e o f Ecuador and one r e g i o n i n Shiawasee c o u n ty , Michigan (1) REGION ALTITUDE ABOVE SEA LEVEL NAME LONGITUDE m LATITUDE degrees-min-sec 1 ECUADOR Chambo 2900 S 1°40'30 " W 78°30'33 2 ECUADOR San Juan 3200 S 1 °3 0 126 " W 78°40'46 3 ECUADOR San Andr&s 3600 S 1°29'5 7 '1 w 7 8 ° 4 0 ' 15 4 ECUADOR Guamote 3200 S 1°50'4 2 '' w 78°40'16 5 ECUADOR Quimiac 3000 S 1°30'42 " w 78°30'16 6 MICHIGAN L ain sbu rg (1) N,S: North, meters 240 South l o n g i t u t e ; N 42 °57' 3 3 ' 1 W: West w 84°19'51 latitude; m: 111 con tain ers. Serum was thaw ed a t room t e m p e r a t u r e p r i o r to analysis. F i v e composite sa m ple s o f p a s t u r e s and s o i l s were take n from each farm. S o i l and p a s t u r e s a m p l e s were c o l l e c t e d from e a c h f i e l d (2 -5 h e c t a r e s ) by w a l k i n g i n z i g - z a g l i n e . A t o t a l o f 20 t o 50 sa m ple s were c o l l e c t e d from each f i e l d . S o i l s a m p l e s w e r e t a k e n w i t h a s o i l p r o b e a t a d e p t h o f 15 t o 20 cm. Samples were a i r d r i e d a t room t e m p e r a t u re . Dry s o i l s a m p l e s were t h e n c r u s h e d u n t i l a m a jo r p o r t i o n o f t h e s a m p l e p a s s e d a 10-mesh (U.S. No. 10) s i e v e . P astu re sam p les were taken a p p r o x i m a t e ly 20 cm from t h e ground. by hand at a h eig h t of H a l f o f each p a s t u r e sample was washed w i t h d i s t i l l e d w a t e r t o a s s e s s s o i l c o n t a m i n a t i o n . P a s t u r e s a m p l e s were d r i e d i n f o r c e d a i r o v e n s a t 6 0 ° C and ground t o a p a r t i c l e s i z e o f a p r o x i m a t e l y 1 mm. Grab sa m ple s of f e c e s f o r p a r a s i t e a n a l y s i s were t a k e n from e a c h a n i m a l t h a t was b l e d . F e c e s s a m p l e s were k e p t i n p l a s t i c b a g s and r e f r i g e r a t e d u n t i l t h e y were a n a l y z e d w i t h i n 24 h o u r s after co llection. A s p l i t p lo t design (G ill, 1 9 7 8 a f b and c) was u s e d t o a n a l y z e t h e r e s u l t s ( T a b l e 2 ) , and t h e c o n t r a s t s among a l l t h e means of t h e r e g i o n s were t e s t e d w ith a B o n f e rr o n i t t e s t ( G i l l , 1 9 7 8 a , Games, 1 9 77). The SPSS ( S t a t i s t i c a l P a c k a g e f o r the S o c i a l Sciences) program was used i n t h e computer p r o c e s s i n g of t h e d a t a (Nie e t a l . , 1975; H u l l and N i e , 1 981). S o i l samples were t a k e n , p r e p a r e d and a n a l y z e d a cc o rd in g t o t h e p r o c e d u r e s recommended f o r t h e N o r t h C e n t r a l R e g io n o f t h e 112 T ab le 2. S t a t i s t i c a l d e s i g n s f o r th e a n a l y s i s o f s o i l , and blood d a t a (1) pasture, SOIL Degrees of freedom Source o f v a r i a t i o n REGION FARMS/REGION SAMPLES/FARM/REGION 5 10 72 TOTAL 87 Farms r e g i o n i s t h e e r r o r term f o r sam ples/farm /region is the error farm s/region region, term and for PASTURE AND BLOOD Degrees o f freedom Source o f v a r i a t i o n PASTURE BLOOD REGION FARMS/REGION TYPE OF SAMPLE REGION X TYPE FARMS/REGION X TYPE SAMPLES/FARM/REGION/TYPE 5 10 1 5 10 130 5 10 1 5 10 288 TOTAL 161 319 Farms/region is the error term for region, and s a m p l e s / f a r m / r e g i o n / t y p e p l u s f a r m s / r e g i o n X type i s t h e e r r o r term f o r f a r m s / r e g i o n , t y p e , and fo r the i n t e r a c t i o n r e g i o n X typ e (1) G i l l , 1978a, b and c 1.13 United S t a t e s ( B u l l e t i n No. 499, 1980). with Bray-1 s o l u t i o n (Knudsen, 1980). Phosphorus was e x t r a c t e d C alcium , magnesium, sodium and p o t a s s i u m w ere e x t r a c t e d w i t h IN ammonium a c e t a t e o f pH 7.0 ( C a rs o n , 1 9 8 0 ). manganese, Co p pe r zinc and was e x t r a c t e d co b alt were with IN HC1. extracted with Iron, 0.1 N HC1 (Whitney, 1 98 0 ). Molybdenum was e x t r a c t e d w i t h Tamm's r e a g e n t : ammonium o x a l a t e s o l u t i o n a t pH 3.3 ( R e i s e n a u e r , 1965). S ulfur was e x t r a c t e d w i t h m o n o c a l c i u m p h o s p h a t e s o l u t i o n (500 ppm P) ( E ik , 1980). N i t r a t e s w ere e x t r a c t e d w i t h a s a t u r a t e d s o l u t i o n o f c a lc iu m hydroxide (Carson, 1980). T o t a l s e l e n i u m in t h e s o i l was d e t e r m i n e d a f t e r w e t d i g e s t i o n w i t h n i t r i c and p e r c h l o r i c a c i d (Whetter and U l l r e y , 1978). Pasture sam ples w ere taken, prepared and a n a l y z e d in accordance w i t h t h e p r o c e d u r e s o f t h e U n i v e r s i t y o f F l o r i d a (Pick e t a l . , 1979). H a l f o f t h e f r e s h p a s t u r e sample from each f i e l d was washed w i t h d i s t i l l e d w a t e r t o a s s e s s s o i l c o n t a m i n a t i o n . Selenium c o n t e n t was d e te r m in e d a f t e r wet d i g e s t i o n with n i t r i c and p e r c h l o r i c a c i d ( W h e t te r and U l l r e y , 197 8). To m e a s u r e t h e amou nt s o f o t h e r m e t a l s i n t h e p a s t u r e s , s a m p l e s were a s h e d o v e r n i g h t a t 600° C and t h e ash d i s s o l v e d with h y d r o c h l o r i c a c id (Fic k e t a l . , 1979). Blood serum sam ple s were d e p r o t e i n i z e d with t r i c h l o r o a c e t i c a c i d (Fick e t a l . , wet d i g e s t i o n p e rc h lo ric acid 1979). of the Selenium c o n t e n t was determined a f t e r w h o le serum sa m p le w ith n i t r i c (W hetter and U l l r e y , 1978). and To d e t e r m i n e man ganese c o n t e n t , t h e se rum s a m p l e s were mixed 1:1 w i t h w a t e r . Ten serum s a m p l e s were p o o l e d f o r c o b a l t a n a l y s i s . Ten ml o f 114 serum were f r e e z e d r i e d and a s h e d a t 600° C o v e r n i g h t . T h e s e a s h e s were d i s s o l v e d w i t h HC1, c h e l a t e d w ith l - n i t r o s o - 2 - n a p h t h o l and e x t r a c t e d with c h lo r o f o r m . A fter ev ap oration to dryness, the s a m p l e s were r e d i s s o l v e d w i t h 0.5 ml c h l o r o f o r m f o r analysis (Barfoot and P r i t c h a r d , cobalt 1980). The pH o f s o i l s was d ete rm in ed by suspending 5 g o f s o i l in 5 ml o f water (McLean, 1980). T e x tu r e o f s o i l s was dete rm ined by t h e Bouyoucus method (Bouyoucos, 1951). Organic m a t t e r i n s o i l s was measured as carbon a f t e r o x i d a t i o n w ith p otassium dich rom ate by t i t r a t i o n w i t h f e r r o i n i n d i c a t o r ( S c h u l t e , 1980). N itrate c o n t e n t i n s o i l s was d e t e r m i n e d w i t h t h e p h e n o l d i s u l f o n i c a c i d method (Carson, 1980). su lfate content su lfates. The t u r b i d i m e t r i c d e t e r m i n a t i o n o f barium (Eik, 1980) was used for the an aly sis of The ash , c ru d e p r o t e i n and crude f i b e r c o m p ositio n of t h e p a s t u r e s was d e t e r m i n e d a c c o r d i n g procedures. t o t h e A.O.A.C. (1975) P h o s p h o r u s i n s o i l s , p a s t u r e s and b l o o d se rum was m e a s u r e d c o l o r i m e t r i c a l l y a s p h o s p h o m o l y b d i c a c i d a t 600 nm ( H a r r i s and P o p a t , 1 9 5 4 ). Selenium c o n te n t in s o i l s , p a s tu r e s and b l o o d se rum was d e t e r m i n e d f l u o r i m e t r i c a l l y U l l r e y , 1 9 78). ( W h e tte r and Molybdenum c o n t e n t i n s o i l s and p a s t u r e s , and c o b a l t and manganese c o n t e n t in s o i l s , p a s t u r e s and b l o o d serum was de te rmined by f l a m e l e s s atomic a b s o r p t i o n s p e c t r o p h o t o m e t r y (Perk in, 1981). blood serum A l l o t h e r m e t a l c o n t e n t s in s o i l s , p a s t u r e s and were d eterm in ed u sin g ato m ic a b so rp tio n s p e c t r o p h o t o m e t r y w i t h an a i r - a c e t y l e n e f l a m e ( P e r k i n , 1982). P a r a s i t e egg c o u n t s were d e t e r m i n e d by t h e d i r e c t f l o t a t i o n m ethod (Cox a n d T o d d , 1 9 6 2 ). F a s c i o l a h e p a t i c a e g g s were 115 determined usin g a f l u k e ov a s e d i m e n t a t i o n te c h n iq u e a l . ,1 9 5 4 ) . (Dennis e t RESULTS AND DISCUSSION T his c h a p t e r of r e s u l t s and d i s c u s s i o n i s d i v i d e d i n t o fou r parts: 3) 1) m in erals in so ils; m i n e r a l s i n blo od ; and 4) 2) n u trie n ts in pastures; g a stro in te stin a l parasites. The l e v e l s of m i n e r a l s found by s o i l a n a l y s i s i n the p r e s e n t i n v e s t i g a t i o n were co m pa red w i t h l e v e l s a t w hich t h e r e i s a p o s s i b l e re s p o n se of a c ro p t o f e r t i l i z a t i o n , whenever t h e r e was in fo rm atio n av aila b le on th is in the lite ra tu re . The i m p l i c a t i o n s f o r f o r a g e p r o d u c t i o n o f t h e l e v e l o f m i n e r a l s found i n t h e s o i l s , a s w e l l a s t h e e f f e c t o f s o i l pH, t e x t u r e , and org an ic m atter co n ten t, are discussed. Where a p p r o p i a t e , recommendations f o r f e r t i l i z a t i o n a r e made. The c o n c e n t r a t i o n s fo u n d in th is study of n u t r i e n t s in p a s t u r e s a r e c o m pared t o t h e r e q u i r e m e n t s o f a n i m a l s f o r t h e s e nutrients. Whenever th e p a s t u r e s do n o t p r o v i d e adeq uate amounts of a given n u tr ie n t, recommendations f o r s u p p l e m e n t a t i o n of the d i e t a r e made. When t h e c r o p i s r e s p o n s i v e t o f e r t i l i z a t i o n , o r when t h e l e v e l o f an e le m e n t can be i n c r e a s e d thro ugh a d d i t i o n of t h e e le m e n t t o the s o i l , suggestions for f e r t i l i z a t i o n are a ls o made. The c o n c e n t r a t i o n s of m in e ra ls in blood fou n d i n t h i s i n v e s t i g a t i o n a r e c om pared t o v a l u e s c o n s i d e r e d n o r m a l i n t h e lite ra tu re review ed. When t h e m i n e r a l c o n c e n t r a t i o n i n t h e a n im als t e s t e d in t h i s stu d y does no t f a l l w i t h in th e range c o n s i d e r e d t y p i c a l , a n d /o r t h e d i e t i s i n a d e q u a t e , s u g g e s t i o n s on how t o p r e v e n t a d e f i c i e n c y a r e made. 116 F i n a l l y , f e c a l egg c o u n ts f o r g a s t r o i n t e s t i n a l p a r a s i t e s a r e d i s c u s s e d because t h e d e t r i m e n t a l e f f e c t s o f p a r a s i t i s m on animal p ro d u ctio n resem ble deficien cies. the d etrim en tal e ffects of m in eral Suggestions for p a r a s i t e c o n tr o l in th e a re a s s t u d i e d a r e made. 118 M inerals in S o ils F e r t i l i z a t i o n P r a c t i c e s i n Ecuador I n E c u a d o r , p a r t i c u l a r l y i n t h e r e g i o n s where t h e p r e s e n t in v estig atio n fertilized . was c a r r i e d out, pastures g enerally are However, c r o p r o t a t i o n i s a common p r a c t i c e . not After a p e r i o d of y e a r s , g e n e r a l l y four t o s i x , o f d e d i c a t i n g t h e l a n d to p a s tu re , the s o i l i s plow ed, d i s i n f e c t e d and f e r t i l i z e d , u s u a l ly in p r e p a r a tio n fo r p o ta to c u l t i v a t i o n . In t h i s case around 136 kg o f N, 400 kg o f P205, and 136 kg o f K20 a r e a p p l i e d p e r h e c t a r e (120 l b o f N, 360 l b P205, and 120 l b o f K20 p e r acre). A f t e r one t o f o u r y e a r s of use f o r growing the a l t e r n a t e crop, the land is retu rn e d to p a stu re . rye-grass A m ixture of bian n u al (L o l i u m m u l t i f l o r u m ) and w h i t e c l o v e r r e p e n s ) i s t h e most commonly used p a s t u r e seed. sp .) , orchard grass (D a c t y l i s (T r i f o l i u m Fescue (F e s t u c a g l o m e r a t a ) , tim othy (Phleum p r a t e n s e ) , red c l o v e r (T r i f o l i u m p r a t e n s e ) , and o t h e r s p e c i e s a r e used o c c a s i o n a l l y . Some f a r m s grow a l f a l f a , and i n some c a s e s o a t s , r y e o r w h e a t a r e r a i s e d t o be u s e d f o r g r e e n c h o p f o r t h e a n im a l s . I n most o f t h e s e s i t u a t i o n s no c hem ic al f e r t i l i z e r a p p lie d to the s o i l , b u t th e farm er is ta k e s advantage of the r e s i d u a l f e r t i l i t y from t h e p r e v i o u s c ro p. On some o t h e r farms, p a s t u r e s a r e permanent. On t h e s e farms t h e s o i l i s plowed and t h e m i x t u r e o f g r a s s and leg u m e s e e d i s p l a n t e d e v e r y f o u r t o s i x years, g e n e r a lly without s o i l fertilizatio n . Sinc e t h e anim als a r e g r a z i n g on t h e p a s t u r e , m o st o f t h e i r manure r e v e r t s t o t h e field . In M ic h ig a n , in c o n t r a s t , f i e l d s used f o r growing co rn and a l f a l f a , the m ain crops grown f o r anim al forage, are 119 f e r t i l i z e d e v e r y y e a r w i t h n i t r o g e n , p h o s p h o r u s and p o t a s s i u m , and o c c a s i o n a l l y m i c r o e l e m e n t s s u c h a s b o r o n , molybdenum and copper. S o il Analysis M i n e r a l a n a l y s i s of p a s t u r e s and s o i l s i s a v e r y u s e f u l t o o l t o diagn o se d e f i c i e n c i e s or e x c e s s e s i n f o r a g e s f o r a n im a l s . In g e n e r a l , low l e v e l s o f a p a r t i c u l a r e l e m e n t i n t h e s o i l w i l l r e s u l t i n t h e growth o f v e g e t a t i o n low i n t h a t e le m e n t . T h is i n tu rn w i l l produce a d e f i c ie n c y in a n im a ls fed w ith t h a t p l a n t m aterial. The same p r i n c i p l e a p p l i e s t o e x c e s s e s o f m i n e r a l s . M i n e r a l c o n c e n t r a t i o n i n the s o i l does n o t alw ays c o r r e l a t e w e l l w ith t h e m i n e r a l c o n t e n t i n the p l a n t or with t h e m i n e r a l s t a t u s of the an im al. T his i s m a i n l y due t o t h e v a r i a t i o n a b i l i t y of d i f f e r e n t p l a n t sp e cie s, in the or even d i f f e r e n t v a r i e t i e s of t h e same s p e c i e s , i n e x t r a c t i n g m i n e r a l s a l t s from s o i l s , and t o h o m e o s t a t i c m ec hanism s i n t h e a n i m a l s (Underwood, 1981 ). P l a n t t i s s u e a n a l y s i s , combined w i t h s o i l a n a l y s i s , i s u s e d by the s o i l s c i e n t i s t s t o d iagn o se t h e m i n e r a l s t a t u s o f t h e s o i l s (J o n e s, 1972). S o i l pH S o i l s from t h e r e g i o n s o f E c u a d o r and M i c h i g a n ( T a b l e 3, F ig u r e 1), r a n g e d from 5.78 t o 6.71 pH. Out o f a t o t a l samples from i n d i v i d u a l f i e l d s , 11% o f 88 were in t h e range o f 5.00- 5.49 pH, 17% from 5.50 t o 5.99, 26% from 6.00 t o 6 .4 9 , 26% from 6.50 t o 6 .9 9 , 9% fr om 7.00 t o 7 .4 9 , 9% from 7.50 t o 7 .9 9 , and 1% from 8.00 t o sig n ifican t 8.49. (p > . 0 5 ) , The d i f f e r e n c e among r e g i o n s was n o t b u t t h e d i f f e r e n c e among f a r m s w i t h i n Table 3. S o i l pH, o r g a n i c m a t t e r , and t e x t u r e from f i v e r e g i o n s i n th e Chimborazo p r o v in c e o f Ecuador and one r e g i o n i n Shiawasee c o un ty , Michigan (1) pH TEXTURE ORGANIC MATTER % SAND % CLAY % X X X REGION (2) N X 1 ECUADOR 15 6.71 (0.33) 3.8 (1.61) 56 (3.47) 2 ECUADOR 15 6.30 (0.33) 10.6 (1.61) 52 (3.47) 3 ECUADOR 15 5.78 (0.33) 10.9 (1.61) 66 (3.47) 4 ECUADOR 15 7.17 (0.33) 4.9 (1.61) 5 ECUADOR 15 6.58 (0.33) 6 MICHIGAN 13 5.97 (0.36) (SEM) (SEM) (SEM) SILT % (SEM) 19ab (1.42) l 5abc (1.42) X (SEM) 25 (2.64) 33 (2.64) (1.42) 24 (2.64) 60 (3.47) 10c l 4bc (1.42) 27 (2.64) 8.1 (1.61) 65 (3.47) llc (1.42) 24 (2.64) 2.3 (1.73) 55 (3.73) 22a (1.53) 23 (2.94) NS NS ** * S i g n i f i c a n c e of F (3) Region Farm /region (1) (2) (3) NS ** * ** NS NS N, X, SEM: number of o b s e r v a t i o n s , means and s t a n d a r d e r r o r s of means Region means w i t h i n a column w ith o u t a common s u p e r s c r i p t a r e d i f f e r e n t (p < .05) NS: n o n - s i g n i f i c a n t ( p < . 0 5 ) ; **: p < .01; *: p < .05 REGION F ig u r e 1 . S o i l pH in f i v e r e g i o n s ( 1 - 5 ) in t h e Chimborazo p r o v in c e of Ecuador and one r e g io n (6 ) i n S h iaw assee County, M ichigan. 122 regions was h i g h l y sig n ifican t (p < . 0 1 ) . The c o r r e l a t i o n c o e f f i c i e n t among s o i l pH and c a l c i u m i n t h e s o i l s was 0.393. Liming i s n o t a common p r a c t i c e f o r p a s t u r e c u l t i v a t i o n in Ecuador. From t h e f i e l d s t e s t e d , 26% had l e s s t h a n 6.0 pH and may need l im in g f o r b e t t e r f o r a g e p r o d u c t i o n . The recommended 01 f o r a l f a l f a c u l t i v a t i o n i s 6.8 ( C h r i s t e n s o n e t a l . , 1983). In t h e c a s e of mixed p a s t u r e s , a pH o f 6.8 would f a v o r t h e growth o f legumes and improve t h e q u a l i t y o f t h e sward. I n c r e a s e d legume growth augments d ry m a t t e r y i e l d n o t o n l y o f t h e legume b u t a l s o of the g r a s s e s , b e c a u s e more n i t r o g e n i s a v a i l a b l e t o them. T a b l e 1.4 (Appendix I) shows t h e l i m i n g recommendations based on so il pH made by t h e E x t e n s i o n S e r v i c e o f M i c h i g a n S t a t e U n iv ersity . li m i n g . S o i l pH i s n o t , h o w e v e r , t h e b e s t c r i t e r i u m f o r Limestone r e q u i r e m e n ts of t h e s o i l a re b e s t e s t i m a t e d by t h e Shoemaker, McLean and P r a t t ' s method (McLean, 1980). Organic M a tte r Organic m a t t e r s u p p l i e s n u t r i e n t s t o th e s o i l , contributes t o i t s ion exchange c a p a c i t y and improves i t s s t r u c t u r e ( S c h u l t e , 1980). A knowledge o f th e o r g a n i c m a t t e r c o n t e n t i s h e l p f u l in estim atin g the catio n exchange s u p p l y i n g power of t h e s o i l capacity and the n itrogen- ( T i s d a l e and N e l s o n , 1975). m a t t e r c o n t e n t o f Ecuador and Michigan s o i l s Organic (Table 3, F i g u r e 2) r a n g e d from 2.3% i n r e g i o n 6 i n M i c h i g a n t o 10.9% i n r e g i o n 3 i n E c u a d o r , and t h e d i f f e r e n c e among r e g i o n s farms w i t h i n r e g i o n s (p C . 0 5 ) and among (p < .10) was s i g n i f i c a n t . I t i s p o s s i b l e t h a t s o i l s i n E c u a d o r had a h i g h e r o r g a n i c m atter co n tent than s o i l s i n M i c h i g a n b e c a u s e a n i m a l s were (%) MATTER ORGANIC SOIL I m m p REGION F ig u re 2 . S o i l o r g a n ic m atter in f i v e r e g i o n s ( 1 - 5 ) in th e Chimborazo p r o v in c e of Ecuador and one r e g io n (6) in S h iaw assee County, M ich igan . 123 m 1.24 g r a z i n g on them a l l year and t h e r e was a g r e a t e r a c c u m u l a t i o n of m anure. Another p o ssib le ex p lan atio n for the d if f e r e n c e in o r g a n i c m a t t e r c o n t e n t i s t h a t t h e Ecuadorean s o i l samples ta k e n from g r a s s - l e g u m e p a s t u r e s may have c o n t a i n e d more r o o t s than th e Michigan sa m p le s, which were take n from between t h e rows of c ro p s i n a l f a l f a and c orn f i e l d s . D e s p i t e t h e h i g h e r v a l u e s found, i t i s p o s s i b l e t h a t o r g a n i c m a t t e r in t h e Ecuadorean r e g i o n s sampled had l e s s chance of being m e t a b o l i z e d by p l a n t s than the o r g a n i c m a t t e r i n t h e M i c h i g a n s a m p l e s , b e c a u s e o f t h e r e l a t i v e l y low tem peratures p r e v a i l i n g (6 t o 11° C). in t h e s e p a r t s of Ecuador a l l year I n M i c h i g a n , s a m p l e s w ere t a k e n i n t h e month o f September, when t e m p e r a t u re s were r e l a t i v e l y high. S o i l s a r e c o n s i d e r e d o r g a n i c when t h e y h a v e an o r g a n i c m a t t e r c o n t e n t g r e a t e r than 20% (Wrancke and C h r i s t e n s o n , 1980), so t h e s o i l s a n a l y z e d from E c u a d o r and M i c h i g a n f a l l in the c a t e g o r y of m i n e r a l s o i l s . T ex ture S o i l s from t h e r e g i o n s sampled i n Ecuador were m o s t l y sandy loam, w h i l e t h e s o i l s from Michigan ranged from sandy c l a y loam t o sandy loam (Table 3). sig n ific an tly (p > . 0 5 ) . among Sand and s i l t p e r c e n t a g e d i d no t d i f f e r regions or among C lay percentage d i f f e r e d farms w ithin among r e g i o n s regions (p < .0 1 ) , ranging from 10% i n r e g i o n 3 o f Ecuador t o 22% i n t h e s o i l s from Michigan. The d i f f e r e n c e in c l a y p e r c e n t a g e among farms w i t h i n r e g i o n s was a l s o s i g n i f i c a n t (p < .0 5 ). N itr o g e n The n i t r o g e n s t a t u s of t h e s o i l depends on s e v e r a l f a c t o r s . 125 Organic m a t t e r c o n t e n t i s one. Organic s o i l s g e n e r a l l y c o n t a i n more n i t r o g e n t h a n m i n e r a l s o i l s . The t y p e o f c r o p p r e v i o u s l y grown on t h e s o i l a l s o h a s an e f f e c t , s i n c e a l f a l f a and o t h e r legumes c o n t r i b u t e n i t r o g e n t o t h e s o i l . Other i m p o r t a n t f a c t o r s i n c l u d e p r e v i o u s n i t r o g e n a p p l i c a t i o n , m anure a p p l i c a t i o n , and e n v i r o n m e n t a l c o n d i t i o n s under which the p r e v i o u s c r o p was r a i s e d (for example d r o u g h t o r p e s t s w i l l d e c r e a s e t h e y i e l d of a legume c r o p and t h e r e f o r e t h e n i t r o g e n s u p p l y f o r t h e n e x t c r o p . The r a t e o f f e r t i l i z a t i o n depends on th e n i t r o g e n r e q u i r e m e n ts o f t h e crop to produce the p o ten tial or d e s i r e d y ield , n i t r o g e n c o n t e n t of t h e s o i l (Vitosh e t a l . , 1979). from E c u a d o r and M i c h i g a n among s o i l m in us the I n th e s o i l s ( T a b l e 4, F i g u r e 3) t h e d i f f e r e n c e n itro g en co ntents i n t h e r e g i o n s was s i g n i f i c a n t (p < . 0 5 ) , and t h e d i f f e r e n c e among f a r m s w i t h i n r e g i o n was n o t (p > .05) . N i t r o g e n f e r t i l i z a t i o n i s n e c e s s a r y f o r c o rn p r o d u c t i o n and for p a s t u r e s i f the sta n d s c o n s i s t of o n ly g r a s s . For mixed p a s t u r e s , or f o r a l f a l f a , n i t r o g e n f e r t i l i z e r i s n o t needed when t h e r e i s a good p r o p o r t i o n o f l e g u m e s i n t h e a s s o c i a t i o n and m anure is reverted to the field s. Indeed, heavy nitrogen a p p l i c a t i o n t o g r a s s - c l o v e r p a s t u r e s r e s u l t s i n a l o s s of c l o v e r from t h e a s s o c i a t i o n due t o c o m p e ti t io n f o r l i g h t , m o is tu r e and n u t r i e n t s , p a r t i c u l a r l y p otas sium (Donald, 1958). The M ich ig an S ta te U n iv e rsity E x ten sio n S erv ice recommendations f o r n i t r o g e n f e r t i l i z a t i o n o f c orn a r e shown i n T a b l e 1.5 (Appendix I ) . Table 4. N i t r a t e s , phosphorus, p otassium , c a l c i u m , and magnesium c o n c e n t r a t i o n s i n s o i l s from f i v e r e g i o n s i n t h e Chimborazo p r o v i n c e o f Ecuado r and one r e g i o n I n Shiawasee county, Michigan (1) NITRATENITROGEN ppm REGION(2) X N (SEM) POTASSIUM ppm PHOSPHORUS ppm X (SEM) X (SEM) CALCIUM ppm X (SEM) MAGNESIUM ppm X (SEM) 1 ECUADOR 15 11.9 (2.11) 25.7 (10.9) 514 (94) 3303 (318) 804a (39) 2 ECUADOR 15 12.8 (2.11) 10.2 (10.9) 229 (94) 3045 (318) 814a (39) 3 ECUADOR 15 10.6 (2.11) 38.5 (10.9) 384 (94) 1938 (318) 586a (39) 4 ECUADOR 15 6.0 (2.11) 15.2 (10.9) 383 (94) 2774 (318) 635a (39) 5 ECUADOR 15 16.8 (2.11) 13.6 (10.9) 531 (94) 3230 (318) 691a (39) 6 MICHIGAN 13 15.9 (2.27) 61.6 (11.7) 175 (101) 1704 (342) 308b (42) * NS NS ** NS ** NS ** ** NS S i g n i f i c a n c e of F (3) Region Farm /region (1) (2) (3) N, X, SEM: number o f o b s e r v a t i o n s , means and s t a n d a r d e r r o r s of means Region means w i t h i n a column w ith o ut a common s u p e r s c r i p t a r e d i f f e r e n t (p < .05) NS: n o n - s i g n i f i c a n t (p < . 0 5 ) ; **: p < .01; *: p < .05 24 22 20 18 16 14 12 10 8 6 4 2 0 REGION ! 3. S o i l n i t r a t e - n i t r o g e n in f i v e r e g i o n s ( 1 - 5 ) in th e Chimborazo o f Ecuador and one r e g io n (6) in Shiaw assee County, M ichigan. 128 Phosphorus D if f e r e n t p l a n t s p e c ie s have d i f f e r e n t requirem ents for phosphorus. A s o i l t e s t o f 1 0 -2 0 ppm i s c o n s i d e r e d l o w , 20-30 ppm medium a n d 30-50 R eco m m end atio n s f o r ppm h i g h for fe rtiliz a tio n corn (M eints, a r e made on t h e 1982). basis of n u t r i e n t r e m o v a l by t h e c r o p , e x p e c t e d c r o p y i e l d , a n d , i n t h e c a s e o f p e r m a n e n t c r o p s s u c h a s a l f a l f a , m a i n t e n a n c e o f a good f e r t i l i t y l e v e l in the s o i l . The M i c h i g a n S tate U n iv ersity E x te n s i o n S e r v i c e recommendations f o r p h o s p h o r u s f e r t i l i z a t i o n f o r corn and a l f a l f a a r e shown i n t a b l e 1.6 and 1.7 (Appendix I ) , respectively. S o i l s from r e g i o n s 2, 4 and 5 from Ecuador (Table 4, F ig u re 4 ) , had a l o w p h o s p h o r u s c o n t e n t f o r c o r n c u l t i v a t i o n , r e g i o n 1 had a medium c o n t e n t , and r e g i o n 5 had a high c o n t e n t . Region 6, in Michigan, had a v e r y h ig h phosphorus c o n t e n t , p r o b a b l y due to recent f e r t i l i z a t i o n . the re g io n s There was no s i g n i f i c a n t d i f f e r e n c e among (p > - . 0 5 ) , b u t t h e d i f f e r e n c e among f a r m s w i t h i n r e g i o n was s i g n i f i c a n t ( p < . 0 1 ) . Potassium For c o r n c u l t i v a t i o n , a s o i l p o t a s s i u m t e s t o f 0 -2 5 ppm i s c o n s i d e r e d v e r y l o w , 25 t o 75 l o w , 75-1 2 5 medium, 1 2 5 -1 7 5 h i g h , and a b o v e 175, v e r y h i g h ( M e i n t s , 1982). R e g io n 6 i n M i c h i g a n had an a v e r a g e o f 175 ppm o f p o t a s s i u m i n t h e s o i l . regions 1 to 5 in Ecuador a ll contained S o i l s from a b o v e 175 ppm o f p o t a s s i u m ( T a b l e 4, F i g u r e 5 ) , p r o b a b l y due t o t h e i r v o l c a n i c o r i g i n . There was no s i g n i f i c a n t d i f f e r e n c e i n po tas siu m c o n t e n t of s o i l s among r e g i o n s (p > . 0 5 ) , b u t t h e d i f f e r e n c e among farms 60 50 40 30 20 10 0 1 2 3 4 5 6 REGION e 4. S o i l phosphorus i n f i v e r e g i o n s ( 1 - 5 ) in th e Chimborazo p r o v in c e o f Ecuador and one r e g io n (6 ) in S h ia w a ssee County, M ichigan. 600 500 W A 400 300 130 SOIL POTASSIUM (p p m ) / // // /.' 200 100 0 REGION F ig u r e 5 . S o i l p o ta s siu m i n f i v e r e g i o n s ( 1 - 5 ) in th e Chimborazo p r o v in c e o f Ecuador and one r e g io n (6) in S h ia w a ssee County, M ichigan. 131 w i t h i n r e g i o n s was s i g n i f i c a n t (p < . 0 1 ) . P h o s p h o r u s and p o t a s s i u m f e r t i l i z a t i o n a r e n e c e s s a r y f o r optim al p a stu re p ro d u ctio n . (W a r n c k e a n d C h r i s t e n s o n , The r e c o m m e n d a t i o n s f o r a l f a l f a 19 8 0 ) c a n be f o l l o w e d for the f e r t i l i z a t i o n of mixed p a s t u r e s t o f a v o r th e growth of legumes. The r e c o m m e n d a t i o n s for annual phosphorus and p o t a s s i u m f e r t i l i z a t i o n f o r a l f a l f a a r e shown i n t a b l e 1.7 (Appendix I ) . Recommendations f o r p h o s p h o r u s and p o t a s s i u m f e r t i l i z a t i o n f o r co rn a r e shown i n t a b l e 1.6 (Appendix I ) . Calcium Calcium , a l t h o u g h e s s e n t i a l f o r p l a n t s and a n i m a l s , seldom i n a d e q u a t e i n t h e s o i l f o r c ro p r e q u i r e m e n ts . is Testing for c a l c i u m c o n t e n t i n s o i l s i s u s e f u l t o a s s e s s magnesium s t a t u s i n t h e s o i l ( R o b e r t s o n e t a l . , 1 9 7 6 a ). When t h e pH o f t h e s o i l i s adequate for p l a n t grow th, the c alciu m c o n te n t of the s o i l is l i k e l y t o be s u f f i c i e n t due to the low r e q u i r e m e n ts of t h e c ro p s (Robertson e t a l . , 1976a). In the p re s e n t in v estig atio n , c alciu m c o n te n t in s o i l s ranged from around 1700 and 1900 ppm i n r e g i o n s 6 i n Michigan and 3 i n E c u a d o r t o 2700 t o 3300 i n t h e o t h e r r e g i o n s o f E c u a d o r (Table 4, F i g u r e 6). was n o t s i g n i f i c a n t The d i f f e r e n c e among t h e means o f r e g i o n s (p > . 0 5 ) , b u t th e d i f f e r e n c e among means of farms w i t h i n r e g i o n s was h i g h l y s i g n i f i c a n t (p . 0 5 ) . Sodium Under most p r a c t i c a l c o n d i t i o n s a n im a l s b e n e f i t from sodium supp lem en tatio n to the d i e t . Some p l a n t s p e c i e s a l s o b e n e f i t from sodium f e r t i l i z a t i o n , depending on t h e adequacy o f potassium i n t h e s o i l , b u t f o r a g e s p e c i e s a r e n o t l i k e l y t o s u f f e r from sodium d e f i c i e n c y . Sodium becomes i m p o r t a n t when n i t r a t e s a r e u s e d a s a n i t r o g e n f e r t i l i z e r , b e c a u s e sodium n i t r a t e h e l p s t o m a i n t a i n t h e s o i l pH, w h i l e c o n tin u o u s use o f t h e ammonium s a l t l o w e r s t h e pH i n t h e s o i l . I n t h i s e x p e r i m e n t , sodium i n s o i l s (Table 5, F i g u r e 9) ranged from 131 ppm i n r e g i o n 5 i n Ecuador to 252 ppm i n r e g i o n 4 i n E c u a d o r . S o i l s from M i c h i g a n , r e g i o n 6, had an a v e r a g e o f 166 ppm so dium . The d i f f e r e n c e i n sodium c o n c e n t r a t i o n among r e g i o n s was s i g n i f i c a n t (p C . 0 5 ) , b u t t h e d i f f e r e n c e among farms w i t h i n r e g i o n s was no t ( p > . 0 5 ) . C o b a lt C o b a l t i s needed by th e legume r o o t n o du le b a c t e r i a system 900 — r~ I 1i 800 H i I j 600 -Ji j 500 - 300 - 400 -4 i I i 200 100 - - M m m i f '% m m , m m m m m ^ ^ s ill a A m w m A m A m 4M Wm W m W A> A A WA wM Zm Am t o Wj/4 A A f/M AAA y/ zy/A & ////A W ///A Wz/ z/ a W /Z/ft vtzzzza xaaaa w m w m W a a & >m m m w m WM ww / amS .Vwz/zzmA wV/zAmzz\ WvzzmZA w W A W //-A AaA //A wW a vw m w m \zZ///A. 0 '/m Y 'W a w m v/A /Z aW/AW\ W /W ' -- w m w m w m m m m W/AZ? V/'-A/A tzW-A V /Am//A w W ym m m m w m REGION F ig u r e 7. S o i l magnesium i n f i v e r e g i o n s ( 1 - 5 ) in t h e Chimborazo p r o v in c e o f Ecuador and one r e g io n (6) in S h iaw assee County, M ichigan. 134 MAGNESIUM i SOIL (p p m ) 700 -j 135 PERCENT OF CA + K +M G 5 -r „ !V\1 F ig u r e 8 . REGION POTASSIUM 1*771 MAGNESIUM S o i l p o ta s siu m and magnesium a s a p e r c e n t o f t o t a l b a s e s in f i v e r e g i o n s ( 1 - 5 ) in t h e Chimborazo p r o v in c e o f Ecuador and one r e g io n (6) i n S h iaw assee County, M ichigan. 260 240 - 220 - SOIL SODIUM (p p m ) 200 IS O H 160 140 120 - 100 - 80 60 40 20 - 1 2 3 4 5 6 REGION F ig u r e 9 . S o i l sodium i n f i v e r e g i o n s ( 1 - 5 ) in th e Chimborazo p r o v i n c e o f Ecuador and one r e g io n (6) in S h iaw assee County, M ichigan. 137 f o r t h e f i x a t i o n o f a tm o sp h e ric n i t r o g e n . S o i l s are suspected to be c o b a l t d e f i c i e n t when t h e y h a v e l e s s t h a n 5 ppm o f t o t a l c o b a l t c o n t e n t or when legumes grown on them have l e s s t h a n 0.07 ppm c o b a l t (Kubota and A l l a w a y , requirem ent of d a iry C o b alt content in c attle the 1972 ). is sam ple about so ils The minimum c o b a l t 0.10 ppm (NRC, (Table 5, 1978). Figure 10), e x t r a c t e d w i t h 0.1 N HC1, r a n g e d from 0.67 ppm i n r e g i o n 6 i n M i c h i g a n t o 2.53 ppm i n r e g i o n 1 i n E c u a d o r . The d i f f e r e n c e among r e g i o n s (p < .05) and among f a r m s w i t h i n r e g i o n (p < .01) was s i g n i f i c a n t . Iron The amount o f ex tra ctab le iron in s o i l d e p e n d s on t h e t e x t u r e , p r o f i l e and d r a i n a g e c h a r a c t e r i s t i c s o f t h e s o i l . In M i c h i g a n (Mokma e t a l . , 1 9 79 ), t h e p l o w l a y e r o f w e l l - d r a i n e d loam and sandy loam s o i l s had 54 ppm i r o n , and t h e plow l a y e r of w e l l - d r a i n e d loamy sand and sand s o i l s had 48 ppm i r o n . d r a i n e d s o i l s of t h e Poorly same t e x t u r e s had h i g h e r e x t r a c t a b l e 119, 145 and 150 ppm r e s p e c t i v e l y . S o i l i r o n i s l e s s f o r p l a n t s a t high s o i l pH v a l u e s (Robertson e t a l . , iron: av ailab le 1981a). In th e p r e s e n t s t u d y (Table 5, F i g u r e 11), s o i l s from r e g i o n 6, in M ichigan, had an a v e r a g e i r o n c o n t e n t o f 89 ppm. h i g h e s t v a l u e fo u n d the sam p les were ch aracteristics was i n r e g i o n taken from and significant. plow lay er. A ll D rainage r a n g e d from w e l l d r a i n e d t o somewhat p o o r l y d r a i n e d in th e f i e l d s sam pled. (p < . 0 5 ) the 2 o f E c u a d o r : 269 ppm. The among farm s The d i f f e r e n c e among r e g i o n s w ith in regions (p < .0 1 ) was Table 5. Sodium, c o b a l t , i r o n , manganese, and molybdenum c o n c e n t r a t i o n s i n s o i l s from f i v e r e g i o n s i n t h e Chimborazo p r o v i n c e of Ecuador and one r e g i o n i n Shiawasee county , Michigan (1) SODIUM ppm X N 1 ECUADOR 15 133 (16) 2 . 53a 2 ECUADOR 15 193 (16) 2.00ab (0.32) 269a 3 ECUADOR 15 134 (16) 4 ECUADOR 15 5 ECUADOR 15 13 (SEM) IRON ppm REGION (2) 6 MICHIGAN X COBALT ppm (SEM) X (0.32) MOLYBDENUM ppm MANGANESE ppm (SEM) X X (SEM) 114 (13) 0.05 b (0.04) (29) 65 (13) 0 . 26a (0.04) 1.29ab (0.32) 225ab (29) 66 (13) 0.2 8a (0.04) 252 (16) 2 . 18ab (0.32) 139ab (29) 78 (13) 0 .1 6b (0.04) 131 (16) 1 . 48ab (0.32) 109b 54 (13) 0 . 23a (0.04) 60 (14) 0.52a (0.05) 166 (17) 0.67 b (01.34) 182ab (29) (SEM) 89b (29) (31) S i g n i f i c a n c e o f F (3) Region Farm /region (1) (2) (3) * NS * ** * ** NS ** ** ** N, X, SEM: number o f o b s e r v a t i o n s , means and s t a n d a r d e r r o r s of means Region means w i t h i n a column w ith o u t a common s u p e r s c r i p t a r e d i f f e r e n t (p < .05) NS: n o n - s i g n i f i c a n t ( p < . 0 5 ) ; **: p < . 0 1 ; *: p < . 0 5 2.4 - 2.2 - 2 - 1.8 - 1. 6 - 1.4 - 1 .2 - 10.8 - 0.6 - 139 SOIL COBALT (p p m ) 2 .6 -r~ 0.4 - 0.2 - 1 2 3 4 5 6 REGION F ig u r e 10. S o i l c o b a l t in f i v e r e g i o n s ( 1 - 5 ) in th e Chimborazo p r o v in c e o f Ecuador and one r e g io n (6) in S h iaw assee County, M ichigan. 280 — t 260 240 - 200 - 180 - 140 - 160 - 120 - 100 - 140 SOIL (p p m ) - IRON 220 80 60 40 20 - 1 2 3 4 5 6 REGION F ig u r e 11 . S o i l ir o n i n f i v e r e g io n s ( 1 - 5 ) in t h e Chimborazo p r o v in c e o f Ecuador and one r e g io n (6) in S h iaw assee County, M ichigan. 141 Manganese S o i l man ganese a v a i l a b i l i t y i n s o i l s d e c r e a s e s when t h e s o i l s a r e n o t w e l l d r a i n e d or when th ey h a v e a h i g h pH (Robertson and L u c a s , 1 9 8 1a ). M anganese c o n t e n t i n s o i l s t e s t e d i n t h i s i n v e s t i g a t i o n (Table 5, F i g u r e 12) ranged from 54 ppm i n r e g i o n 5 t o 114 ppm i n r e g i o n 1 i n E c u a d o r . M ichigan, S o i l s from r e g i o n 6, had an a v e r a g e o f 60 ppm m a n g a n e s e . s i g n i f i c a n t d i f f e r e n c e among r e g i o n s (p > . 0 5 ) , regions d i f f e r e d in T h e r e was no b u t farms w i t h i n (p < .01). Manganese f e r t i l i z a t i o n i s recommended f o r r e s p o n s i v e c ro ps when t h e s o i l t e s t (0.1 N HC1 e x t r a c t a b l e manganese) g i v e s v a l u e s b e l o w 20 ppm; t h e pH o f t h e s o i l a l s o m u s t be c o n s i d e r e d when fertiliz atio n i s recommended. I t i s p ro b a b le t h a t the s o i l s t e s t e d in t h i s stud y do n o t need manganese f e r t i l i z a t i o n . A l f a l f a , g r a s s e s and c o r n a r e medium r e s p o n s i v e c r o p s t o m an g an ese fertiliz atio n fe rtiliz a tio n (V itosh et a l., 19 81). r e c o m m e n d a t i o n s made by t h e U n i v e r s i t y E x te n sion S e r v i c e (Vitosh e t a l . , M anganese M ichigan S t a t e 1981) a r e shown i n t a b l e 1.8 (Appendix I ) . Molybdenum Molybdenum i s e s s e n t i a l functions, R hizobia to p l a n t s . Among i t s i t h a s a p a r t i n t h e enzyme n i t r a t e for f i x a t i o n of n itro g e n . other re d u c ta se of A lthough e s s e n t i a l for a n i m a l s , molybdenum i s of i n t e r e s t i n n u t r i t i o n a l s t u d i e s m a in ly b e c a u s e o f i t s i n t e r a c t i o n w i t h s u l f u r and c o p p e r . Molybdenum a v a i l a b i l i t y i n c r e a s e s a t h i g h e r s o i l pH v a l u e s ( R o b e r t s o n e t a l., 198 1b). The c r i t i c a l lev el (T able 1.2, A p p e n d ix I) o f 120 110 - 100 - SOIL 80 70 60 50 142 MANGANESE (p p m ) 90 - 40 30 - 20 - 10 - 1 2 3 4 5 6 REGION F ig u r e 12 . S o i l manganese i n f i v e r e g i o n s ( 1 - 5 ) in t h e Chimborazo p r o v in c e o f Ecuador and one r e g io n (6) in S h iaw assee County, M ichigan. 143 molybdenum i n t h e s o i l ( e x t r a c t e d w i t h ammonium o x a l a t e a t pH 3.3) i s 0 .0 4 - 0 . 2 0 ppm (Cox and K a m p ra th , 1972). Molybdenum in sampled s o i l s (Table 5, Figure 13) ranged from 0.05 ppm in r e g io n 1 i n Ecuador t o 0.52 ppm in r e g io n 6 in Michigan. S o i l s from region 4 in Ecuador had a molybdenum conten t of 0.16 ppm. S o i l s from the other r eg io n s stu d ied in t h i s study had a molybdenum c o n t e n t ab ove 0.20 ppm, which i s th e c r i t i c a l le v e l. A lfa lfa is a c r o p h i g h l y r e s p o n s i v e t o molybdenum f e r t i l i z a t i o n and b e n e f i t s from tr e a tin g seed with molybdenum in s o i l s d e f i c i e n t in t h i s elem ent. I t i s p o s s i b l e th a t a l f a l f a and legumes in gen eral grown on s o i l s with a molybdenum con ten t below or w i t h i n the c r i t i c a l l e v e l , such as t h o s e from r e g io n 1 and 4 in Ecuador, w i l l respond to molybdenum f e r t i l i z a t i o n . I t is a lso p o s s i b l e th a t molybdenum in the s o i l w i l l become more a v a i l a b l e to the p la n t a fte r lim ing in the f i e l d s th a t need pH ammendment. For molybdenum in s o i l s , there was a s i g n i f i c a n t d if f e r e n c e among r e g i o n s (p < . Q 1 ) , a s w e l l as among farms w i t h i n r e g i o n s (p < .0 1 ). The c o r r e l a t i o n c o e f f i c i e n t betw een s o i l pH and molybdenum in s o i l s was -0.443. Selenium The s e le n iu m c o n t e n t o f most s o i l s l i e s betw een 0.1 and 2 ppm. The maximum c o n c e n t r a t i o n o f s e l e n iu m found in s e v e r a l thousand s o i l samples in the United S t a t e s was under 100 ppm, and th e m a j o r it y o f th e s e l e n i f e r o u s s o i l s a n a ly z e d c o n t a in e d an a v e r a g e o f l e s s than 2 ppm s e le n iu m (NRC, 1983). S e le n iu m i s more a v a i l a b l e to p la n t s when the pH o f the s o i l i s high (T isd ale e t a l . , 1985). Based on feed a n a l y s i s , the s o i l s o f the S ta te of 0.6 SOIL 0.4- -I 0.3 - 144 MOLYBDENUM (p p m ) 0.5 - 0.2 -I 0.1 - 1 2 3 4 5 6 REGION F ig u r e 1 3 . S o i l molybdenum i n f i v e r e g i o n s ( 1 - 5 ) in th e Chimborazo p r o v in c e o f Ecuador and one r e g io n (6 ) in S h iaw assee County, M ichigan. 1.45 Michigan a r e c l a s s i f i e d as s e l e n i u m d e f i c i e n t . Approxim ately 80% o f a l l f o r a g e and g r a i n from M i c h i g a n c o n t a i n e d l e s s t h a n 0.05 ppm s e l e n i u m (Kubota and A lla w a y , 1972). S o i l s a m p l e s ( T a b l e 6, F i g u r e 14) from r e g i o n 4 i n E c u a d o r had an a v e r a g e s e l e n i u m c o n t e n t of 0.09 ppm. Samples from r e g i o n 3 i n Ecuador had an a v e r a g e se len iu m c o n t e n t o f 3.41 ppm. Soils from r e g i o n 6 i n Michigan c o n t a i n e d 0.41 ppm o f se le n iu m . There was no s i g n i f i c a n t d i f f e r e n c e among r e g i o n s (p > . 0 5 ) , b u t farms w i t h i n r e g i o n s d i f f e r e d i n se l e n i u m c o n t e n t ( p < . 0 1 ) . Zinc The c r i t i c a l l e v e l f o r zinc in s o i l s ran g e s from 1.0 t o 7.5 ppm (Table 1.2, Appendix I ) . for p lan ts leached, in s o i l s acid, prevalent w ith c a lc a r e o u s su rfa c e h o rizo n s or sandy where t h e Zinc i s more l i k e l y t o be d e f i c i e n t so ils. so il is Z in c high deficiency in av ailab le may a l s o in be phosphorus. I n t e r a c t i o n s i n v o l v i n g z i n c , phosphorus and i r o n r e s u l t in poor u t i l i z a t i o n o f z in c by p l a n t s (Kubota and A l l a w a y , 1972). Zinc d e f i c i e n c i e s have been i d e n t i f i e d in M ichigan in navy b e a n s, e s p e c i a l l y the S a n ila c v a r i e ty . to zinc response fe rtiliz a tio n , Corn i s a c ro p h i g h l y r e s p o n s i v e w hile g rasses (Robertson and Lucas, 1981b). and a l f a l f a show low Recommendations f o r zin c f e r t i l i z a t i o n a r e shown i n t a b l e 1.9 (Appendix I ) . Z in c i n s o i l s s a m p l e d r a n g e d from 3.7 ppm i n r e g i o n 6 i n M i c h i g a n t o 12 ppm i n r e g i o n 2 i n E c u a d o r ( T a b l e 6, F i g u r e 15). The a v e r a g e z i n c c o n t e n t i n s o i l s from r e g i o n 1 i n E c u a d o r was 6.5 ppm, and i n r e g i o n 4 i n E c u a d o r 5.1 ppm. The a v e r a g e pH o f s o i l s from r e g i o n 4 i n Ecuador was 7.2, t h u s i t i s p o s s i b l e t h a t Table 6. Selenium, z in c , s u l f a t e s , and copper c o n c e n t r a t i o n s i n s o i l s from f i v e r e g i o n s i n t h e Chimborazo p r o v i n c e o f E c u a d o r and one r e g i o n i n S h i a w a s e e c o u n t y , Michigan (1) SELENIUM ppm X REGION(2) (SEM) ZINC ppm X (SEM) SULFATESULFUR ppm COPPER ppm X (SEM) X (SEM) 1 ECUADOR 15 0.64 (0. 74) 6.5 (1.92) 8C (5. 06) 312a (1.60) 2 ECUADOR 15 0.32 (0. 74) 12.0 (1.92) 46a (5. 06) 138° (1.60) 3 ECUADOR 15 3.41 (0. 74) 9.0 (1.92) 63a (5. 06) 130° (1.60) 4 ECUADOR 15 0.09 (0. 74) 5.1 (1.92) 18c (5. 06) 231ab (1.60) 5 ECUADOR 15 0.18 (0. 74) 9.5 (1.92) 170bc (1.60) 6 MICHIGAN 29b (5. 06) 7c (5. 44) 27d (1.72) ** ** ** * 13 0.41 (0 . 79) 3.7 (2.07) S i g n i f i c a n c e of F (3) Region Fa rm /region (1) (2) (3) NS ** NS ** N, X, SEM: number o f o b s e r v a t i o n s , means and s t a n d a r d e r r o r s of means Region means w i t h i n a column w i th o u t a common s u p e r s c r i p t a r e d i f f e r e n t (p < . 0 5 ) NS: n o n - s i g n i f i c a n t ; **: p < .01; *: p < .05 (p p m ) 3.5 2.5 - - 1.5 147 SOIL SELENIUM 2 0.5 - 77WA 1 2 4 3 5 6 REGION F ig u r e 14 . S o i l s e le n iu m i n f i v e r e g i o n s (1~5) i n th e Chimborazo p r o v in c e o f Ecuador and one r e g io n (6) in S h ia w a sse e County, M ichigan. (p p m ) ZINC SOIL 148 1 2 3 4 5 6 REGION F ig u r e 1 5 . S o i l z in c in f i v e r e g i o n s ( 1 - 5 ) in th e Chimborazo p r o v in c e o f Ecuador and one r e g io n (6) in S h iaw assee County, M ichigan. 150 z in c f e r t i l i z a t i o n w i l l i n c r e a s e t h e y i e l d of r e s p o n s i v e c ro p s such as c orn i n t h i s r e g i o n . There was no s i g n i f i c a n t d i f f e r e n c e among r e g i o n s (p > . 0 5 ) , b u t t h e d i f f e r e n c e among f a r m s w i t h i n r e g i o n were s i g n i f i c a n t (p C . 0 1 ) . Soil Sulfates The t h r e s h o l d l e v e l s b e lo w w h ic h s u l f u r f e r t i l i z a t i o n i s f r e q u e n t l y recommended in t h e G r e a t Lakes a r e a i s between 6 t o 7 ppm (12 t o 14 l b / a c r e ) o f s u l f a t e - s u l f u r in the s o i l . Several f i e l d s i n Michigan had been found t o have s u l f u r c o n c e n t r a t i o n s below t h e l e v e l s mentioned, but s u l f u r f e r t i l i z a t i o n f a i l e d to cause an i n c r e a s e i n c ro p y i e l d s . Legumes a r e more r e s p o n s i v e t o s u l f u r f e r t i l i z a t i o n than o t h e r c ro p s (Robertson e t a l . , 1976b). S u l f u r c o n t e n t o f t h e s o i l was 7 ppm i n r e g i o n 6 i n Michigan and 8 ppm i n r e g i o n 1 i n E c u a d o r . The o t h e r r e g i o n s i n E c u a d o r had a v e r a g e s u l f u r v a l u e s above 18 ppm (Table 6, F i g u r e 16). It i s p o s s i b l e t h a t some s u l f u r f e r t i l i z a t i o n i s needed in re g i o n 1 and 6. The p r o c e d u r e recommended by t h e E x t e n s i o n S e r v i c e o f M ichigan S tate fe rtiliz e U n iv ersity (Robertson et a l., 1976b) is to t e s t s t r i p s a c r o s s t h e f i e l d a t a r a t e o f 22 t o 44 k g / h e c t a r e (20 t o 40 l b / a c r e ) . I f t h e r e i s an i n c r e a s e i n y i e l d o f t h e c r o p i n t h e s t r i p s t e s t e d , t h e n a l l t h e c r o p s h o u l d be f e r t i l i z e d w ith s u l f u r . The d i f f e r e n c e s o f s o i l s u l f a t e c o n t e n t among r e g i o n s and farms w i t h i n r e g i o n s were s i g n i f i c a n t (p < .01). The c o r r e l a t i o n c o e f f i c i e n t of s o i l pH and s o i l s u l f u r was -0.295. CQE g e r The c ritic a l lev el (Table 1.2 A p p e n d ix I) for copper ^07569 REGION F ig u r e 16 . S o i l s u l f a t e - s u l f u r in f i v e r e g i o n s ( 1 - 5 ) in th e Chimborazo p r o v in c e o f Ecuador and one r e g io n (6) in Shiaw assee County, M ichigan. 1.52 c o n c e n t r a t i o n i n o r g a n i c s o i l s measured a f t e r e x t r a c t i o n w i t h 1.0 N HC1 ra nges from 9-20 ppm (Whitney, 1980). S o i l s in region 6 in M i c h i g a n ( T a b l e 6, F i g u r e 17) had t h e l o w e s t c o p p e r c o n t e n t o f t h e s i x r e g i o n s sampled f o r t h i s i n v e s t i g a t i o n (2.7 ppm). 1 i n E c u a d o r had t h e h i g h e s t c o p p e r c o n c e n t r a t i o n Region (31.2 ppm). Co p per c o n t e n t i n r e g i o n 6 i n M i c h i g a n i s b e l o w c r i t i c a l l e v e l range. S o i l s from r e g i o n s 2 and 3 i n E c u a d o r had 13.8 and 13.0 ppm c o p p e r , and t h e r e f o r e were a l s o low i n copper. a re w ith in th e range of c r i t i c a l fertiliz atio n is (p among .01) and p o ssib le. farm s These v a l u e s l e v e l , w h e re a r e s p o n s e t o The d i f f e r e n c e w ith in regions among r e g i o n s (p .01) was significant. Crops, e s p e c i a l l y legumes, grown i n s o i l s from r e g i o n s 2, 3 and 6 may b e n e f i t from copper f e r t i l i z a t i o n . 32 30 28 26 24 22 20 18 16 14 153 12 10 8 6 4 2 0 REGION 17 S o i l copper i n f i v e r e g i o n s ( 1 - 5 ) in th e Chimborazo p r o v in c e o f Ecuador and one r e g io n (6 ) in S h iaw assee County, M ichigan. 154 N u trien ts in Pastures P astures Management in Ecuador P a s t u r e s s t u d i e d in Ecuador are g e n e r a l l y a s s o c i a t i o n s o f g r a s s e s and legumes. Preferred s p e c ie s for pasture are ryegrass (Lolium m u ltiflo ru m ) and white c lo v e r (T r ifo liu m repens) . le ss fre q u en tly c u lt iv a t e d s p e c i e s (D a c t y l i s g l o m e r a t a ) , f e s c u e s in c lu d e orchard (F e s tu c a s p . ) , tim o th y p r a ten se ) and red c lo v e r (T\ p r a ten se ). Other grass (Phleum Some farms grow a l f a l f a (M edicago s a t i v a ) , and in some c a s e s o a t s (Avena s a t i v a ) , rye (S e c a le c e r e a l e ) , or wheat (Triticum sp.) for greenchop. Some o f the weeds commonly found among th e c u l t i v a t e d sp e c ie s are d a n d e l i o n (Taraxacum o f i c i n a l e ) , c h ic o r y (C hicorium i n t i b u s ) , th istle s (C irsiu m s p . ) , dock s (Rumex s p . ) , p l a n t a i n s (P la n t a g o s p . ) , grama (Paspalum s p . ) , sw ee t v e r n a l g r a s s (Anthoxantum odoratum) and v e l v e t g r a ss (Holcus la n a tu s). D airy c a t t l e a r e k e p t p e rm a n en tly on p a s t u r e . The r o t a t i o n o f t h e h e r d from p a s t u r e t o p a s t u r e i s p r a c t i c e d on a l l f a r m s . The s i z e o f t h e l o t s wh e re t h e a n i m a l s a r e k e p t from 1 t o 5 d a y s d e p e n d s on t h e s i z e o f t h e h e r d , i s from 1 t o 5 h e c t a r e s (2.5 t o 12 a c r e s ) . Grazing l o t s a r e fenced with barbed w ire. Depending on t h e a l t i t u d e of the farm, r o t a t i o n s a re completed i n 45 t o 90 days. Average te m p e ra tu re s a t h ig h e r a l t i t u d e s a re lo w e r, th e p a s t u r e grows more s l o w l y , and r o t a t i o n s t h e r e f o r e t a k e l o n g e r . At 3000 m (9800 f t ) t h e a v e r a g e t e m p e r a t u r e i s a b o u t 12 ° C, and t h e r o t a t i o n s a r e c o m p l e t e d i n a b o u t 60 d a y s . For e a c h 200 m (650 f t ) i n c r e a s e in a l t i t u d e , a 1° C d e c r e a s e i n t e m p e r a t u re i s e x p e c t e d (Ter&n, 1979). 155 A lm ost a l l d a i r y c a t t l e in th e r e g i o n s s t u d i e d are e i t h e r H o l s t e i n F r i e s i a n s or c r o s s e s o f H o l s t e i n s w ith n a t i v e b r e e d s . In d e e d , a lm o s t a l l th e d a i r y c a t t l e are b l a c k and w h it e . Few farms have Brown S w iss, J e r se y , or other breeds. Dairy anim als are maintained alm ost e x c l u s i v e l y on pasture. V ery few farms g i v e th e a n im a ls g r a i n a t th e tim e o f m i l k i n g . S a l t i s provided to a l l anim als, but tra c e m ineral s a l t i s seldom u sed . Some farm ers o c a s s i o n a l l y g i v e bone ash t o a n im a ls as a so u r c e o f ph osp horus; d i c a l c i u m p h o sp h a te or o th e r phosphorus sources are seldom used. in th e farm s t o r e s , S e v e r a l mineral mixtures can be found but farm ers do n o t use them on a r e g u la r b a sis. S in c e s e v e r a l o f th e a r e a s s t u d i e d are d e f i c i e n t in io d in e , t h i s m ineral i s provided to the anim als in io d ized s a l t or mixed with m o la sse s. D a ir y fa rm ers a re c o n s c io u s o f th e need fo r m in e r a l s u p p le m e n t a t io n fo r th e c a t t l e , but e i t h e r th e proper m in e r a l m ixtures or in g r e d ie n ts are not a v a i l a b l e , or the market p r ic e i s to o h ig h . S p e c ific r eq u ire m en ts f o r , m icrom inerals are not w e l l understood. or p r o b l e m s w i t h , The common dairy farmer la c k s a good guide on mineral n u t r it io n for dairy c a t t l e . Ash The amount o f m ineral elem en ts as a group in feed or animal tissu e is d e ter m in e d by burning o f f th e o r g a n ic m a tter and weighing the r e sid u e , which i s c a l l e d ash. The fig u r e a r riv ed at by a sh d e t e r m i n a t i o n of a sp e c ific feed is used in th e c o n v e n t i o n a l fe e d a n a l y s i s as one v a r i a b l e in computing the n itr o g e n f r e e e x t r a c t v a lu e for th a t fe e d . The ash from a fe e d 156 may a l s o be u se d as a startin g point for determ ining the c o n c e n t r a t i o n s o f t h e s p e c i f i c e l e m e n t s p r e s e n t (Maynard and L oosli, 1969). Mean a s h c o n t e n t i n p a s t u r e s ( T a b l e 7, F i g u r e 18) r a n g e d from a r o u n d 11 t o 14% i n t h e f i v e r e g i o n s s t u d i e d i n E c u a d o r . Mean a s h c o n t e n t i n p a s t u r e s from M i c h i g a n was 5.6%. Mean a s h c o n c e n t r a t i o n d i f f e r e d among r e g i o n s (p < . 0 5 ) , t y p e o f s a m p l e (p < .0 1 ), and farms w i t h i n re g i o n ( p < . 0 1 ) . The i n t e r a c t i o n of typ e o f sample and r e g i o n was no t s i g n i f i c a n t (p > . 0 5 ) . Mean ash c o n t e n t o f a l l sam ples was 11.5% when th e p a s t u r e s were washed w i t h d i s t i l l e d w a t e r , and 12.6% when t h e y were n o t washed. T h is d i f f e r e n c e in ash c o n t e n t i s an i n d i c a t i o n o f s o i l c o n ta m i n a ti o n . Grazing a n i m a l s i n g e s t s o i l a l o n g w i t h h e r b a g e and t h i s ingested s o i l c a n be a s o u r c e o f e l e m e n t s f o r the an im als. S o i l t y p e , s t o c k i n g r a t e , e a r t h w o r m p o p u l a t i o n , and management a l l a f f e c t t h e amount of s o i l i n g e s t e d (Healy, 1974). S o i l i n g e s t e d can be a s u b s t a n t i a l p a r t o f t h e dry m a t t e r i n t a k e . Measurements in Southwest England i n d i c a t e s o i l i n t a k e s from 3 t o 6% o f the to tal dry m a tte r in tak e t i t a n i u m as an i n d i c a t o r , F r i e s e t a l . (Thornton, 1 9 74 ). U s in g (1982) found t h a t t h e s o i l i n g e s t i o n o f d r y cows and y e a r l i n g h e i f e r s from M a r y l a n d and M ichigan was a r o u n d 2.4% o f t h e d r y m a t t e r a n i m a l s were k e p t on p a s t u r e . i n t a k e , when t h e A d d itio n o f s o i l to th e d i e t of n on pre gnant, n o n l a c t a t i n g cows a p p a r e n t l y d i d n o t have any e f f e c t on t h e a b s o r p t i o n o f o t h e r n u t r i e n t s fr om t h e d i e t 1977). (M iller, 1.57 T able 7. P a s t u r e a s h , crude p r o t e i n , and crude f i b e r from f i v e r e g i o n s i n t h e Chimborazo p r o v i n c e o f Ecuador and one r e g i o n i n Shiawasee c o u n ty , Michigan (1) ASH % DM CRUDE PROTEIN % DM CRUDE FIBER % DM X REGION (2) N X (SEM) X 1 ECUADOR 30 1 3 . 7a (1.02) 14.0 (1.33) 35.4 (1.38) 2 ECUADOR 30 1 2 . 7 ab (1.02) 15.4 (1.33) 29.2 (1.38) 3 ECUADOR 30 1 1 . 5ab (1.02) 10.4 (1.33) 35.1 (1.38) 4 ECUADOR 30 14.5 a (1.02) 13.6 (1.33) 32.9 (1.38) 5 ECUADOR 30 1 1 . 2ab (1.02) 14.7 (1.33) 35.0 (1.38) 6 MICHIGAN 12 5 . 6 bc (1.33) 14.0 (2.11) 30.0 (2.18) (SEM) (SEM) WASHED 81 11.5 (0.26) 13.2 (0.48) 34.0 (0.35) NON-WASHED 81 12.8 (0.26) 14.1 (0.48) 32.6 (0.35) NS ** NS NS * ** ** NS S i g n i f i c a n c e o f F (3) Region F a rm /re g io n Type o f sample Type X r e g i o n (1) (2) (3) * ** ** NS N, X, SEM: number o f o b s e r v a t i o n s , means and s t a n d a r d e r r o r s o f means Region means w i t h i n a column w i th o u t a common s u p e r s c r i p t a r e d i f f e r e n t (p < . 0 5 ) NS: n o n - s i g n i f i c a n t (p < . 0 5 ) ; **: p < . 0 1 ; *: p < . 0 5 (% DM) ash pasture 158 1 [S 3 F ig u r e 18. 2 WASHED 3 4 5 6 region NON-WASHED Ash i n washed and non-washed p a s t u r e sam ples in f i v e r e g i o n s ( 1 - 5 ) in th e Chimborazo. p r o v in c e o f Ecuador and one r e g io n (6 ) in S h iaw assee County, M ichigan. 159 Crude F i b e r Crude f i b e r i n the d i e t of ruminants i s n e c e s s a r y f o r p r o p e r digestion. A minimum crude f i b e r c o n t e n t of 17.3% o f t h e d i e t i s suggested by t h e NRC (1978) percentage. to m aintain a normal m ilk fat I n t h i s i n v e s t i g a t i o n p a s t u r e s had a c r u d e f i b e r c o n t e n t r a n g i n g from 29.2% i n r e g i o n 2 i n E c u a d o r t o 35.4% i n r e g i o n 1 i n E c u a d o r ( T a b l e 7, F i g u r e 19). Region 6 in M ichigan had an a v e r a g e o f 30.0% crude f i b e r i n t h e p a s t u r e s . s i g n i f i c a n t d i f f e r e n c e among r e g i o n s (p < . 0 5 ) , r e g i o n s (p < . 0 1 ) , and t y p e o f s a m p l e (p < . 0 1 ) . had an a v e r a g e o f 34.0% f i b e r There was a farms w i t h i n Washed s a m p l e s and n o n - w a s h e d s a m p l e s 32.6%, p r o b a b l y because some s o i l co n ta m in a tio n . Nitrogen N i t r o g e n in p a s t u r e s , e xp re ss ed as p e r c e n t p r o t e i n , ranged from an a v e r a g e o f 10.4 i n r e g i o n 3 i n E c u a d o r t o 15.4 i n r e g i o n 2 i n E c u a d o r ( T a b l e 7, F i g u r e 20). The a v e r a g e i n r e g i o n 6 i n Michigan f o r c o rn s i l a g e and a l f a l f a samples was 14.0% p r o t e i n . The d i f f e r e n c e s in te rac tio n among r e g i o n s , ty p es of were n o t s i g n i f i c a n t sam ple, (p > . 0 5 ) . T h e r e was a s i g n i f i c a n t d i f f e r e n c e among farms w i t h i n r e g i o n s (p amount o f n i t r o g e n i n s o i l s and t h e .01). The was p o o r l y c o r r e l a t e d w i t h t h e amount o f n i t r o g e n i n p a s t u r e s (r = - 0 .0 4 3 ) . The c o r r e l a t i o n c o e f f i c i e n t b e tw e e n c r u d e f i b e r and p r o t e i n i n p a s t u r e s was 0.261. L a c t a t i n g cows, depending on t h e i r l e v e l o f m i l k p r o d u c t i o n , r e q u i r e from 13 t o 16% p r o t e i n in t h e d i e t . Growing h e i f e r s and b u l l s r e q u i r e 12% p r o t e i n i n t h e r a t i o n , and d r y p r e g n a n t cows crude fiber (3» DM) 50 pasture 160 rvXl WASHED F ig u r e 19. NON-WASHED Crude f i b e r in washed and non-washed p a s t u r e sam ples in f i v e r e g i o n s ( 1 - 5 ) in th e Chimborazo p r o v in c e o f Ecuador and one r e g io n (6 ) i n S h iaw assee County, M ichigan. (% DM) protein pasture 161 G 53 F igu re 20. WASHED NON-WASHED Crude p r o t e i n in washed and non-washed p a s t u r e sam ples in f i v e r e g i o n s ( 1 - 5 ) i n th e Chimborazo p r o v in c e o f Ecuador and one r e g io n (6) i n S h iaw assee County, M ichigan. 162 11% (NRC, 1978). P a s t u r e s from r e g i o n 3 i n E c u a d o r may n o t h a v e enough p r o t e i n t o s u s t a i n adequate growth or m i l k p r o d u c t i o n of d a i r y a n im a l s . High producing cows i n a l l t h e a r e a s s t u d i e d may need p r o t e i n s u p p l e m e n ta t io n . Calcium Calcium c o n t e n t of th e p a s t u r e sa m p le s ranged from 0.40% i n region 2 t o 0.76% i n r e g i o n 1 i n E c u a d o r . Average c alciu m c o n t e n t i n r e g i o n 6 i n M i c h i g a n was 0.66% o f t h e d r y m a t t e r ( T a b l e 8, F i g u r e 21). T h e r e was n o t a s i g n i f i c a n t d i f f e r e n c e (p > . 0 5 ) among r e g i o n s , t y p e o f s a m p l e , o r i n t h e i n t e r a c t i o n between t h e two, b u t t h e d i f f e r e n c e was significant (p O O l). among farms w ithin region The c o r r e l a t i o n c o e f f i c i e n t between c a l c i u m i n p a s t u r e s and c a lc iu m i n s o i l s was 0.026. C a l c i u m r e q u i r e m e n t s a r e c a l c u l a t e d by m u l t i p l y i n g t h e p h o s p h o r u s r e q u i r e m e n t by a f a c t o r t h a t c a n r a n g e fr om 1 t o 7. The b e s t a b s o r p t i o n o f both e le m e n ts has been a c h i e v e d when t h e r e l a t i o n o f c a l c i u m t o p h o s p h o r u s i s a r o u n d 2:1 (NRC, C alcium -to-phosphorus r e l a t i o n order, 1978 ). i n r e g i o n 1 t o 6 was i n t h i s 2 .5 , 1.7 , 2 .0 , 1.8, 2.8 and 2.8. L a c t a t i n g cows h a v e a high phosphorus r e q u i r e m e n t, so phosphorus sup p le m e n ts a r e o f t e n added t h e d i e t . When such s u p p l e m e n ta t io n o c c u r s , i t i s p o s s i b l e t h a t c a l c i u m a l s o n e e d s t o be ad d ed t o t h e d i e t t o m a i n t a i n a pr o p e r c a l c i u m - t o - p h o s p h o r u s r e l a t i o n s h i p . Phosphorus Mean p h o s p h o r u s c o n t e n t i n p a s t u r e s r a n g e d from 0.21% i n r e g i o n s 3 and 5 t o 0.30% i n r e g i o n 1 o f Ecuador. Mean phosphorus c o n t e n t o f p a s t u r e s i n r e g i o n 6 i n M i c h i g a n was 0.24% ( T a b l e 8, Table 8. Calcium, phosphorus, sodium, po tassium, and magnesium c o n c e n t r a t i o n s i n the dry m a t t e r o f washed and n on-w ashed p a s t u r e s a m p l e s from f i v e r e g i o n s i n t h e Chimborazo p r o v i n c e o f E cu a d or and one r e g i o n i n S h i a w a s e e c o u n t y , M i c h i g a n ( 1) CALCIUM % DM (SEM) PHOSPHORUS % EM SODIUM % DM POTASSIUM % DM MAGNESIUM % DM X X X (SEM) 0.30 (0.03) 0.018b (0.003) 3.07 (0.25) 0.26 (0.03) 0.40 (0.12) 0.24 (0.03) 0.018b (0.003) 2.22 (0.25) 0.24 (0.03) 30 0.42 (0.12) 0.21 (0.03) 0.020ab (0.003) 2.03 (0.25) 0.20 (0.03) ECUADOR 30 0.50 (0.12) 0.27 (0.03) 0 . 033a (0.003) 2.68 (0.25) 0.29 (0.03) 5 ECUADOR 30 0.58 (0.12) 0.21 (0.03) 0.021ab (0.003) 2.68 (0.25) 0.21 (0.03) 6 MICHIGAN 12 0.66 (0.09) 0.24 (0.05) 0 . 018b (0.004) 1.70 (0.38) 0.24 (0.05) WASHED 81 0.56 (0.04) 0.24 (0.01) 0.021 (0.001) 2.30 (0.10) 0.30 (0.01) NON-WASHED 81 0.52 (0.04) 0.25 (0.01) 0.022 (0.001) 2.63 (0.10)) 0.32 (0.01) NS * NS NS NS ** NS NS * ** NS NS REGION(2) N X 1 ECUADOR 30 0.76 (0.12) 2 ECUADOR 30 3 ECUADOR 4 X (SEM) (SEM) (SEM) S i g n i f i c a n c e of F (3) Region Fa rm /region Type of sample Type X re g i o n (1) (2) (3) NS ** * NS NS ** NS NS N, X, SEM: number of o b s e r v a t i o n s , means and s t a n d a r d e r r o r s of means Region means w i t h i n a column w i th o u t a common s u p e r s c r i p t a r e d i f f e r e n t (p < .05) NS: n o n - s i g n i f i c a n t ( p < . 0 5 ) ; **: p < . 0 1 ; *: p < . 0 5 1 0.9 - DM) 0.6 0.5 pasture 0.7 - (X - calcium 0.8 m \ I 0.4 0.3 0.2 - 0.1 - 0 i hi i m m 3 IV \1 WASHED F igu re 21 . 4 real on 5 6 NON- WASHED Calcium in washed and non-washed p a s t u r e sam ples from f i v e r e g i o n s ( 1 - 5 ) i n th e Chimborazo p r o v in c e o f Ecuador and one r e g io n (6) in Sh iaw assee County, M ichigan. 165 F igure 22). The d i f f e r e n c e s i g n i f i c a n t (p > . 0 5 ) . among r e g i o n a l m e a n s was n o t The d i f f e r e n c e b e t w e e n means o f washed and nonwashed samples was n o t s i g n i f i c a n t in teractio n of type of sam ple w ith (p > .0 5 ), region nor was the (p > . 0 5 ) . The d i f f e r e n c e among f a r m s w i t h i n r e g i o n s was h i g h l y s i g n i f i c a n t (p .0 1 ). The c o r r e l a t i o n c o e f f i c i e n t b e t w e e n p h o s p h o r u s i n p a s t u r e s and s o i l s was 0.317. L a c t a t i n g cows, depending on t h e i r l e v e l o f m i l k p r o d u c t i o n , r e q u i r e from 0.31 t o 0.40% p h o s p h o r u s i n t h e r a t i o n . Growing h e i f e r s and b u l l s , and d ry p r e g n a n t cows r e q u i r e 0.26% phosphorus i n t h e d i e t (NRC, 1978). Phosphorus s u p p le m e n ta tio n i s o f te n n e c e s s a r y f o r h i g h p r o d u c i n g c o w s, and e v e n f o r d r y cows and growing a n im a ls i f t h e y a r e consuming f o r a g e s low in phosphorus s u s h a s t h o s e i n r e g i o n s 2, 3 and 5 o f E c u a d o r , and i n r e g i o n 6 i n Michigan. Calcium and phosphorus a r e u s u a l l y s u p p l i e d t o t h e a n im als a s p a r t o f t h e g r a i n mix. G r a z i n g a n i m a l s t h a t do n o t r e c e i v e c o n c e n t r a t e sh o u l d be p r o v i d e d w ith m i n e r a l s i n a m i n e r a l f e e d e r . C a l c i u m and p h o s p h o r u s s o u r c e s may be mixed w i t h t h e trace m i n e r a l s a l t in a p r o p o r t i o n c a l c u l a t e d t o meet th e r e q u i r e m e n ts , based on t h e s a l t consumption o f t h e a n im a l s . Magnesium The s u g g e s t e d magnesium r e q u i r e m e n t of d r y p r e g a n a n t cows, and g r o w i n g h e i f e r s and b u l l s i s 0.16 p e r c e n t o f t h e d i e t ; it i n c r e a s e s t o 0.20-0.25% p e r c e n t o f t h e d i e t of l a c t a t i n g cows fed s u b s t a n t i a l am ounts o f p r e s e r v e d f o r a g e s a n d / o r c o n c e n t r a t e s (NRC, 1978). Magnesium c o n t e n t i n t h e p a s t u r e samples t e s t e d in 0 .4 phosphorus (% DM) 0.35 J 0.3 0.25 0.2 - 0.15 - pasture ^ 4 . M 0.1 i ii f \ * ! 0.05 H m r \X l WASHED F ig u r e 2 2 . s ii I %* r//y Km vsm s s i ii lion N s 3 1 NON-WASHED Phosphorus in washed and non-washed p a s t u r e sam ples from f i v e r e g i o n s ( 1 - 5 ) in th e Chimborazo p r o v in c e o f Ecuador and one r e g io n (6) in S h ia w a ssee County, M ichigan. 167 t h e p r e s e n t e x p e r i m e n t r a n g e d from 0.20% i n r e g i o n 3 t o 0.26% i n reg io n 1 o f Ecuador. A v e r a g e magnesium c o n t e n t i n p a s t u r e s i n r e g i o n 6 i n Michigan was 0.24% (Table 8, F i g u r e 23). Differences among r e g i o n s , t y p e s o f s a m p le s, and t h e i n t e r a c t i o n between th e two were n o t s i g n i f i c a n t ( p > . 0 5 ) . The d i f f e r e n c e among w ithin (p < . 0 1 ) . r e g i o n s was s i g n i f i c a n t farms The c o r r e l a t i o n c o e f f i c i e n t between magnesium i n p a s t u r e s and s o i l s was 0.228. Magnesium s u p p l e m e n t a t i o n t o t h e d i e t o f c a t t l e in the r e g i o n s s t u d i e d seems u n n e c e s s a r y , e x c e p t when l a c t a t i n g cows a re consuming a high amount o f c o n c e n t r a t e s , s i n c e magnesium c o n t e n t in c orn g r a i n i s low er than in f o ra g e s (Adams, 1975). I t is worth n o t i n g , however, t h a t magnesium oxide in the d i e t h e l p s t o p r e v e n t low m i l k f a t syndrome i n d a i r y cows (Emery e t a l . , 1965). Sodium I n p a s t u r e s , sodium c o n t e n t ranged from 0.018% i n r e g i o n s 1 and 2 o f E c u a d o r and r e g i o n 6 i n M i c h i g a n , t o 0.33% i n r e g i o n 3 in Ecuador ( T a b l e 8, Figure 24). The d i f f e r e n c e i n sodium c o n t e n t i n p a s t u r e s among r e g i o n s was s i g n i f i c a n t (p < . 0 5 ) , as was t h e d i f f e r e n c e among f a r m s w i t h i n r e g i o n s (p < . 0 1 ) . The d i f f e r e n c e among t y p e s o f s a m p l e s and t h e i n t e r a c t i o n o f t y p e s w i t h r e g i o n s were n o t s i g n i f i c a n t (p > . 0 5 ) . The c o r r e l a t i o n c o e f f i c i e n t between sodium i n s o i l s and i n p a s t u r e s was 0.288. The NRC (1978) e s t i m a t e of the sodium req u ire m e n ts of c a t t l e i s 0.18 p e r c e n t o f t h e r a t i o n dry m a t t e r f o r l a c t a t i n g cows, and 0.10% f o r o t h e r types of d a iry c a t t l e . This requirem ent is o b v i o u s l y n o t met by t h e sodium c o n t e n t o f p a s t u r e s a l o n e , so the a n i m a l s ' d i e t s ne ed s u p p l e m e n t a t i o n . When t h e a n i m a l s r e c i e v e (% DM) 0.5 0.2 i posture magnesium 0.3 - ± m 1 2 KZ3 WASHED F igu re 2 3 . 3 4 5 6 reg io n V 7 7 ,\ NON-WASHED Magnesium in washed and non-washed p a s t u r e sam ples from f i v e r e g io n s ( 1 - 5 ) in th e Chimborazo p r o v in c e o f Ecuador and one r e g io n (6) in Shiaw assee County, M ichigan. 0.0 5 0.03 H pasture sodium (% DM) 0.04 - 0.02 - 0.01 - 1 r \X l F ig u r e 24. 2 WASHED 3 4 5 6 reg io n NON-WASHED Y7Z^X Sodium in washed and non-washed p a s t u r e sam ples from f i v e r e g i o n s ( 1 - 5 ) in th e Chimborazo p r o v in c e o f Ecuador and one r e g io n (6) i n S h iaw assee County, M ichigan. 170 c o n c e n t r a t e , so dium c h l o r i d e i s i n c l u d e d i n t h e g r a i n m i x t u r e , u s u a l l y a t a r a t e o f 1% o f t h e g r a i n m i x t u r e . G razing a n im a ls t h a t do n o t r e c e i v e c o n c e n t r a t e need t o be o f f e r e d s a l t , a l o n g w ith o t h e r m i n e r a l s , i n m i n e r a l f e e d e r s i n the f i e l d . s a l t i n t a k e by c a t t l e is v a ria b le , consume on t h e a v e r a g e Voluntary b u t l a c t a t i n g d a i r y cows 45 g p e r d a y . Dry cows and h e i f e r s consume from 15 t o 30 g o f s a l t p e r day (Crampton and H a r r i s , 19 69). T h i s i n t a k e s h o u l d be c o n s i d e r e d when d e t e r m i n i n g t h e p e r c e n t a g e o f each m i n e r a l t o be i n c l u d e d i n the m in e r a l mix. P o ta ssiu m P o t a s s i u m c o n c e n t r a t i o n i n p a s t u r e s r a n g e d from 1.70% i n r e g i o n 6, i n M i c h i g a n , t o 3.07% i n r e g i o n 1 i n E c u a d o r ( T a b l e 8, F i g u r e 25). I n p a s t u r e s , t h e d i f f e r e n c e s among r e g i o n s and t h e i n t e r a c t i o n o f r e g i o n w i t h t y p e o f s a m p l e were n o t s i g n i f i c a n t (p > . 0 5 ) . The d i f f e r e n c e sig n ifican t (p < .0 1 ), potassium (p < .0 5 ). among f a r m s w i t h i n region was as was t h e d i f f e r e n c e between t h e a v e r a g e c o n t e n t o f washed and no n-w ash ed p a s t u r e sam ples The c o r r e l a t i o n c o e f f i c i e n t b e tw e e n p o t a s s i u m i n p a s t u r e s and in s o i l s was 0.268. The p o ta s s iu m r e q u i r e m e n t of d a i r y c a t t l e i s 0.8 t o 1.0% o f t h e d i e t ' s d r y m a t t e r (NRC, 1978; Underwood, 1981). The f o r a g e s a n a l y z e d i n t h i s s t u d y have enough potas si um to meet t h e a n i m a l s ' r e q u i r e m e n ts , but i f g r a i n i s supplem ented to th e r a t i o n t o t a l p o t a s s i u m i n t h e d i e t may be b e lo w t h e i r r e q u i r e m e n t s . g r a i n has around 0.35% p otassium (NRC, 1978). Corn potassium pasture r ^ \l F ig u r e 25 . WASHED N O N -W A S H E D P o ta ssiu m i n washed and non-washed p a s t u r e sam ples from f i v e r e g i o n s ( 1 - 5 ) in t h e Chimborazo p r o v in c e o f Ecuador and one r e g io n (6 ) in S h iaw assee County, M ichigan. ] 72 Cogger The minimum e s t i m a t e d copper re q u i r e m e n t f o r d a i r y c a t t l e i s 10 ppm (NRC, 19 78). C o p p e r r e q u i r e m e n t s m u st be c a l c u l a t e d i n relatio n t o t h e molybdenum c o n t e n t o f t h e f e e d , to in su re a minimum 2:1 r a t i o o f copper t o molybdenum. Pastures i n r e g i o n s 2 and 3 i n E c u a d o r and r e g i o n 6 i n M i c h i g a n had 4 .6 , 4.7 and 5.5 ppm o f c o p p e r ( T a b l e 9, F i g u r e 26). Copper i n p a s t u r e s from r e g i o n s 1, 4 and 5 i n E c u a d o r was 9 .3 , 7 .8 a n d 6.8 ppm. A ll these v alu es a r e b e l o w t h e minimum r e q u i r e m e n t o f 10 ppm, a l t h o u g h t h e c o p p e r t o molybdenum r a t i o was i n a l l th e c a s e s g r e a t e r th an 2:1. The d i f f e r e n c e among r e g i o n s (p < . 0 5 ) , w i t h i n r e g i o n s (p < . 0 1 ) , was s i g n i f i c a n t . and among f a r m s The d i f f e r e n c e s among ty p e s o f sa m ple s and t h e i n t e r a c t i o n between type and r e g i o n were not s i g n i f i c a n t ( p > . 0 5 ) . The c o r r e l a t i o n c o e f f i c i e n t b e tw e e n copper i n p a s t u r e s and i n s o i l s was 0.322. To p r e v e n t c o p p e r d e f i c i e n c y i n c a t t l e , 0.5 t o 1.0% c o p p e r su lfate (0.125 t o 0.250% c o p p e r ) may be added t o t h e s a l t c o p p e r d e f i c i e n t a r e a s (NRC, 1978; Underwood, 1 981). in The t r a c e m i n e r a l s a l t used i n r e g i o n 6 i n Michigan a t t h e time of sampling had o n l y 0.03% c o p p e r . the to tal copper T h i s p e r c e n t a g e i s n o t enough t o r a i s e con cen tratio n s u g g e s t e d by t h e NRC (1978). a ll the six reg io n s in the d iet to 10 ppm, as I t i s p o s s i b l e t h a t a n i m a l s from studyed co u ld b en efit from c o p p e r supplementation v ia the tra c e mineral s a l t . The s u f f i c i e n c y range o f copper c o n c e n t r a t i o n i s 6 t o 20 ppm f o r c o r n , and 11 t o 30 ppm f o r a l f a l f a ( T a b l e 1 . 2 , A p pe nd ix 1). Table 9. Copper, i r o n , z i n c , c o b a l t , and manganese c o n c e n t r a t i o n s i n th e dry m a t t e r of washed and n on -w ashed p a s t u r e s a m p l e s from f i v e r e g i o n s i n t h e Ch imborazo p r o v i n c e of Ecuador and one re g i o n m Shiawasee county, Michigan (1) COPPER ppm REGION(2) X N (SEM) IRON ppm X (SEM) ZINC ppm X (SEM) COBALT ppm X (SEM) MANGANESE ppm X (SEM) 1 ECUADOR 30 9.3 (0.9) 221 (55) 41 (6) 0.25 (0.02) 35 ( 7) 2 ECUADOR 30 4.6 (0.9) 138 (55) 40 (6) 0.15 (0.02) 36 ( 7) 3 ECUADOR 30 4.7 (0.9) 106 (55) 31 (6) 0.20 (0.02) 48 ( 7) 4 ECUADOR 30 7.8 (0.9) 357 (55) 38 (6) 0.18 (0.02) 42 ( 7) 5 ECUADOR 30 6.8 (0.9) 108 (55) 41 (6) 0.26 (0.02) 27 ( 7) 6 MICHIGAN 12 5.5 (1.5) 44 (80) 28 (9) 0.15 (0.03) 46 (12) WASHED 81 6.5 (0.3) 145 (15) 39 (2) 0.19 (0.01) 37 ( 2) NON-WASHED 81 6.6 (0.3) 205 (15) 34 (2) 0.22 (0.01) 40 ( 2) * ** NS NS * ** ** NS NS ** * ** NS NS * ** NS ** S i g n i f i c a n c e of F (3) Region Fa rm /regio n Type of sample Type X r e g i o n (1) (2) (3) * NS N, X, SEM: number of o b s e r v a t i o n s , means and s t a n d a r d e r r o r s o f means Region means w i t h i n a column w ith o u t a common s u p e r s c r i p t a r e d i f f e r e n t (p < .05) NS: n o n - s i g n i f i c a n t ( p < . 0 5 ) ; **: p < .01; *: p < .05 10 9 - copper (ppm ) - 7 - pasture 8 4 - 6 - 5 - 3 2 - 1 - 0 - WASHED F ig u r e 2 6 . Copper i n washed and non-washed p a s t u r e sam ples from f i v e r e g i o n s ( 1 - 5 ) in t h e Chimborazo p r o v in c e o f Ecuador and one r e g io n (6 ) in S h ia w a ssee County, M ichigan. 175 Even though the samples for t h i s i n v e s t i g a t io n rep resen t e n t ir e p la n t s th a t are l i k e l y to have a lower elem ent c o n cen tra tio n than th e p l a n t ' s p a r t s s u g g e s t e d in th e t a b l e , th e ir low copper c o n t e n t may be an i n d i c a t i o n o f low copper a v a i l a b i l i t y in th e so il. A lso , th e copper c o n t e n t in th e s o i l (T ab le 6 ) , as d i s c u s s e d above i s lo w . Copper f e r t i l i z a t i o n may i n c r e a s e the copper c o n t e n t in th e p a s t u r e , and p o s s i b l y im prove th e crop y ie ld , e s p e c ia lly of a lfa lfa and legu m es th a t are h ig h ly re sp o n siv e to copper f e r t i l i z a t i o n . The r e c o m m e n d a t i o n o f t h e E x t e n s i o n S e r v i c e o f M i c h i g a n S t a t e U n i v e r s i ty to c o r r e c t p o s s i b l e copper d e f i c i e n c i e s is a band a p p l i c a t i o n of 6.7 kg o f copper per h e c t a r e (6 l b / a c r e ) per y e a r , u n t i l 18 kg (40 lb ) of copper has been a p p l i e d or u n t i l th e s o i l t e s t i s o ve r 20 ppm copper (Robertson e t a l . , 1981c). Iron According to the NRC (1978), an iron l e v e l o f 100 ppm in the dry matter o f the d i e t should be adequate for a l l needs o f c a l v e s t o 3 months o f a g e , and 50 ppm s u f f i c i e n t fo r a l l o t h e r d a ir y c a ttle . In p a s t u r e s , th e ir o n c o n c e n t r a t i o n ranged from 45 ppm in region 6 in Michigan to 357 ppm in region 4 in Ecuador (Table 9, Figure 27). 100 ppm. A l l regions in Ecuador had an iron co n ten t above The d if f e r e n c e among regions (p < .05) and among farms w ith in reg ion s (p < .01) was s i g n i f i c a n t . Non-washed samples had s i g n i f i c a n t l y more i r o n , 205 ppm, than washed s a m p le s , which contained 145 ppm ( p < . 0 1 ) , in d ic a tin g s o i l contam ination. The e f f e c t o f i n t e r a c t i o n o f ty p e o f sam p le w ith r e g io n was not sig n ific a n t (p > . 0 5 ) . The c o r r e l a t i o n o f i r o n in so ils pasture iron (ppm) 500 S 3 ! F ig u r e 27 . WASHED N O N -W A S H E D Iron in washed and non-washed p a s t u r e sam ples from f i v e r e g i o n s ( 1 - 5 ) in t h e Chimborazo p r o v in c e o f Ecuador and one r e g io n (6) in S h iaw assee County, M ichigan. 177 ( e x t r a c t e d w i t h 0.1 N HC1) t o t h a t i n p a s t u r e s was - 0 . 0 2 . c o r r e l a t i o n of i r o n i n s o i l s The t o pH i n s o i l s was -0.153. An i r o n c o n c e n t r a t i o n o f 45 ppm i n t h e f o r a g e s o f r e g i o n 6 i s n o t enough t o m e e t t h e a n i m a l s ' r e q u i r e m e n t s . H o w ev e r, a t r a c e m i n e r a l s a l t was fed t h a t p r o v i d e d s u f f i c i e n t i r o n f o r t h e animals. Trace m i n e r a l s a l t s have around 0.2 % i r o n (Table 1 . 10, Appendix I). Zinc The e s t i m a t e d z i n c r e q u i r e m e n t o f d a i r y c a t t l e (NRC, 1978). i s 40 ppm Z in c i n p a s t u r e s ( T a b l e 9, F i g u r e 28) r a n g e d from 28 ppm i n . r e g i o n 6 i n M i c h i g a n t o 41 ppm i n r e g i o n s 1 and 5 i n E c u a d o r . A n i m a l s from r e g i o n 6 i n M i c h i g a n and r e g i o n 3 in E c u a d o r may b e n e f i t from z i n c s u p p l e m e n t a t i o n v i a t h e t r a c e m ineral s a l t . There was no s i g n i f i c a n t d i f f e r e n c e among r e g i o n s (p > . 0 5 ) , b u t t h e d i f f e r e n c e among farms w i t h i n r e g i o n s (p < . 0 1 ) and among ty p es of sam ples (p < .05) was s i g n i f i c a n t . The i n t e r a c t i o n between ty pe of sample and r e g i o n was not s i g n i f i c a n t C o r r e l a t i o n c o e f f i c i e n t s were as f o l l o w s : (p > . 0 5 ) . 0.024 between z in c in s o i l s and i n p a s t u r e s , 0.004 b e tw e e n z i n c i n p a s t u r e s and pH i n s o i l s , - 0 . 0 8 6 b e tw e e n z i n c i n p a s t u r e s and p h o s p h o r u s i n s o i l s , and 0.066 between z in c i n p a s t u r e s and i r o n i n s o i l s . The s u f f i c i e n c y range o f zinc f o r c o rn i s 20-70 ppm f o r corn and 21-70 ppm f o r a l f a l f a . Average zin c c o n t e n t i n c o rn sam p le s i n r e g i o n 6 was 23 ppm, i t was 31 i n a l f a l f a . The e x t r a c t a b l e z in c l e v e l i n th e s o i l s in t h i s r e g i o n was a l s o low, as d i s c u s s e d above. Corn i s a c ro p h i g h l y r e s p o n s i v e t o z in c (Robertson and 80 (ppm) zinc 40 30 20 - 10 - 178 5 0 -i pasture 7 0 -I 1 2 4 3 5 6 reg io n CSS F ig u r e 2 8 . WASHED V Z7X N O N -W A S H E D Zinc i n washed and non-washed p a s t u r e sam ples from f i v e r e g io n s ( 1 - 5 ) in t h e Chimborazo p r o v in c e o f Ecuador and one r e g io n (6) in S hiaw assee County, M ichigan. 179 L u c a s , 1 9 8 1 b ) , so i t i s p o s s i b l e t h a t z i n c f e r t i l i z a t i o n w o u ld improve the y i e l d s i n t h i s r e g i o n . To t r e a t a d e f i c i e n t s o i l , a band a p p l i c a t i o n a t p l a n t i n g t i m e o f 3.4 t o 4.5 kg o f inorganic z in c or 0.6 t o 0.9 kg o f o r g a n i c z i n c ( c h e l a t e ) p e r h e c t a r e (3 t o 4 l b / a c r e o r 0.5 t o 0.8 lb/acre) i s recommended. Where z in c i s b r o a d c a s t , r a t e s sh o u ld be i n c r e a s e d . F o r h i g h l y r e s p o n s i v e c r o p s , 28 k g / h e c t a r e (25 l b / a c r e ) of z i n c showed good a v a i l a b i l i t y f o r s e v e n y e a r s . Also, after o f 28 several kg/hectare years of banding (25 l b / a c r e ) zin c, h a s b e en u s e d , when a t o t a l r a t e s c a n be g r e a t l y r e d u c e d , and i n some i n s t a n c e s e v e n e l i m i n a t e d ( R o b e r t s o n and Lucas, 1981b). Cobalt In pastu res c o b a l t con ten t ranged from 0.15 ppm in region 6 in M ichigan t o 0.26 ppm i n r e g i o n 5 in Ecuador (T able 9, F ig u r e 29). R e g io n a l means o f c o b a l t c o n t e n t in p a s t u r e s (p < .05) and means in farms w i t h i n d ifferen t. r eg io n s (p < .01) were sig n ific a n tly The d i f f e r e n c e among means o f type of sample and the i n t e r a c t i o n were n o t s i g n i f i c a n t (p > . 0 5 ) . The c o r r e l a t i o n c o e f f i c i e n t between c o b a l t in s o i l s and in pastures was 0.052. The c o b a l t r e q u i r e m e n t o f d a i r y c a t t l e i s 0.10 ppm o f t h e d i e t ' s d r y m a t t e r (NRC, 19 7 8 ). T h i s r e q u i r e m e n t seems t o be met by t h e f o r a g e s a n a l y z e d i n t h e p r e s e n t i n v e s t i g a t i o n . Trace m in e ra l s a l t s , how ever, a lm o s t alw ays in c lu d e c o b a l t in t h e i r fo r m u la s , u s u a l l y a t a r a t e o f 0.003 t o 0.005% o f t h e m ix t u r e , in order to p rev en t p o s s ib l e d e fic ie n c ie s . 5 180 pasture cobalt (ppm ) 4 -t 1 2 3 4 5 6 reg io n IV q F ig u r e 29 . WASHED U Z7X N O N -W A S H E D C obalt i n washed and non-washed p a s t u r e sam ples from f i v e r e g i o n s ( 1 - 5 ) in t h e Chimborazo p r o v in c e o f Ecuador and one r e g io n (6) in S h iaw assee County, M ichigan. 181 Manganese The m a n g a n es e requirem ent of c a t t l e h a s n o t b een w e l l d e f i n e d b u t t h e su g g e s t e d manganese d i e t a r y requ irem ent i s 40 ppm (NRC, 1978). Manganese c o n t e n t i n p a s t u r e s i n r e g i o n s 1, 2 and 5 i n E c u a d o r was 35, 36 and 27 ppm. I n r e g i o n s 3 and 4 i n E c u a d o r , and r e g i o n 6 i n Michigan, a v e r a g e manganese c o n t e n t in p a s t u r e s was 48, 42 and 46 ppm (Table 9, F i g u r e 30). These f a c t s i n d i c a t e a p o s s i b l e m ang a nes e d e f i c i e n c y i n r e g i o n s 1, 2 and 5. The u s e o f a m anganese c o n t a i n i n g t r a c e m i n e r a l s a l t s h o u l d p r e v e n t a d e fic ie n c y of t h i s m ineral sa lt e lem e n t in the a n im a ls. (Table I . 10, A ppendix I) A ty p ic a l trace contains around 0.2% m a n g a n e s e , which i s enough t o m eet t h e r e q u i r e m e n t s o f d a i r y a n im a l s under most p r a c t i c a l c o n d i t i o n s . T h e r e was a s i g n i f i c a n t d i f f e r e n c e among r e g i o n s (p < .05) and among farms w i t h i n r e g i o n s (p .01). The i n t e r a c t i o n among r e g i o n s w i t h t y p e o f s a m p l e was a l s o s i g n i f i c a n t (p < .0 1). The d i f f e r e n c e among t y p e s of samples was n o t s i g n i f i c a n t (p > . 0 5 ) . The c o r r e l a t i o n c o e f f i c e n t b e tw e e n m anga nes e i n p a s t u r e s and s o i l s was 0.065. The c o r r e l a t i o n c o e f f i c i e n t among manganese in p a s t u r e s and pH v a l u e in s o i l s was -0.323. Molybdenum Molybdenum i s im p o r t a n t i n animal n u t r i t i o n because of i t s i n t e r a c t i o n w i t h c o p p e r and s u l f u r . D iffe re n t authors suggest copper-to-molybdenum r a t i o s ran gin g from 4:1 t o 2:1 i n t h e d i e t o f ru m in a n ts to a v o id m olybdenum-induced copper d e f i c i e n c y in r u m i n a n t s (Underwood, 1981). I n p l a n t s , molybdenum i s e s s e n t i a l fo r n i t r o g e n f i x a t i o n and pasture manganese (ppm ) 80 i^ s l F ig u r e 30. WASHED N O N —WASHED Manganese i n washed and non-washed p a s t u r e sam ples from f i v e r e g io n s ( 1 - 5 ) in th e Chimborazo p r o v in c e o f Ecuador and one r e g io n (6) in Shiaw assee County, M ichigan. 183 n i t r a t e r e d u c t i o n . The p r e s e n c e o f 0.1 t o 2.0 ppm o f molybdenum i n t h e e&r l e a f o f i n i t i a l s i l k i n t h e c o r n p l a n t and 1.0 t o 5.0 ppm i n t h e t o p s i x i n c h e s o f t h e a l f a l f a p l a n t p r i o r t o i n i t i a l f l o w e r i n g i s an i n d i c a t i o n of s u f f i c i e n t amounts o f molybdenum i n the s o i l (Cox and Kamprath, 1972). In the p r e s e n t ex p erim e n t, v a l u e s r a n g i n g from 0.18 ppm ( r e g i o n 6 i n M i c h i g a n ) t o 1.93 ppm ( r e g i o n 3 i n E c u a d o r ) were f o u n d f o r molybdenum i n p a s t u r e s ( T a b l e 10, Figure 31). The molybdenum c o n t e n t i n p a s t u r e s from t h e o t h e r r e g i o n s i n Ecuador r a n g e d from 0.54 ( r e g i o n 1) t o 1.74 ppm ( r e g i o n 5). i n s o i l o f r e g i o n 1 was a l s o lo w . Molybdenum I t is p o ssib le th a t pastures can b e n e f i t from molybdenum f e r t i l i z a t i o n i n r e g i o n s where s o i l molybdenum i s low . In re g io n s where s o i l m olybdenum is r e l a t i v e l y h i g h , such as i n r e g i o n 6, l im i n g would p r o b a b l y make s o i l molybdenum more a v a i l a b l e t o t h e p l a n t s . The E x t e n s i o n S e r v i c e o f Michigan S t a t e U n i v e r s i t y has p u b l i s h e d a p r a c t i c a l g u i d e s on molybdenum and o t h e r m i n e r a l s f e r t i l i z a t i o n (Robertson e t a l . , 1981b). The d i f f e r e n c e s among r e g i o n s , t y p e s o f s a m p l e , and t h e in teractio n were n o t s i g n i f i c n t co n ten t p astu res in sig n ifican tly from (p < . 0 1 ) . molybdenum i n s o i l s (p > .0 5 ). farm s w ith in Mean molybdenum reg io n d iffered The c o r r e l a t i o n c o e f f i c i e n t b e tw e e n and p a s t u r e s was 0.86. The c o r r e l a t i o n c o e f f i c i e n t b e tw e e n s o i l pH and molybdenum c o n t e n t i n p a s t u r e s was -0.106. c o e f f i c i e n t between s o i l pH and molybdenum i n s o i l s was - 0 . 4 4 3 . The c o r r e l a t i o n c o e f f i c i e n t b e tw e e n s o i l pH and molybdenum in p a s t u r e s was -0.106. 184 T able 10. Molybdenum and se lenium c o n c e n t r a t i o n s i n t h e d ry m a t t e r o f washed and non-washed p a s t u r e samples from f i v e r e g i o n s i n t h e Chimborazo p r o v i n c e o f Ecuador and one r e g i o n i n Shiawasee c o u n ty , Michigan (1) MOLYBDENUM ppm SELENIUM ppm X REGION (2) N X (SEM) (SEM) 1 ECUADOR 30 0.54 (0.37) 0.46 (0.06) 2 ECUADOR 30 1.10 (0.37) 0.55 (0.06) 3 ECUADOR 30 1.93 (0.37) 0.41 (0.06) 4 ECUADOR 30 1.09 (0.37) 0.51 (0.06) 5 ECUADOR 30 1.74 (0.37) 0.53 (0.06) 6 MICHIGAN 12 0.18 (0.58) 0.19 (0.10) WASHED 81 1.12 (0.09) 0.46 (0.02) NON-WASHED 81 1.27 (0.09) 0.48 (0.02) NS ** NS NS NS ** NS NS S i g n i f i c a n c e o f F (3) Region F a r m /r e g io n Type o f sample Type X r e g i o n (1) (2) (3) N, X, SEM: number of o b s e r v a t i o n s , means and s t a n d a r d e r r o r s o f means Region means w i t h i n a column w i t h o u t a common s u p e r s c r i p t a r e d i f f e r e n t (p < .05) NS: n o n - s i g n i f i c a n t (p < .0 5 ); **: p < . 0 1 ; *: p < . 0 5 2.8 -j 2 .6 -j 2.2 - 2 - 1.8 H 1.6 H 1.4 185 posture molybdenum (ppm ) 2 .4 -j k \; 0.8 H 0.6 0.4 H 0.2 H 1 2 3 4 5 6 region iX X I F ig u r e 31 . WASHED N O N -W A S H E D Molybdenum in washed and non-washed p a s t u r e sam p les from f i v e r e g io n s ( 1 - 5 ) in th e Chimborazo p r o v in c e o f Ecuador and one r e g io n (6) in S h iaw assee County, M ichigan. 186 Selenium Selenium r e q u i r e m e n t o f rum inants i s not w e l l d e f i n e d , b u t t h e NRC (1978) s u g g e s t s 0.10 ppm. The amount r e q u i r e d depends on t h e c h e m i c a l form o f s e l e n i u m and t h e l e v e l s o f i n t e r f e r i n g o r enhancing f a c t o r s in th e d i e t , i n c l u d i n g v i t a m i n E, su lfu r, l i p i d s , p r o t e i n s , amino a c i d s , and s e v e r a l m ic r o e le m e n ts . The c r i t i c a l l e v e l a t which ru m in ants s t a r t showing s i g n s o f s e l e n i u m d e f i c i e n c y seems t o be a r o u n d 0.05 ppm i n t h e d i e t (Kubota and A l l a w a y , a n i m a l s may be a s factors. 1972 ). low a s The l e v e l o f s e l e n i u m t o x i c t o 3 to 5 ppm. d e p e n d i n g on s e v e r a l The c h e m i c a l form f e d h a s an e f f e c t on t h e l e v e l o f to x icity : t h e n a t u r a l l y o c c u r r i n g o r g a n i c s e l e n i u m fou n d i n p l a n t s i s a p p a r e n t l y much more t o x i c t h a n t h e i n o r g a n i c form (NRC, 1978). T o x i c i t y can a l s o be a f f e c t e d by c om position o f the d i e t , p a r t i c u l a r l y p r o t e i n , s u l f u r , and a r s e n i c . These n u t r i e n t s reduce selenium t o x i c i t y (NRC, 1978). In the present study selenium c o n c e n tra tio n ( T a b l e 10, Figure 32) the low est i n p a s t u r e s was fo u n d i n r e g i o n 6 i n M i c h i g a n (0.19 ppm) and t h e h i g h e s t i n r e g i o n 2 o f E c u a d o r (0.55 ppm). Selenium c o n c e n t r a t i o n i n p a s t u r e s i n th e o t h e r r e g i o n s in E c u a d o r r a n g e d from 0.41 t o 0.53 ppm. A ll th ese v a lu e s are w i t h i n the range o f minimum r e q u i r e m e n ts (0.10 ppm) and l e s s than t o x i c i t y l e v e l s (3 t o 5 ppm) g i v e n by t h e NRC (1978). The d i f f e r e n c e s among r e g i o n s , t y p e s o f s a m p l e , and t h e in teractio n were co n ten t p astu res in sig n ifican tly not sig n ifican t (p .0 5 ). w ith in Mean s e l e n i u m reg io n d iffered The c o r r e l a t i o n c o e f f i c i e n t b e tw e e n 0.9 H (ppm) 0.8 -1 0.7 - 0.5 0.4 -* 187 pasture selenium 0.6 -J 0.3 -i 0.2 - ^ 1 8 2 3 4 5 6 region K 3 F ig u r e 32. WASHED N O N -W A S H E D Selenium i n washed and non-washed p a s t u r e sam ples from f i v e r e g io n s ( 1 - 5 ) in t h e Chimborazo p r o v in c e o f Ecuador and one r e g io n (6 ) in S hiaw assee County, M ichigan. 188 s e l e n i u m i n s o i l s and i n p a s t u r e s was - 0 .1 2 8 . The c o r r e l a t i o n c o e f f i c i e n t b e tw e e n s e l e n i u m i n p a s t u r e s and pH i n s o i l s was 0.2 3 7 . 189 M i n e r a l s in Blood M in e r a l c o n c e n t r a t i o n in b lood i s in g e n e r a l r e g u l a t e d by h o m e o s t a t i c m echan ism s ( M i l l e r , 197 5). M e ta b o lic p r o f i l e s of d a i r y cows u s e d t o a s s e s s n u t r i t i o n a l s t a t u s h a v e shown l i t t l e r e l a t i o n between c a lc iu m and phosphorus i n ta k e and c o n c e n tr a ti o n o f th e same m in e r a l s i n b lood (Parker e t a l . , 1970, B low ey e t a l . , 1975; A l l e n e t a l . , 1970; Payne e t a l . , 1976; R ow lands and P o c o c k , 1976; Adams e t a l . , 1978; Lee e t a l . , 1978; K r o n f e l d e t a l . , 1982; R o u s s e l e t a l . , 198 2). N e v e r t h e l e s s , b lo o d a n a l y s i s i s a f a v o r e d m ethod t o d i a g n o s e m i n e r a l because of its im p o rta n t, sin c e a c c e s ib ility b lo o d n u t r i e n t s i n th e body, is an d e a s e n u tritio n p ro b lem s of h a n d lin g . t h e m ain s y s te m f o r M ore tr a n s p o rt of d e fic ie n c ie s or excesses of a p a r t i c u l a r n u t r i e n t may be r e f l e c t e d in i t s c o n c e n t r a t i o n in th e b lo o d . Calcium A n im a ls c o n su m in g d i e t s low i n c a l c i u m , o r d i e t s w i t h a c a lc iu m - to - p h o s p h o ru s r a t i o o f l e s s th an 1:1 w i l l d e v e lo p s ig n s o f c a lc iu m d e f i c ie n c y such as d e p re ss e d feed i n t a k e , reduced r a t e o f g a i n , re d u c e d m i l k p r o d u c t i o n and o s t e o m a l a c i a b e f o r e t h e c a lc iu m c o n c e n tr a ti o n in b lo od i s reduced (Underwood, 1981). T a b l e 11 shows t h e c o n c e n t r a t i o n o f c a l c i u m , p h o s p h o r u s , so d iu m , p o t a s s i u m and m agnesium i n t h e b l o o d serum o f d a i r y a n im a ls t e s t e d in th e p r e s e n t ex p erim en t. T a b le 1.3 (Appendix I) shows t y p i c a l m in e r a l c o n c e n tr a ti o n i n b loo d plasm a o r serum of ru m in a n ts . T he t y p i c a l ra n g e o f serum c a l c i u m c o n c e n tra tio n r u m i n a n t s i s 9.0 t o 12.0 m g/100 ml (C hurch, 197 6). in Except fo r Table 11. Calcium, phosphorus, sodium, potassium and magnesium concentrations in the blood serum of calves and dairy cows from five regions in the Chimborazo province of Ecuador and one region in Shiawasee county, Michigan (1) CALCIUM mg/100 ml REGION(2) N X (SEM) SODIUM mg/100 ml PHOSPHORUS mg/100 ml 'X (SEM) X (SEM) POTASSIUM mg/100 ml X (SEM) MAGNESIUM mg/100 ml X (SEM) 1 ECUADOR 60 9.47 (0.40) 7.55 (0.74) 477 (22) 25 (1.36) 3.04 (0.20) 2 ECUADOR 60 8.76 (0.40) 6.90 (0.74) 443 (22) 23 (1.36) 3.00 (0.20) 3 ECUADOR 60 8.57 (0.40) 6.25 (0.74) 526 (22) 26 (1.36) 2.96 (0.20) 4 ECUADOR 60 8.64 (0.40) 6.47 (0.74) 432 (22) 26 (1.36) 2.44 (0.20) 5 ECUADOR 60 9.96 (0.40) 6.57 (0.74) 485 (22) 23 (1.36) 3.47 (0.20) 6 MICHIGAN 20 8.14 (0.69) 5.52 (1.29) 380 (39) 20 (2.35) 2.13 (0.35) COWS 160 8.88 (0.12) 4.62 (0.34) 474 ( 5) 24 (0.28) 2.93 (0.05) CALVES 160 9.16 (0.12) 7.35 (0.34) 460 ( 5) 24 (0.28) 2.92 (0.05) NS ** NS NS NS ** ** * NS ** * ** NS ** NS * NS NS NS S i g n if ic a n c e o f F (3) Region F arm /region Type of animal Type X re g io n (1) (2) (3) N, X, SEM: number o f o b s e r v a t i o n s , means and sta n d a rd e r r o r s o f means Region means w ith in a column w ith o u t a common s u p e r s c r i p t a re d i f f e r e n t (p < .05) NS: n o n - s i g n i f i c a n t (p < . 0 5 ) ; **: p < . 0 1 ; *: p < .05 191- r e g i o n s 1 and 5 i n E c u a d o r (T a b le 11, F i g u r e 3 3 ), a v e r a g e serum c a lc iu m l e v e l s in th e r e g io n s s t u d i e d i n Ecuador and i n M ichigan, w ere b e lo w 9.0 m g /10 0. A l l a v e ra g e v a lu e s w ere, n e v e r t h e l e s s , a b o v e 8.0 m g/100 m l. T h e r e was no s i g n i f i c a n t d i f f e r e n c e among re g io n s (p > . 0 5 ) . The d i f f e r e n c e among t y p e s o f a n i m a l s (p > .05) and t h e i n t e r a c t i o n o f t y p e w i t h r e g i o n (p > .05) w ere n o t s i g n i f i c n t e i t h e r , b u t t h e d i f f e r e n c e b e tw e e n fa rm s w i t h i n r e g io n was h i g h l y s i g n i f i c a n t (p < .0 1 ). The c o r r e l a t i o n c o e f f i c i e n t between serum c a lc iu m and serum p h o s p h o r u s was 0.332; b e tw e e n serum c a l c i u m and c a l c i u m in p a s t u r e s i t was 0 .5 0 9 ; b e tw e e n serum c a l c i u m and p h o s p h o r u s i n p a s t u r e s i t was 0.074. Phosphorus Serum phosphorus l e v e l s ranged from 5.52 mg/100 ml in r e g io n 6 i n M ichigan t o 7.55 mg/100 ml i n r e g io n 1 i n Ecuador (Table 11, F i g u r e 3 4 ), b u t t h e d i f f e r e n c e among r e g i o n a l m eans was n o t s ig n ific a n t (p > .0 5 ). A l l th e v a l u e s found a r e w i t h in th e range c o n s id e re d normal f o r ru m in a n ts , which i s 4-9 mg/100 ml (Church, 1976). S eru m p h o s p h o r u s s i g n i f i c a n t l y h ig h er in c a lv e s ( 7 .3 5 m g /1 0 0 m l) was (p < .01) t h a n i n cows (4.62 m g/100 m l ) . Phosphorus v a l u e s of 4-6 mg/100 ml in cows, and 6-8 mg/100 ml in young a n i m a l s , h a v e b e e n o b s e r v e d i n b l o o d p l a s m a (Underwood, 1981). The d i f f e r e n c e among farms w i t h in r e g io n s was s i g n i f i c a n t (p < . 0 1 ) , a s was t h e i n t e r a c t i o n o f t y p e o f a n i m a l w i t h r e g i o n (p < .05). The c o r r e l a t i o n c o e f f i c i e n t between serum phosphorus and p a s t u r e phosphorus was 0.210. 12 -i-------- - SERUM 192 CALCIUM ( m g /1 0 0 m t) 11 H 1 2 ZZ3 F ig u r e 33 . 3 COWS 4. 5 6 REGION E S I CALVES Calcium in th e b lo o d serum o f c a l v e s and d a ir y cows from f i v e r e g i o n s ( 1 - 5 ) in th e Chimborazo p r o v in c e o f Ecuador and one r e g io n (6) in S h ia w a ssee County, M ichigan. 9 SERUM 7 - s i 6 FSI v S3 - 5 z V s /, 4 H z s 3 2 H P7K K N K z $ V /> V. S VS. "V M X z X _ _ 1771 COWS F ig u r e 3 4 . i \ 193 PHOSPHORUS ( m g / 100 ml) 6 -i YV / ' X R3Si9N C Sl II CALVES Phosphorus i n the b lo o d serum o f c a l v e s and d a ir y cows from f i v e r e g i o n s ( 1 - 5 ) in th e Chimborazo p r o v in c e o f Ecuador and one r e g io n (6) in Shiaw assee County, M ichigan. 194 Magnesium The normal c o n c e n t r a t i o n o f magnesium in th e b loo d serum of c a ttle i s a ro u n d 1.8 t o 3.0 m g/100 ml (C h u rch , 1 9 7 6 ). p resent in v e s tig a tio n a l l In th e v a l u e s were w i t h in o r s l i g h t l y above th e c o n c e n t r a t i o n s c o n s id e r e d norm al (T able 11, F ig u r e 35). The m eans o f r e g i o n s d i f f e r e d s i g n i f i c a n t l y ( p < . 0 5 ) , b u t m u l t i p l e c o m p a r is o n s o f a l l r e g i o n a l means ( B o n f e r r o n i 's t t e s t ) showed n o n sig n ific a n t d iffe re n c e s (p > . 1 0 ) . There was no s i g n i f i c a n t d i f f e r e n c e o f serum magnesium among farm s w i t h in r e g io n nor among ty p e s o f a n im a ls (p > .05). was n o t s i g n i f i c a n t e i t h e r The i n t e r a c t i o n o f re g io n w ith type (p > .05). No s ig n s o r h i s t o r y o f magnesium t e t a n y were o b se rv e d in any o f t h e fa rm s s t u d i e d . m agnesium o x i d e in Cows i n r e g i o n th e c o n c e n tr a te 6 w ere p r o v i d e d w i t h t o p r e v e n t low m i l k - f a t syndrome. Sodium and P otassiu m N orm al c o n c e n t r a t i o n s i n t h e b l o o d p l a s m a o f c a t t l e a r e a r o u n d 300 m g/100 ml f o r so d iu m , p o t a s s i u m (C h u rch , 1 9 7 6 ). and 14 t o 18 m g/100 ml f o r I n t h e p r e s e n t i n v e s t i g a t i o n , sodium and p o t a s s i u m l e v e l s i n b l o o d p l a s m a w ere h i g h e r t h a n w h at i s c o n s id e re d normal (Table 11, F ig u r e s 36 and 37). I t is p o ssib le t h a t a t h ig h a l t i t u d e th e c o n c e n t r a t i o n o f t h e s e two e le m e n ts i s in c re a sed , as r e p o r t e d by W ilson (1975). A nim als in th e r e g io n s s t u d i e d looked h e a l t h y , so i t i s p o s s i b l e t h a t t h e s e h ig h e r than n o rm a l sodium and p o t a s s i u m c o n c e n t r a t i o n s i n serum a r e n o t p a th o lo g ic a l. There was no t a s i g n i f i c a n t d i f f e r e n c e among r e g i o n a l means 4 - SERUM 195 MAGNESIUM ( m g / 100 m l) 5 1 2 IT T ! F ig u r e 35. 3 COWS 4 5 6 REGION 1 V \1 CALVES Magnesium in th e b lo o d serum o f c a l v e s and d a ir y cows from f i v e r e g io n s ( 1 - 5 ) in t h e Chimborazo p r o v in c e o f Ecuador and one r e g io n (6 ) in Shiaw assee County, M ichigan. X 600 SERUM SODIUM ( m g /1 0 0 m !) 500 H 400 3 0 0 -> 200 - 100 - 0 1 2 ZZl F ig u r e 36. 3 COWS 4 5 6 REGION S 3 CALVES Sodium i n th e b lo o d serum o f c a l v e s and d a ir y cows from f i v e r e g io n s ( 1 - 5 ) in th e Chimborazo p r o v in c e o f Ecuador and one r e g io n (6 ) in S h iaw assee County, M ichigan. 30 -r 28 - SERUM POTASSIUM ( m g /1 0 0 m l) 26 24 - 22 - 20 - 18 16 14 12 - 10 - 8 - 6 - 4 2 - 1 2 [7 7 1 F ig u r e 37. 3 COWS 4 5 6 REGION [ < 3 3 CALVES P o ta ssiu m i n th e b lood serum o f c a l v e s and d a ir y cows from f i v e r e g io n s ( 1 - 5 ) in t h e Chimborazo p r o v in c e o f Ecuador and one r e g io n (6) in S h iaw assee County, M ichigan. 198 f o r sodium and p o t a s s i u m i n seru m (p > .0 5 ) , b u t t h e d i f f e r e n c e among farm s w i t h in r e g io n s and th e i n t e r c t i o n of type o f anim al w ith re g io n were h i g h l y s i g n i f i c a n t (p < . 0 1 ) . Young a n im als had a s l i g h t l y h ig h e r sodium c o n c e n t r a t i o n in b lo od serum than a d u l t s (p < .0 5 ) . The c o r r e l a t i o n c o e f f i c i e n t between serum sodium and p a s t u r e sodium was -0 .2 1 4 , and th e c o r r e l a t i o n c o e f f i c i e n t between serum p o tassiu m and p a s t u r e p o tassiu m was -0.135. r e c e i v e d s a l t s u p p le m e n ta tio n . A l l a n im a ls s tu d ie d Serum c o n c e n tr a ti o n o f sodium and p o tassiu m i s n o t a good i n d i c a t o r o f th e adequacy o f the d i e t in m eeting th e need f o r t h e s e m i n e r a l s o r o f th e n u t r i t i o n a l s t a t u s o f th e anim al ( M i l l e r , 1974). I ro n The c o n c e n t r a t i o n o f i r o n , c o p p e r , z i n c , m a n g a n e s e , and se le n iu m in b lo o d serum i s shown i n T a b le 11. I r o n c o n c e n tr a ti o n ranged from 325 ug/100 ml in M ichigan t o 446 ug/100 ml in re g io n 3 i n E c u a d o r ( T a b le 1 2 , F i g u r e 38). T y p ic a l iro n c o n c e n tra tio n i n b l o o d p l a s m a i s a ro u n d 150 u g /1 0 0 ml a t s e a l e v e l (C hurch, 1979). B l o o d 's iro n c o n te n t is in c re a se d as a r e s u l t of i n c r e a s e d e r y t h r o p o i e s i s due t o t h e r e d u c e d a t m o s p h e r i c oxygen p ressure. H e m a t o c r i t c o u n t i n s h e e p e x p o s e d f o r 32 d a y s t o low p r e s s u r e (348 mm Hg) s i m i l a r t o t h a t found a t 6200 m of a l t i t u d e , was 37; i n t h e c o n t r o l (640 mm Hg) t h e h e m a t o c r i t c o u n t was 27 (P h illip s e t a l., 1969). R e l a t i v e l y high v a l u e s fo r serum ir o n fo u n d i n M ic h ig a n (240 m a b o v e s e a l e v e l ) a r e p r o b a b l y due t o p a r t i a l h e m o ly sis o f red b lo o d c e l l s . The means o f r e g io n s d id n o t d i f f e r s i g n i f i c a n t l y (p > .0 5 ), Table 12. Iron, copper, zinc, manganese and selenium concentrations in the blood serum from calves and dairy cows from five regions in the Chimborazo province of Ecuador and one region in Shiawasee county, Michigan (1) IRON ug/100 ml REGION(2) X N (SEM) COPPER ug/100 ml X (SEM) 1 ECUADOR 60 443 (22) 83 (7) 2 ECUADOR 60 426 (22) 3 ECUADOR 60 4 ECUADOR 5 6 ZINC ug/100 ml X (SEM) MANGANESE ug/100 ml X (SEM) SELENIUM ug/100 ml X (SEM) 184 (12) 4 .4 8 a (0.60) 2.62 (1.26) 73 ( 7) 171 (12) 1 .0 1 b (0.60) 2.72 (1.26) 446 (22) 86 ( 7) 167 (12) 2 . 26ab (0.60) 7.81 (1.26) 60 392 (22) 72 ( 7) 171 (12) 0 .7 7 b (0.60) 4.09 (1.26) ECUADOR 60 408 (22) 84 ( 7) 164 (12) 2 . 64ab (0.60) 5.90 (1.26) MICHIGAN 20 325 (39) 90 (13) 164 (20) 3 .4 5 ab (1.04) 11.65 (2.36) 160 404 ( 7) 87 ( 2) COWS CALVES 160 430 ( 7) 74 ( 2) 169 ( 3) 172 ( 3) 2.21 2.40 (0.09) 5.80 (0.18) (0.09) 5.87 (0.18) S ig n if ic a n c e o f F (3) Region F arm /region Type o f animal Type X re g io n (1) (2) (3) NS ** * ** NS ** ** NS NS ** NS * * ** NS ** * ** NS ** N, X, SEM: number o f o b s e r v a t i o n s , means and sta n d a rd e r r o r s of means Region means w ith in a column w ith o u t a common s u p e r s c r i p t a re d i f f e r e n t (p < .05) NS: n o n - s i g n i f i c a n t (p < . 0 5 ) ; **: p < .01; *: p < .05 500 3 0 0 -j - 100 - 200 200 SERUM IRON ( u g /1 0 0 m !) 400 H 0 1 2 £23 cows F ig u r e 38. 3 4 REGION E 3J 5 6 calves Iron in th e b lo o d serum o f c a l v e s and d a ir y cows from f i v e r e g io n s ( 1 - 5 ) in th e Chimborazo p r o v in c e o f Ecuador and one r e g io n (6 ) in S h iaw assee County, M ichigan. 201 b u t t h e r e was s i g n i f i c a n t v a r i a t i o n among fa r m s w i t h i n r e g i o n (p < .01) and between ty p e s o f anim al of ty p e w ith c o rre la tio n re g io n w as a l s o c o e ffic ie n t b e tw e e n (p < .0 5 ). sig n ific a n t iro n in The i n t e r a c t i o n (p > . 0 1 ) . serum and iro n The in p a s t u r e s was -0.082. Copper Normal copper c o n c e n tr a ti o n in th e blood o f h e a l t h y a n im a ls ranges f ro m 50 to 150 u g /1 0 0 ml ( U n d e rw o o d , 1 977 ). A c o n c e n t r a t i o n under 50 ug/100 ml i s c o n s id e re d an i n d i c a t i o n of d e f i c i e n c y . H o w e v e r, a n i m a l s w i l l show s i g n s o f d e f i c i e n c y and le s io n s when f e d c o p p e r d e f i c i e n t d i e t s c o n c e n tra tio n fa lls in th e b lo o d . T h is lo n g b e fo r e copper is p r o b a b l y due to h o m e o s ta tic mechanisms ( M i l l e r , 1974), and to th e i n t e r a c t i o n of molybdenum and s u l f u r w ith copper ( M i l l s , 1960). I n f a c t , when sheep were fed a d i e t w ith su p p le m e n ta ry molybdenum a n d /o r s u l f u r t h e i r b lo o d copper c o n c e n t r a t i o n i n c r e a s e d (B rem ner, 197 6). In o th e r c a s e s , a n im a ls i n which th e copper l e v e l in b loo d i s under 50 u g /1 0 0 ml do n o t show s i g n s o f d e f i c i e n c y 1 9 7 6 ). (M ills e t a l . , P u l s (1981) c o n s i d e r s n o rm a l serum c o p p e r l e v e l s t o be 80 -150 u g /1 0 0 m l , d e f i c i e n t l e v e l s t o be 6 -70 u g /1 0 0 m l, and a m a rg in a l o r b o r d e r l i n e d e f i c ie n c y to be 55-80 ug/100 m l. I n t h e p r e s e n t i n v e s t i g a t i o n , b l o o d p la s m a c o p p e r v a l u e s were w i t h in th e range c o n s id e re d normal e x c e p t in re g io n s 2 and 4 i n Ecuador, where l e v e l s a v erag e d 73 and 72 ug/100 ml (Table 12, F ig u re 39). These l e v e l s can be c o n s id e re d m a r g i n a l l y d e f i c i e n t . A n im a ls from r e g i o n s 1, 3 and 5 had 83, 86, and 84 u g /1 0 0 m l o f serum c o p p e r . T h e s e v a l u e s a r e on t h e low s i d e o f t h e r a n g e 110 -r 100 Va V r y / j/ 80 V 70 f t X _ 60 \| \ 7V '/ / j S I 30 20 -'V / Vs 0 II a V. z V /N o z \_ /. / a . /> / 1 v \ & /\\ 6 Z 23 F ig u r e 39. "X / /\ A 10 / \ V, 50 40 Z /\N 7 /\\ COWS REGION K 3 CALVES Copper i n th e b lood serum o f c a l v e s and d a ir y cows from f i v e r e g io n s ( 1 - 5 ) in t h e Chimborazo p r o v in c e o f Ecuador and one r e g io n (6) in S h iaw assee County, M ichigan. 202 SERUM COPPER ( u g /1 0 0 m l) 90 203 c o n s id e re d norm al. serum v a l u e : A nim als from r e g io n 6 had th e h i g h e s t copper 90 u g /1 0 0 m l. At t h e tim e o f s a m p l i n g t h e s e a n i m a l s w ere r e c e i v i n g a t r a c e m i n e r a l s a l t c o n t a i n i n g 0.03% copper. Copper c o n t e n t i n s o i l s and in p a s t u r e s was a l s o a t th e low o r d e f i c i e n t l e v e l s i n t h e a r e a s s t u d i e d . T h i s seem s t o c o n firm a g e n e r a l copper d e f i c i e n c y and to i n d i c a t e th e need fo r copper s u p p le m e n ta tio n i n t h e d i e t o f th e a n im a ls in th e r e g io n s s t u d i e d , and a l s o th e need fo r copper f e r t i l i z a t i o n . R e g io n a l means d i d n o t d i f f e r s i g n i f i c a n t l y (p > . 0 5 ) , b u t th e d i f f e r e n c e among farm s w i t h in r e g io n was d i f f e r e n t ( p < . 0 1 ) . C a l v e s had lo w e r p l a s m a c o p p e r t h a n cows (p < .0 1 ) . T h is i s c o n s i s t e n t w ith th e o b s e r v a t i o n o f B in g le y and D ufty (1969) t h a t c a l v e s had low er copper l e v e l s in b lo o d th a n t h e i r m oth ers. The c o r r e l a t i o n c o e f f i c i e n t between serum copper and p a s t u r e copper was 0.260, and th e c o r r e l a t i o n c o e f f i c i e n t between serum copper and p a s t u r e molybdenum was -0.077. Zinc Z in c c o n c e n tra tio n in b lo o d p lasm a in Ecuador and in M ichigan ranged from 164 t o 184 ug/100 ml (Table 12, F ig u r e 40). These v a l u e s a r e h ig h in r e l a t i o n t o what i s c o n s id e re d a normal ran ge: 8 0 -1 2 0 u g /1 0 0 ml (C h u rch , 1 9 7 6 ). P u l s (1981) c o n s i d e r s n o rm a l serum z i n c l e v e l t o be 7 0 -140 u g /1 0 0 m l , and t h e t o x i c le v e l to se n sitiv e range fro m 520 t o 7500 u g /1 0 0 m l. to z in c c h an g e s in d i e t . B lo o d z in c is R e p e a te d o b s e r v a t i o n s o f plasm a z in c l e v e l s under 40 ug/100 ml a r e an i n d i c a t i o n o f s e v e r e d e fic ie n c y (M ills e t a l . , 1967). T h e re was no s i g n i f i c a n t d i f f e r e n c e among r e g i o n a l means ml) SERUM ZINC (ug/100 - rv] - - V/ a \ z \ - / - V. ' / - * n \ V //I 'S.. - Y' H - v , u - 1 204 200 190 180 170 160 150 14 0 130 120 110 100 90 80 70 60 50 40 30 20 10 0 - M - \i - m VIV h OM — m 1771 F ig u r e 40. V Z V COWS Z Z zz REGION K S CALVES Zinc i n th e b lo o d serum o f c a l v e s and d a ir y cows from f i v e r e g i o n s ( 1 - 5 ) in th e Chimborazo p r o v in c e o f Ecuador and one r e g io n (6) in S h iaw assee County, M ichigan. 205 n o r among t y p e s o f a n im a l (p farm m eans w i t h i n .0 5 ) , b u t t h e d i f f e r e n c e r e g i o n s was s i g n i f i c a n t (p among . 0 1 ) . The i n t e r a c t i o n o f t y p e o f a n im a l w i t h r e g i o n was a l s o s i g n i f i c a n t (p .0 5 ) . The c o r r e l a t i o n c o e f i c i e n t b e tw e e n seru m z i n c and p a s t u r e z in c was 0.107. Manganese T y p ic a l c o n c e n t r a t i o n s o f manganese in b lo o d p lasm a o r serum a r e i n t h e r a n g e o f 2 -3 u g /1 0 0 ml (C h u rch , 1 9 7 6 ). P u l s c o n sid e rs 0.5 u g /1 0 0 ml to be a m a rg in a lly (1981) su ffic ie n t b o r d e r l i n e manganese c o n c e n t r a t i o n in b lo od serum or p la s m a , 0 .6 to 3.0 u g / 1 0 0 ml t o be a d e q u a t e . or and D a ta fro m s e v e r a l i n v e s t i g a t i o n s show t h a t th e l e v e l o f manganese found i n b lo o d v a r i e s c o n s i d e r a b l y a c c o rd in g t o th e a n a l y t i c a l te c h n iq u e used. C o n c e n tra tio n s found i n c a t t l e b lood range from 0.5 t o 27 ug/100 m l, b u t most v a l u e s f a l l between 1 t o 3 ug/100. c o n c e n tra tio n s decrease, but v ery slo w ly , Blood manganese in response to manganese d e f i c i e n c y i n th e d i e t (H id iro g lo u , 1979). I n th e p r e s e n t e x p e rim e n t, serum manganese ranged from 0.77 t o 4.48 ug/100 ml (Table 12, F ig u re 41). d i f f e r e n c e (p < .05) among r e g i o n s . There was a s i g n i f i c a n t The d i f f e r e n c e among fa r m s w i t h i n r e g i o n s (p < . 0 1 ) , and t h e i n t e r a c t i o n o f r e g i o n s w i t h ty p e of a n im a l (p < .01) were s i g n i f i c a n t (p < .0 1 ) . Serum manganese l e v e l s fo r cows and c a l v e s d id n o t d i f f e r s i g n i f i c a n t l y (p > . 0 5 ) . L e v e l s u n d e r o r c l o s e t o 1 u g /1 0 0 ml i n r e g i o n 2 and 4 i n d i c a t e a p o s s i b l e d e f i c ie n c y . P a s tu r e manganese, a s d is c u s s e d a b o v e , was a l s o low in some o f th e re g io n s s t u d i e d . Manganese may be s u p p l i e d to th e a n im a ls in th e tr a c e m in e ra l s a l t . The 8 6 - 5 - SERUM 206 MANGANESE ( u g /1 0 0 m l) 7 - 1 2 ^ 17 7 1 F ig u r e 4 1 . 3 4 5 6 REGION COWS CALVES Manganese i n th e b lo o d serum o f c a l v e s and d a ir y cows from f i v e r e g io n s ( 1 - 5 ) in t h e Chimborazo p r o v in c e o f Ecuador and one r e g io n (6 ) in Sh iaw assee County, M ichigan. 207 c o r r e l a t i o n c o e f f i c i e n t between manganese in serum and manganese i n p a s t u r e s was -0.122. Selenium B lo o d 's s e le n iu m c o n t e n t v a r i e s w ith i n ta k e . Serum se le n iu m o f b e e f s t e e r s i n M i c h ig a n was 4.4 u g /1 0 0 m l when t h e d i e t had 0.085 ppm s e l e n i u m , and i n c r e a s e d t o 6.5 and 7.3 u g /1 0 0 ml when th e a n im a ls' feed c o n ta in e d (U llrey e t a l . , 0.206 and 0.294 ppm o f s e l e n i u m 1977). B lo o d p l a s m a s e l e n i u m l e v e l s o f 1 t o 5 u g /1 0 0 ml i n d i c a t e d e fic ie n c y . A b l o o d l e v e l o f a b o u t 10 u g /1 0 0 ml i s d e s i r a b l e . B lo o d p l a s m a l e v e l s o f a b o u t 20 u g /1 0 0 ml i n d i c a t e t h a t t h e anim al i s r e c e i v i n g to o much se le n iu m and t h a t a t o x ic s i t u a t i o n may e x i s t (Marczewski e t a l . , 1982). P la s m a s e l e n i u m i n E c u a d o r r a n g e d from 2.62 t o 7.81 u g /1 0 0 ml f o r c a t t l e n o t f e d a s e l e n i u m s u p p l e m e n t . The a v e r a g e f o r M ic h ig a n c a t t l e was 11.65 u g /1 0 0 ml when t h e a n im a ls w ere supplem ented w ith a t r a c e m in e r a l s a l t c o n ta in i n g 20 ppm se len iu m i n t h e form o f sodium s e l e n i t e ( T a b le 12, F i g u r e 42). p la s m a a n im a ls se len iu m c o n te n t d i f f e r e d (p < .0 5 ). from in d i f f e r e n t B lo o d reg io n s D i f f e r e n c e s among fa rm s w i t h i n r e g i o n s and t h e i n t e r a c t i o n o f r e g i o n w i t h ty p e o f a n im a l w ere s i g n i f i c a n t (p < .0 1 ). stu d ie d It in is E cuador p o ss ib le are th a t a n im a ls d e fic ie n t in from th e se le n iu m reg io n s and need s u p p l e m e n t a t i o n , e v e n th o u g h p a s t u r e s from t h o s e r e g i o n s had a p p a r e n t l y a d equate s e le n iu m c o n te n t. 20 SERUM SELENIUM ( u g /1 0 0 m l) 19 18 17 16 15 14 13 12 11 10 9 6 7 6 5 4 3 2 1 0 1 2 [7 7 1 F ig u r e 4 2 . 3 COWS 4 5 6 REGION ( V \ I CALVES Selen iu m i n th e b lo o d serum o f c a l v e s and d a ir y cows from f i v e r e g i o n s ( 1 - 5 ) in th e Chimborazo p r o v in c e o f Ecuador and one r e g io n (6) in S h iaw assee County, M ichigan. 209 C o b a lt C o b a l t l e v e l s i n b l o o d a r e v e r y lo w , and t h e r e p o r t s o f c o b a l t c o n c e n t r a t i o n v a r y c o n s i d e r a b l y depending on th e method o f a n a l y s i s used. I n human b l o o d , v a l u e s a s h ig h a s 110 u g /1 0 0 ml an d a s lo w a s 0 .0 0 3 u g / 1 0 0 ml h a v e b e e n r e p o r t e d . fla m e le ss P ritc h a rd a to m ic a b so rp tio n U sin g s p e c t r o p h o m e t r y , B a r f o o t and (1 9 8 0 ), f o u n d 0.12 t o 0.20 u g /1 0 0 ml i n human b l o o d serum . McAdam and O 'D e l l (1 9 8 2 ), u s i n g a l s o a to m ic a b s o r p t i o n , found 7.5 ug/100 ml o f c o b a l t i n th e b lo o d plasm a o f d a i r y cows. B lo o d serum c o b a l t v a l u e s ra n g e d from 0.72 i n r e g i o n 5 i n E c u a d o r t o 1.39 u g /1 0 0 ml i n r e g i o n 1 i n E c u a d o r. A n im a ls i n M ichigan had 1.23 ug/100 ml c o b a l t in th e b loo d serum (Table 13, F i g u r e 43 ). They w ere r e c e i v i n g c o b a l t s u p p l e m e n t a t i o n i n t h e t r a c e m in e r a l s a l t (50 ppm). There was no s i g n i f i c a n t d i f f e r e n c e among r e g i o n s , and th e i n t e r a c t i o n o f r e g io n w ith type o f anim al was n o t s i g n i f i c a n t e i t h e r (p > . 0 5 ) . C a lv e s had a s i g n i f i c a n t l y h ig h e r serum c o b a l t c o n c e n t r a t i o n th an cows (p < .05). 210 T able 13. C o b a lt c o n c e n t r a t i o n in th e blood serum o f c a lv e s and d a i r y cows from f i v e r e g io n s in th e Chimborazo p r o v in c e o f Ecuador and one r e g io n in Shiawasee c o u n ty , M ichigan (1) REGION (2) 2 1 3 4 5 6 ECUADOR ECUADOR ECUADOR ECUADOR ECUADOR MICHIGAN N 5 5 6 6 6 2 X 1.39 0.78 1.05 1.20 0.72 1.23 (0.26) (0.26) (0.24) (0.24) (0.24) (0.42) 1 2 SEM ANIMAL COWS CALVES N 15 15 X 1.16 0.89 (0.09) (0.09) SEM S i g n i f i c a n c e o f F (3) Region Type o f anim al Type X r e g io n NS * NS (1) N: number o f o b s e r v a t i o n s ; X: means; SEM: sta n d a r d e r r o r s o f means (2) Region means w i t h i n a row w ith o u t a common s u p e r s c r i p t a re d i f f e r e n t (p < .05) (3) NS: n o n - s i g n i f i c a n t ( p < . 0 5 ) ; **: p < .01; *: p < .05 3 -r 2.8 - 2.6 - SERUM COBALT ( u g /1 0 0 m l) 2 .4 - 2.2 - 2 - 1. 8 - 1. 6 - / 1 .4 - 1. 2 - 1 - 0.8 - 0.6 - 0 .4 - A :v\ Yk /V 0.2 - v\ 17 / V. /■ / pr / v\\ V A Z 7 x z / /. v \ \ 6 1771 F ig u r e 4 3 . REGION COWS IVsl CALVES C obalt i n th e b lo o d serum o f c a l v e s and d a ir y cows from f i v e r e g io n s ( 1 - 5 ) in th e Chimborazo p r o v in c e o f Ecuador and one r e g io n (6) in S h iaw assee County, M ichigan. 212 G a stro in te stin a l P a ra site s D airy c a t t l e are in te rn a l p a ra site s . commonly in fe c te d w ith a v a rie ty of S e v e r a l i n v e s t i g a t i o n s have d em o n strated t h a t e v e n low p a r a s i t i s m i n young a n i m a l s r e s u l t s i n d e c r e a s e d g r o w th and l a t e r in d e c re a se d m ilk p ro d u c tio n (G ib b s, 1982; Adrichem and Shaw, 1977a & b). The m ain e n d o p a r a s i t e s in c a ttle are n e m a to d e s w orm s), t r e m a t o d e s ( l i v e r f l u k e s ) and c o c c i d i a . O s te rta g ia o ste rta g i is one of th e m ost (ro und The nem atode p a th o g e n ic and e c o n o m ic a lly d e t r i m e n t a l p a r a s i t e s in tem p era te re g io n s such as th e S t a t e o f M ichigan and Ecuador. The o p tim a l te m p e ra tu re fo r th e d e velop m ent o f O s t e r t a g i a 's l a r v a e in th e p a s t u r e ran g e s from 15 t o 25° C. The o p tim a l te m p e ra tu re fo r s u r v i v a l o f th e l a r v a e i s much l o w e r : b e tw e e n 0 and 15° C. H igh t e m p e r a t u r e s a l l o w r a p i d d e velopm ent b u t a s h o r t s u r v i v a l p e rio d ; low te m p e ra tu re s slow d e velopm ent b u t i n c r e a s e th e s u r v i v a l tim e ( S c h i l l h o r n van Veen, 1981). F a s c i o l a h e p a t i c a i s th e most im p o rta n t trem atode i n f e s t i n g d o m e s t i c a n i m a l s and t h e m o st common c a u s e o f l i v e r f l u k e d i s e a s e (M erk, 197 9). h e p a tic a had h ig h e r m ilk D a i r y cows i n f e c t e d w i t h F a s c i o l a p ro d u c tio n when tre a te d w ith h e x a c h lo ro e th a n e th an d id n o n - t r e a te d i n f e c t e d a n im a ls (R andell and B r a d le y , 1980). C o c c id ia i n f e s t a t i o n i n c a t t l e i s t y p i c a l l y a d i s e a s e o f young a n im a ls between the ages o f one t o two months and one y e ar when th e y a r e r a i s e d i n c o n fin e d l o t s . R e s u l t s o b ta in e d in th e p r e s e n t i n v e s t i g a t i o n o f f e c a l egg c o u n t s a r e shown i n T a b l e s 14 and 15. A n im a ls from r e g i o n 6 i n M ichigan d id n o t show s ig n s o f i n f e s t a t i o n , p ro b a b ly due to being T able 14. Region Mean worm burden in fe c e s o f d a i r y c a t t l e from f i v e re g io n s in th e Chimborazo p r o v in c e o f Ecuador and one re g io n in Shiawasee co u n ty , Michigan Haemonchus Oesophagostomum O s te rta g ia mean No. epg mean No. epg mean No. epg mean No. epg No. mean epg (1) COWS CALVES 0 0 0 0 4 1 325 200 2 1 100 300 1 1 100 100 3 2 330 200 2 COWS 2 CALVES 0 3 0 130 0 9 0 490 0 6 0 350 0 5 0 220 1 9 100 400 COWS CALVES 0 0 0 0 0 0 0 0 0 0 0 0 1 0 100 0 0 0 0 0 1 COWS 1 CALVES 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 1 0 100 2 COWS 2 CALVES 0 1 0 600 1 1 300 100 0 0 0 0 1 0 100 0 1 2 200 100 Farm 1 ECUADOR 1 1 3 3 2 ECUADOR 3 ECUADOR (1) T ric h o s tro n g y lu s Cooperia Type of animal 3 3 COWS CALVES 0 — 0 — 2 — 150 — — — 0 1 — 100 — 2 — 100 — 1 1 COWS CALVES 1 0 100 0 1 0 100 0 0 0 0 0 0 0 0 0 0 0 0 0 2 COWS 2 CALVES 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 3 3 0 1 0 100 1 2 100 200 0 2 0 100 0 0 0 0 0 2 0 100 COWS CALVES 0 No. = number of positives out of 10 animals; mean epg = positives mean eggs per gram among Table 14. Region (Cont'd.) Mean worm burden in feces of dairy cattle from five regions in the Chimborazo province of Ecuador and one region in Shiawasee county, Michigan Farm Type of anim al C ooperia Haemonchus Oesophagostomum O ste rta g ia mean No. epg mean No. epg mean No. epg mean No. epg No. mean epg (1) T ric h o s tro n g y lu s 4 ECUADOR 1 1 COWS CALVES 0 0 0 0 0 4 0 175 0 2 0 100 0 0 0 0 0 4 0 150 2 2 COWS CALVES 0 0 0 0 0 0 0 0 1 1 100 100 0 1 0 200 0 2 0 150 3 3 COWS CALVES 0 0 0 0 1 0 100 0 0 0 0 0 0 0 0 0 2 1 100 100 1 1 COWS CALVES 2 1 50 50 3 3 100 120 0 0 0 0 0 1 0 50 2 0 100 0 2 2 COWS CALVES 0 0 — 0 — 0 - 0 — 0 0 — — 0 — 0 — 0 0 0 0 2 2 200 200 0 1 0 200 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 5 ECUADOR 3 COWS 3 CALVES 6 MICHIGAN 1 1 (1) COWS CALVES — 0 — No. = number of positives out of 10 animals; mean epg = mean eggs per gram among positives Table 15. Region Mean nematodes, coccidia and Fasciola hepatica burden in feces of dairy cattle from five regions in the Chimborazo province of Ecuador and one region in Shiawasee county, Michigan Farm 1 ECUADOR Type of animal Nematodes mean No. epg range F a s c i o la h e p a t ic a C o c cid ia mean No. epg number o f p o sitiv e s range COWS CALVES 5 3 520 470 100-1400 100-1000 0 0 0 0 2 2 COWS CALVES 1 9 100 1330 700-2000 2 3 100 170 100- 100 100- 300 0 0 3 3 COWS CALVES 1 0 100 0 1 5 100 500 100-1900 0 0 2 ECUADOR 1 1 COWS CALVES 0 1 0 100 5 0 840 0 400-1700 0 0 2 2 COWS CALVES 4 1 175 600 100- 300 7 1 770 100 100-1700 0 0 3 3 COWS CALVES 2 300 300- 300 — - 0 — 1 1 COWS CALVES 0 2 0 100 100- 100 0 3 0 470 100-1100 0 0 2 2 COWS CALVES 0 0 0 0 0 3 0 430 100-1000 0 0 3 3 COWS CALVES 2 3 100 300 2 2 150 250 100- 200 200- 300 0 0 3 ECUADOR (1) — — 100- 100 100- 500 0 — 0 0 — — 0 — No. = number of positives out of 10 animals; mean epg = mean eggs per gram among positives 215 1 1 Table 15. Region (Cont'd.) Mean nematodes, coccidia and Fasciola hepatica burden in feces of dairy cattle from five regions in the Chimborazo province of Ecuador and one region in Shiawasee county, Michigan Farm Type of animal Nematodes mean No. epg F a s c i o la h e p a tic a C o c cid ia mean No. epg range number of p o sitiv e s range 1 1 COWS CALVES 0 9 0 200 100- 400 0 0 0 0 3 10 2 2 COWS CALVES 2 3 150 270 100- 200 100- 600 0 1 0 100 0 0 3 3 COWS CALVES 2 1 150 100 100- 200 0 1 0 100 5 1 1 1 COWS CALVES 8 6 90 80 50- 150 50- 150 0 0 0 0 2 2 COWS CALVES 0 — 5 200 100- 400 4 — 3 3 COWS CALVES 2 3 200 300 3 0 130 0 100- 200 0 0 6 MICHIGAN 1 1 COWS CALVES 0 0 0 0 0 0 0 0 4 ECUADOR 5 ECUADOR (1) 0 — — “ 100- 300 200- 500 — — — — 0 0 No. = number of positives out of 10 animals; mean epg = mean eggs per gram among positives 217 t r e a t e d w ith t h i a b e n d a z o l e two months b e f o r e Ecuador, farms from a l l th e fiv e s a m p lin g . In r e g i o n s s t u d i e d had some nematode i n f e s t a t i o n . A l l the anim als in Ecuador were on pasture a l l yea r around, e x c e p t th e c a l v e s i n farm t h r e e o f r e g io n o n e. Farms one and two from r e g io n one had th e h i g h e s t number o f a n im a ls whose f e c a l sa m p le s had nematode e g g s p r e s e n t and th e h ig h e s t mean egg per gram count. In s e v e r e c l i n i c a l c a s e s , f e c a l c o u n ts of O s t e r t a g i a eggs u s u a l l y e x c e e d 1000 (Armour, 1970). F e c a l egg c o u n t s a l o n e , h o w e v e r , do n o t p r o v i d e t h e b e s t method o f p a r a s i t e i n f e c t i o n d i a g n o s i s . F a c t o r s such a s c l i n i c a l s i g n s , se a s o n o f th e y e a r , g r a z i n g h i s t o r y , pl asma p e psin o gen, serum albumen and packed c e l l volume p e r c e n t a g e , and r e s u l t s o f p o s t - m o r t e m e x a m i n a t i o n m ust o f t e n be c o n s i d e r e d t o a c c u r a t e l y a s s e s s t h e s e v e r i t y o f nematode i n f e c t i o n (Armour, 1970). In the herds s tu d ie d , t h e p r e s e n c e of nematode eggs i n s e v e r a l a n i m a l s , and t h e f a c t t h a t t h e a n im a l s were g r a z i n g a l l y e a r a r o u n d , i n d i c a t e s t h e need o f p r e v e n t i v e measures and p e r i o d i c t r e a t m e n t . C occidia oocy sts were p r e s e n t in s e v e r a l of the fecal sa m ple s o f t h e a n im a l s s t u d i e d i n Ecuador (Table 15), b u t n o t i n numbers high enough t o i n d i c a t e an a c u t e i n f e s t a t i o n . F a s c i o l a h e p a t i c a eggs (according t o q u a l i t a t i v e a n a l y s i s ) were f o u n d i n t h e f e c e s o f a n i m a l s on f a r m s one and t h r e e o f r e g i o n f o u r , and on f a r m two i n r e g i o n f i v e i n E c u a d o r ( T a b l e 15). At t h e s e f a r m s , t h e a n i m a l s were g r a z i n g on wet p a s t u r e s near c r e e k s or swamps, and a q u a t i c p l a n t s were p r e s e n t . In these c a s e s , p r e v e n t i v e management p r a c t i c e s and a n t i f l u k e t r e a t m e n t 218 are n e c e ss a r y . Nematode i n f e s t a t i o n , i s more s e v e r e , e s p e c i a l l y i n young a n im a l s where i t c a n be p r e v e n t e d by t h e p r o v i s i o n o f c l e a n p a s t u r e s , e i t h e r i n t h e form o f newly p l a n t e d l o t s o r p a s t u r e n o t g r a z e d by c a t t l e i n t h e p r e v i o u s y e a r (Armour, 19 74). T his i s seldom p o s s i b l e , however, and under p r a c t i c a l c o n d i t i o n s t h e use of a n th e lm in tic s is necessary . For e f f e c t i v e p a s t u r e r o t a t i o n and t r e a t m e n t of t h e a n i m a l s , a knowledge o f t h e r a i n p a t t e r n s i s n e c e s s a r y because t h e i n f e s t a t i o n o f nematodes i n t h e a n im a l s i s c l o s e l y r e l a t e d t o weather ( S c h i l l h o r n van Veen, 1976). In th e a r e a s s t u d i e d in E cuad or, th e r a in y s e a s o n (around 400 mm o f rain /year) l a s t s from around October to A p r il. case o f O s te r ta g ia , In the tran sm issio n occurs during the rainy season when the la r v a e grow b e tte r on the p a stu re, and the anim als then show symptoms o f th e i n f e s t a t i o n a t th e b e g in n in g o f th e dry season . T r a n s m is s io n i s low d u r in g th e dry s e a s o n . A n im als s h o u ld be t r e a t e d a t th e b e g in n in g o f th e dry s e a s o n , when th e p a s t u r e s are a l r e a d y d r y , and th en moved t o c l e a n p a s t u r e s . c le a n p a stu res are If not a v a i l a b l e , a new t r e a t m e n t w i t h a n t h e l m i n t i c four or s i x weeks a f t e r the f i r s t tr e a tm e n t i s a d v is a b le (Armour, 1970; S c h illh o r n van Veen, 1976). In Michigan, i f the grazing anim als cannot be moved to c le a n pastures a f te r a f i r s t treatment during a dry period in the summer, the treatment s h o u ld be r e p e a te d a t th e end o f th e g r a z in g s e a s o n , around November (S c h illh o r n van Veen, 1976). In th e U n ite d S t a t e s t h e r e are s i x a n t h e l m i n t i c s approved fo r u se in c a t t l e : th ia b e n d a z o le , le v a m iso le , coumaphos, 219 h alo x o n , p h en o th iazin e lev am iso le have high and m o r a n t e l . degrees T h iabendazole efficacy o t ag ain st an d ad u lt g a s t r o i n t e s t i n a l nematodes and some l a r v a e , and they a r e t h e most w i d e ly used. M o r a n t e l i s co mparable i n e f f i c a c y . a l s o e f f e c t i v e a g a i n s t lungworms. L ev a m iso le i s The remaining t h r e e compounds are g e n e r a l l y l e s s e f f i c a c i o u s , b u t have s p e c i f i c use s. an th elm in tics recen tly approved or a p p r o v e d by t h e FDA a r e in iv erm ectin New the p r o c e s s of being and the benzim idazole d e r i v a t i v e s a l b e n d a z o l e , f e n b e n d a z o l e , and o x f e n d a z o l e (American Assoc. Vet. P a t h o l o g i s t s , 1983). The i n t e r m e d i a r y h o s t o f F a s c i o l a h e p a t i c a i s t h e lymnaeid s n a i l (Lymnaea sp.) which l i v e s i n a q u a t i c e n v ir o n m e n ts. Control m e a s u r e s f o r E\ h e p a t i c a a r e d e s i g n e d t o r e d u c e t h e number o f f l u k e s in t h e h o s t a nim al and t o reduc e t h e s n a i l p o p u l a t i o n in t h e environm ent (Merck, 1979). Whenever p o s s i b l e , c a t t l e sh o u l d not g r a z e in p a s t u r e s c o n t a i n i n g swamps or ponds or near c r e e k s , where t h e s n a i l s grow. anim als, Hay from such p a s t u r e s can be fed t o the since d e s ic c a tio n parasite. k ills the m etacercaria of the M o l l u s c a c i d e s , such as copper s u l f a t e , can be used to c o n tro l the s n a i l p o p u latio n . H e x a c h l o ro e t h a n e was one o f t h e most common t r e a t m e n t s used f o r F a s c i o l a i n t h e U n i t e d S t a t e s u n t i l 1979 when t h e Food and Drug A d m i n i s t r a t i o n rem o ve d i t from t h e m a r k e t a s a p o t e n t i a l c a r c in o g e n . S in c e t h e n , t h e r e i s no f l u k i c i d a l drug a v a i l a b l e i n the Un ited S t a t e s t h a t i s f u l l y approved f o r use i n l i v e s t o c k by t h e Food and Drug A d m i n i s t r a t i o n . anthelm intic s t i l l A l b e n d a z o l e , a broad-sp ec tru m b e ing t e s t e d , has been approved f o r emergency 220 u s e a g a i n s t F. h e p a t i c a and F. magna i n c a t t l e and s h e e p i n some states (American A s s o c . V e t . P a t h o l o g i s t s , countries, c a ttle however, 1983). In o th er there are s e v e ra l flu k ic id e s a v a i la b l e for s u c h a s r a f o x a n i d e , b r o t i a n i d e and n i t r o x y n i l . These compounds can a l s o k i l l immature f l u k e s (Merck, 1979). C o ccid io sis can be p r e v e n t e d by m a i n t a i n i n g s a n i t a r y c o n d i t i o n s when t h e a n i m a l s , e s p e c i a l l y t h e y o u n g , a r e k e p t i n confinem ent. S u l f a d r u g s and a m p r o l i u m c a n be u s e d t o p r e v e n t f u r t h e r i n f e c t i o n (American Assoc. Vet. P a t h o l o g i s t s , 1983). SUMMARY The i n t e r r e l a t i o n s h i p p lan ts, of the m in e ral statu s of so ils, and a n i m a l s was i n v e s t i g a t e d i n f i v e r e g i o n s o f t h e C h im b o r a z o p r o v i n c e o f E c u a d o r and i n one r e g i o n i n S h i a w a s e e c o u n ty , Michigan. There were s e v e r a l m i n e r a l d e f i c i e n c y problem s a f f e c t i n g p l a n t and an im al p r o d u c t i o n . No t o x i c e x c e s s e s of the m i n e r a l s s t u d i e d were d e t e c t e d . F ertilizatio n L iming o f t h e s o i l s i s n e e d e d i n most r e g i o n s f o r o p t i m a l legu m e p r o d u c t i o n . R e g i o n s 1 and 4, where t h e pH was c l o s e t o n e u t r a l , do n o t r e q u i r e l im i n g . N itrogen production. fe rtiliz a tio n is needed f o r c o r n and g r a s s A l f a l f a and mixed g r a s s - l e g u m e p a s t u r e s do not need nitrogen f e r t i l i z a t i o n . Most o f t h e s o i l s o f t h e r e g i o n s s t u d i e d had low t o medium phosphorus c o n t e n t . Phosphorus f e r t i l i z a t i o n i s needed i n t h e s e areas for forage production. I n g e n e r a l s o i l s from r e g i o n 6 had a high phosphorus c o n t e n t . However, phosphorus f e r t i l i z a t i o n i s n e e d e d i n some f i e l d s o f r e g i o n 6 f o r m a i n t e n a n c e o f p e r m a n e n t c r o p s such a s a l f a l f a and g r a s s - l e g u m e p a s t u r e s . P otassium c o n ten t in so ils was h i g h in a l l reg io n s. P o ta ssiu m f e r t i l i z a t i o n i s needed, n e v e r t h e l e s s , f o r maintenance o f permanent c ro p s such as a l f a l f a and g r a s s - l e g u m e p a s t u r e s . T reatment of s e e d s with molybdenum w i l l p r o b a b l y i n c r e a s e grass-legume p a stu re y i e l d s was lo w . in r e g i o n 1 , where s o i l molybdenum I n r e g i o n 6 s o i l molybdenum was r e l a t i v e l y h i g h , b u t 221 222 molybdenum c o n c e n tr a tio n in the forages was low. In t h i s region , l im in g th e s o i l w i l l p r o b a b ly i n c r e a s e th e a v a i l a b i l i t y o f molybdenum for legumes. Zinc f e r t i l i z a t i o n i s needed i n r e g i o n 1 and in r e g i o n 6 f o r c o rn c u l t i v a t i o n . Zinc c o n t e n t i n t h e s o i l and i n f o r a g e s was low in these regions. Copper i n t h e s o i l s from r e g i o n s 2, 3, 5 and 6 was low. P a s t u r e copper was low i n a l l r e g i o n s e x c e p t r e g i o n 1. p articu larly legum es, Forages, grown i n t h e s e r e g i o n s w i l l p r o b a b l y b e n e f i t from c o p p e r f e r t i l i z a t i o n . A l s o , c o p p e r f e r t i l i z a t i o n w i l l i n c r e a s e copper c o n c e n t r a t i o n i n f o r a g e s , p r o b a b l y enough t o meet animal r e q u i r e m e n t s . S ulfur fertiliz atio n is improved f o r a g e p r o d u c t i o n . needed in region 1 and 6 f o r S o i l s u l f u r i n t h e s e r e g i o n s was low. Magnesium f e r t i l i z a t i o n may be needed fo r co rn and o th e r responsive crops in reg io n 6. Calcium, sodium, cobalt, i r o n , manganese and se l e n i u m were fo u n d t o be p r e s e n t i n a d e q u a t e a m ou n ts i n t h e s o i l s t e s t e d , so f e r t i l i z a t i o n w i t h t h e s e m i n e r a l s i s p r o b a b l y n o t needed. Mineral Supplementation for Animals N itr o g e n s u p p l e m e n t a t i o n i s needed in r e g i o n 3 f o r improved animal p r o d u c t i v i t y . H ig h -producing cows i n a l l t h e r e g i o n s w i l l a l s o need e x t r a n i t r o g e n t o meet t h e i r re q u i r e m e n ts . Calcium i n p a s t u r e s was found t o e x i s t in adeq uate amounts in a l l the r e g io n s s t u d i e d . need c a l c i u m s u p p l e m e n t a t i o n . High p r o d u c i n g cows, h o w e v e r , may Calcium s u p p l e m e n t a t i o n may a l s o 223 be needed where t h e a n i m a l s a r e e a t i n g h i g h - g r a i n r a t i o n s . Phosphorus s u p p le m e n t a t io n fo r c a t t l e i s needed in a l l r e g io n s , e s p e c i a l l y for high producing cows. Magnesium c o n t e n t i n f o r a g e s from a l l t h e r e g i o n s s t u d i e d was found t o be adequate t o meet a nim al r e q u i r e m e n t s . Lactating cows fed h i g h - g r a i n r a t i o n s may need e x t r a magnesium t o p r e v e n t low m i l k - f a t syndrome. P o ta ssiu m c o n c e n t r a t i o n i n f o r a g e s from a l l r e g i o n s was found t o be ad eq u ate t o m eet an im al r e q u ir e m e n ts . A n im als on h igh -grain r a tio n s , however, may need e xtra potassium. Sodium s u p p l e m e n t a t i o n i s needed f o r a l l c a t t l e i n a l l th e reg io n s studied. I r o n s u p p l e m e n t a t i o n i s needed f o r c a t t l e i n r e g i o n 6 . I r o n can be p r o v i d e d t o t h e a n im a l s i n the t r a c e m i n e r a l s a l t . Zinc c o n c e n t r a t i o n i n f o r a g e s from r e g i o n s 1 and 6 was low. Animals i n t h e s e r e g i o n s need z i n c s u p p l e m e n t a t i o n in t h e t r a c e m i n e r a l s a l t i n o r d e r t o meet t h e i r r e q u i r e m e n ts . M anganese s u p p l e m e n t a t i o n i s n e e d e d i n r e g i o n s 1, 2 and 5. F o r a g e s from t h e s e r e g i o n s had a m an g a n es e c o n t e n t t o o low t o meet t h e manganese re q u ir e m e n t o f d a i r y c a t t l e . Manganese s a l t s can be p r o v i d e d t o t h e s e a n i m a l s in t r a c e m i n e r a l s a l t . Selenium c o n t e n t i n t h e b l o o d serum o f a n im a l s from a l l t h e r e g i o n s s t u d i e d , e x c e p t r e g i o n 6 , was b e l o w 10 ug / 1 0 0 m l , w h ic h i s considered a d e s i r a b l e l e v e l . Animals from t h e s e r e g i o n s w i l l p r o b a b l y b e n e f i t from s e l e n i u m s u p p l e m e n t a t i o n i n t h e t r a c e mineral s a l t . C o b a l t and molybdenum were found i n t h e f o r a g e s in amounts 224 ad eq u a te t o meet a nim al r e q u i r e m e n ts . In c lu s io n of c o b a l t s a l t s i n t h e t r a c e m i n e r a l s a l t w i l l n o t produce t o x i c e f f e c t s i n the anim als. Copper c o n c e n t r a t i o n i n blood serum was low o r m a r g i n a l i n a l l t h e r e g i o n s s t u d i e d . Copper c o n c e n t r a t i o n i n p a s t u r e s was also below th e requirem ent of 10 ppm i n t h e r a t i o n . C op p er s u p p l e m e n ta t io n i s needed f o r th e a n im a ls in a l l the regions s t u d i e d . Copper s u l f a t e may be added t o t h e t r a c e m i n e r a l s a l t a t a rate of 0 .5 t o 1.0% o f the m ix tu re. The u s e o f c o p p e r f e r t i l i z e r w i l l r a i s e t h e copper c o n t e n t of f o r a g e s and p r o b a b l y improve t h e i r y i e l d . P a r a s i te Control Nematode e g g s w e r e fo u n d i n t h e f e c a l s a m p l e s o f a n i m a l s fro m a l l t h e r e g i o n s s t u d i e d , e x c e p t r e g i o n 6 . R e l a t i v e l y h i g h num bers o f c o c c i d i a o o c y s t s were fo und i n t h e f e c e s o f a n i m a l s from r e g i o n s 1, 2 and 3. F a s c i o l a h e p a t i c a eggs were found i n t h e feces from a n i m a l s in regions 4 and 5. C h e m o t h e r a p y a n d p r e v e n t i v e measures o f p a r a s i t e c o n t r o l a r e needed i n t h e r e g i o n s m e n tio n e d . L it e r a t u r e Cited AAFCO. 1979. O ffic ia l p u b licatio n . Assoc, C o n t r o l O f f i c i a l s I n c . , C h a r l e s t o n , WV. o f Amer. Feed Adams, R.S. 1978. V a r i a b i l i t y i n m i n e r a l and t r a c e e l e m e n t c o n t e n t o f d a i r y c a t t l e f e e d s . J . D airy S c i . 58:1538. A d r i c h e m , P.W.M. v a n a n d J . C . Shaw. 1977a. E f fe c ts of g a s t r o i n t e s t i n a l n e m a t o d i a s i s on t h e p r o d u c t i v i t y o f monozygote tw in c a t t l e . I . Grow th p e r f o r m a n c e . J . Anim. S c i . 46:417. 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I n f l u e n c e o f r a t e o f r e a c t i v i t y o f c a l c i t i c l i m e s t o n e s and l e v e l o f c a l c i u m a d d i t i o n on u t i l i z a t i o n o f h i g h c o n c e n t r a t e d i e t s by b e e f s t e e r s . J . Anim. S c i . 53:112 0. W h e t t e r , P.A. and D.E. U l l r e y . 1978. Improved f l u o r o m e t r i c m eth od f o r d e t e r m i n i n g s e l e n i u m . J . A s so c . O f f . A n a l . Chem. 61:927. 241 W h i t n e y , D.A. 1980. M ic ro n u trien t s o i l t e s t s - zinc, iro n , m an ga nes e and c o p p e r . Recommended C h e m i c a l S o i l T e s t P r o c e d u r e s f o r t h e N o r t h C e n t r a l R e g i o n . B u l l e t i n No. 499. North Dakota A g r i c u l t u r a l E x p e r i m e n t S t a t i o n . N o r t h D a k o t a S t a t e U n i v e r s i t y , Fargo, p. 18. W i g g e r s , K.D., D.K. N e l s o n and N.L. J a c o b s o n . 1975. P r e v e n t i o n o f p a r t u r i e n t p a r e s i s by a l o w - c a l c i u m d i e t p r e p a r t u m : a f i e l d s t u d y . J . D a iry S c i . 58:430. W i l s o n , K.A. 1975. An a sse ss m e n t o f h igh a l t i t u d e g r a s s l a n d s i n Ecuador as a r e s o u r c e f o r l i v e s t o c k p r o d u c t i o n . Ph. D. D i s s e r t a t i o n , Michigan S t a t e U n i v e r s i t y , E a s t Lansing. APPENDIX I 1 -1 Table I . l . N itrogen, phosphorus, potassium , calcium , maganesium, and s u lfu r in s o i l s ; method o f e x tr a c t io n and s u f f i c i e n c y con cen tration range for a l f a l f a and corn SUFFICIENCY RANGE (2) ELEMENT EXTRACTING SOLUTION (1) CORN (3) ALFALFA (4] % NITROGEN Ca(OH)2 s a t u r a t e d 2 .7 6 - 3 .5 0 3 .7 6 - 5 . 5 0 PHOSPHORUS 0.025N HC1 in 0.03N NH4f 0.25-0.50 0 .2 6 - 0 .7 0 POTASSIUM IN NH4OAC pH 7 1 .7 1 - 2 . 5 0 2 .0 1 - 3 . 5 0 CALCIUM IN NH4OAc pH 7 0 . 21 - 1 .0 0 1 . 7 6 - 3 .0 0 MAGNESIUM IN NH4OAc pH 7 0.16-0.60 0 .3 1 - 1 . 0 0 SULFUR Ca(H2P 0 4 ) 2 , 0 . 1 6 - 0 .5 0 0 .3 1 - 0 . 5 0 (1) (2) (3) (4) P 500 ppm Recommended Chemical S o i l T e s t P r o c e d u r e s f o r the C e n t r a l Region (N. Dakota Exp. S t a t i o n ) Vitosh e t a l . (1981) Ear l e a f sample of i n i t i a l s i l k Top s i x in ch e s sampled p r i o r t o i n i t i a l f l o w e r i n g Nortt 1 -2 T able 1 . 2 . ELEMENT I r o n , manganese, molybdenum, z i n c , c o p p e r , and c o b a l t i n s o i l s ; method o f e x t r a c t i o n , range i n c r i t i c a l l e v e l and s u f f i c i e n c y c o n c e n t r a t i o n range f o r a l f a l f a and c orn EXTRACTING SOLUTION RANGE IN CRITICAL LEVEL (1) SUFFICIENCY RANGE (2) CORN (3) ALFALFA (4) ppm 21-250 31-250 MANGANESE 0.1N HC1 20-150 31-100 MOLYBDENUM (NH4 )2C 20 4 , 0 . 1- 2 .0 1 OJ. 0 0.1N HC1 o**• o IRON 1.0-5.0 pH 3.3 ZINC 0 . IN HC1 1.0-7.5 20-70 21-70 COPPER 1.0N HC1 9-20 6 -2 0 11-30 COBALT (5) TOTAL (1) (2) (3) (4) (5) 5.0 Cox and Kamprath (1972) V i t o s h e t a l . (1981) Ear l e a f sample o f i n i t i a l s i l k Top s i x i n c h e s sampled p r i o r t o i n i t i a l flow erin g Kubota and Allaway (1972) 0.07 1-3 T able 1 . 3 . T y p i c a l m i n e r a l c o n c e n t r a t i o n s i n blood serum of ru m in a n ts ( 1 ) CALCIUM PHOSPHORUS SODIUM plasma POTASSIUM MAGNESIUM mg/ 1 0 0 ml 9.0-12.0 4-9 300 14-18 1.8-3.0 IRON COPPER ZINC MANGANESE SELENIUM 2-3 10 -20 ug/ 1 0 0 ml 80-120 5-10 100 COBALT (2) 0 . 3 5 - 6 . 3 0 ug/ 1 0 0 ml (1) (2) Church (1971) Koch e t a l . (1951) or 1-4 T ab le 1 .4 . K ilogram s e s tim a te d o f a 23 cm s o i l pH t o o f lim e sto n e p e r h e c ta r e r e q u ir e d , as from s o i l pH and t e x t u r e , to r a i s e th e pH plow la y e r to pH 6 .5 ; add 1680 kg to r a i s e 6 . 8 (1) S o il pH Range T e x tu re o f-----------------------------------------------------------------------------------------Plow Layer 4 .5 - 4 .9 5 .0 -5 .4 5 .5 - 5 .9 6 .0 - 6 .4 Kg o f lim e sto n e per h e c ta r e C lay and s i l t y c la y 17930 15130 12330 7850 C lay loams or loams 15130 12330 8970 6160 Sandy loams 12330 8970 7850 4480 Loamy sands 8970 7850 6160 3360 Sands 7850 6160 4480 1680 (1) T rasform ed to m e tr ic u n i t s from C h ris te n s o n et a l., 1983 Table 1.5. Nitrogen fertilizer guides for corn (1) Y ie ld G o a l/h e c ta re S h e lle d corn kg/ha Corn s i l a g e 1000 kg/ha ( 2 ) 1700-2550 2550-3390 3400-4240 4250-5090 2 2 .4 -3 1 .4 3 3 .5 -4 2 .6 4 2 .7 -5 3 .8 5 3 .9 -6 7 .3 5100-5950 5960-6830 P re v io u s c ro p or manure a p p lic a tio n Legume and 22000 kg m anure/ha 0 56 112 168 224 Good legume 11 45 101 157 213 269 Manure 22000 k g /h e c ta re 34 67 123 179 235 291 No legum es, no manure 78 112 168 224 280 336 (1) (2) Transform ed to m e tric u n its from Warncke and C h ris te n s o n , 1980 F o r su d a n g r a s s , su d a x , and s i m i l a r c r o p s , u se n i t r o g e n r a t e s c o m p a ra b le t o s i l a g e p r o d u c tiv ity 1 -5 0 T able 1 .6 . Annual phosphorus (P205) and p o tassiu m (K20) recom m endations fo r co rn grown on m in e ra l s o i l s ( 1 ) Y ie ld G o a l/h e c ta re S h e lle d co rn kg/ha Corn s ila g e 1000 kg/ha ( 2 ) T e s t Level ppm 0102030405060- 9 19 29 39 49 59 69 70 0- 49 50- 74 75- 99 100-124 125-149 150-174 175 2550-3390 2 2 .4 -3 1 .4 84 56 28 28 28 28 0 0 3400-4240 4250-5090 5100-5950 4 2 .7 -5 3 .8 5 3 .9 -6 7 .3 3 3 .5 -4 2 .6 Phosphorus recom m endations, kg P 2 0 5 /h e c ta re 5960-6830 140 84 56 28 28 196 168 140 112 84 56 28 112 84 56 28 28 28 0 0 112 0 0 168 140 112 84 56 28 28 0 0 P otassium recom m endations, kg K 20/ha, on sandy loams and loamy sands 168 224 280 336 336 112 168 224 308 280 84 112 252 224 168 56 56 112 196 168 0 28 112 56 140 0 84 0 0 56 0 0 0 0 0 P otassium recom m endations, kg K20 / h a , on loam s, c la y loams and c la y s 168 224 448 336 448 112 168 224 392 336 56 112 168 224 280 0 112 56 224 168 0 0 112 56 168 0 0 0 112 56 0 0 0 0 56 0 - 49 50- 74 75- 99 100-124 125-137 138-149 150-162 163 0 0 0 (1) Transform ed to m e tric u n its from Warncke and C h ris te n s o n , 1980 0 0 1 -7 T ab le 1 .7 . Annual phosphorus (P 2O5 ) an<^ p o tassiu m (K20 ) recom m endations fo r a l f a l f a grown in m in e ra l s o i l (1) Y ie ld , 1000 k g/ha T e s t le v e l ppm 6 .7 - 8 .9 1 3 .6 -1 7 .9 Phosphorus recom m endations, kg P 205 / h e c t a r e 84 56 28 0- 9 10-19 20-29 30-39 40-49 50 9 .0 -1 3 .5 0 0 0 112 140 84 56 28 112 0 0 84 56 28 0 P o tassiu m recom m endations, kg K2o /h e c ta r e on sandy loams and loamy s o i l s 0 - 24 25- 49 50- 74 75- 99 100-124 125-149 150-174 175-200 200 336 280 224 168 112 392 336 280 224 168 56 112 448 392 336 280 224 168 0 0 0 56 112 0 0 56 0 P o tassiu m recom m endations, kg K2° / h e c t a r e on loam s, c la y loams and c la y 0 - 24 25- 49 50- 74 75- 99 100-124 125-149 150-174 175 (1) T ransform ed 1980 112 448 336 224 168 56 112 560 448 336 224 168 0 0 0 56 112 0 0 56 336 224 168 to m e tric u n i ts from Warncke and 0 C h ris te n s o n , T able 1 .8 . Manganese recom mendations fo r band a p p li c a t io n fo r re s p o n s iv e c ro p s grown on m in e ra l and o rg a n ic s o i l s (1 ) Manganese (0. 1 N HC1 E x tra c tio n ) MINERAL SOILS S o il te s t ppm Mn Response Mn-kg/ha Below 5 P ro b ab le 5-10 Above pH 6 .5 ORGANIC SOILS pH 6 .0 - 6 .5 Above pH 6.4 pH 5.8--6 .4 Response Mn-kg/ha Response Mn-kg/ha Response Mn-kg/ha 9 P ro b ab le 7 C e rta in 18 C e rta in 13 P robable 7 P o s s ib le 4 C e rta in 13 P ro b ab le 9 11-20 P o s s ib le 4 None 0 P ro b ab le 9 P o s s ib le 4 21-40 None 0 None 0 P o s s ib le 4 None 0 Above 40 None 0 None 0 None 0 None 0 (1) Transform ed t o m e tric u n i ts from V ito sh e t a l . , 1981 1-9 T ab le 1 .9 . Zinc recom m endations f o r band a p p l i c a t i o n on m in e ra l and o rg a n ic s o i l s ( 1 ) Zinc fo r M in e ral and O rganic S o ils (0 .1 HC1 E x tr a c tio n ) S o il te s t ppm z in c Below 2 pH 6 .7 to 7 .4 Below pH 6 .7 Response Z n-kg/ha Response Z n-kg/ha R esponse Z n-kg/ha C e r ta in 5.6 P ro b a b le 3 .4 P o s s ib le 2.2 3-5 P ro b a b le 3.4 P o s s ib le 3.4 None 0 5-10 P ro b a b le 3 .4 P o s s ib le 2.2 None 0 11-15 P o s s ib le 2.2 None 0 None 0 Above 15 None 0 None 0 None 0 (1) Above pH 7 .5 Recommended r a t e s a re fo r in o rg a n ic s a l t s such a s z in c s u l f a t e ; use o n e -f o u rth t h i s r a t e fo r c h e la te d m a t e r i a l s . T ransform ed to m e tric u n i ts from V ito s h e t a l . , 1981 1 -1 0 T ab le I . 10. C om position and in g r e d ie n ts o f a t r a c e m in e ra l ( 1) G uaranteed a n a ly s is s a lt I n g r e d ie n ts % Z in c , m in. 0.350 z in c o x id e M anganese, m in. 0.200 manganous o x id e I r o n , m in. 0.200 f e r r o u s c a rb o n a te , f e r r o u s s u l f a t e C opper, m in. 0.030 copper oxide C o b a lt, m in. 0.005 c o b a lt c a rb o n a te I o d in e , m in. 0.007 c alciu m io d a te S elen ium , m in. 0.002 sodium s e l e n i t e S a l t , m in. 96.000 sodium c h lo r id e S a l t , max. 98.500 red ir o n o x id e (fo r c o lo r o nly) m in e ra l o i l a n e th o l (1) Hardy S a l t C o ., S t . L o u is , MO 63166. APPENDIX I I II-l CALCIUM SERUM mg/ 1 0 0 ml REGION FARM COWS YOUNG 1 2 7.83 11.07 8.78 3 10.21 10.04 9.70 9.23 1 2 9.69 8.39 3 8.20 9.12 8.84 8.33 8.76 8.76 8.99 9.23 7.33 10.07 7 .4 1 8 .37 8.52 8 .62 8.13 7.76 8.71 9.70 9.43 8.13 8.20 9.09 9.86 9.26 9.87 10.06 9.73 10.98 9 .66 10.26 7.57 8.71 AVG 7.57 8.71 GEN. AVG. 8.88 9 .1 6 1 AVG 2 AVG 3 1 2 3 AVG 4 1 2 3 AVG 5 1 2 3 AVG 6 1 2 PASTURES % DM AVG SOILS ppm WASHED N-WASHED AVG 0.61 0.61 1.16 0.58 0.58 1.05 0.79 0.73 0.32 0.34 0.48 0.30 0.36 0.57 0.38 0.41 0.62 0.36 0.35 0.55 0.28 0.31 0.44 0.38 0.52 0.57 0.62 0.42 0.33 0.50 0.57 0.42 0.36 0.57 0.79 0.51 0.36 0.94 0.57 0 .6 1 0.70 0.61 8.14 0.70 0.61 0.65 1704 9.02 0.56 0.52 0.54 2688 8.88 9.47 8.76 8.57 8.64 9.96 3226 3201 3484 0.76 3303 3067 2792 3276 0.39 3045 2640 1824 1351 0.41 1938 3593 2225 2505 0.49 2774 4035 2773 2881 0.59 3230 1704 3 II-2 PHOSPHORUS SERUM mg/ 100 ml SION FARM 1 1 2 3 AVG 2 8.72 5.73 8.97 7.55 0.30 0.24 0.32 0 .36 0.24 0.32 0.28 0.31 0.22 12.4 10.1 54.7 0.30 25.7 3 7.37 6.66 7.14 5.93 6.96 4.18 8.12 5.69 6.81 1 4.77 6.05 2 6.21 8.02 3 6.50 7.25 5.83 7.10 4.53 6.81 6.17 5.30 7.94 0.22 8.66 5.84 7.30 4.62 6.43 4.62 6.43 5.52 0.25 0.24 61.6 5.99 7.35 6.67 0.24 0.25 26.7 1 2 AVG 1 2 3 AVG 6 6.38 7.08 7.44 5.84 8.13 AVG 5 10.11 WASHED N-WASHED AVG 6.88 3 4 5.73 9.67 3.74 AVG SOILS ppm 1 2 AVG 3 COWS YOUNG PASTURES % DM 1 2 6.90 5.77 6.55 6.25 6.47 6.57 0.18 0.29 0.22 0.20 12.0 12.2 0 .31 6 .5 0.23 0.24 0.29 0.17 0.17 0.28 0.15 0.18 0.21 0.20 0.28 0.23 0.26 0.34 0.24 0.27 0.25 0.28 0.15 0.25 0.18 0.23 0.25 0.21 0.22 0.25 0.24 0.24 10.2 72.5 16.3 26.6 0.21 38.5 15.7 12.0 17.9 0.27 15.2 5.1 4 .6 31.2 0.21 13.6 61.6 3 AVG M. AVG. II-3 SODIUM SERUM mg/ 1 0 0 ml 5ION FARM COWS YOUNG 486 542 407 504 511 411 478 474 456 473 406 473 442 409 445 441 438 542 550 516 568 545 510 543 473 464 453 466 345 394 463 402 457 504 534 488 494 435 498 472 395 365 AVG 395 365 1. AVG. 474 460 1 1 2 3 AVG 2 1 2 3 AVG 3 1 2 3 AVG 4 1 2 3 AVG 5 1 2 3 AVG 6 1 2 PASTURES % DM AVG SOILS ppm WASHED N-WASHED AVG 157 126 117 0.020 0.021 0.015 0.019 0.016 0.018 0.018 0.018 0.018 0.017 0.014 0.021 0.016 0.019 0.023 0.021 167 0.022 110 0.016 0.023 0.017 0.020 0.020 0.030 0.029 0.036 0.036 0.033 0.034 0.032 0.034 0.017 0.018 0.029 0.014 0.014 0.032 0.021 0.020 0.018 0.019 380 0.018 0.019 0.018 166 467 0.021 0.022 0.022 168 477 443 526 432 485 0.018 133 168 190 219 0.019 0.017 0.018 193 126 O'. 020 134 252 211 293 0.033 252 113 144 135 0.021 131 166 3 II-4 POTASSIUM REGION FARM COWS YOUNG 1 2 22 3 22 24 30 23 24 26 24 20 20 23 29 19 22 24 34 24 26 24 25 28 24 25 24 30 24 29 26 27 26 23 22 22 24 25 23 22 24 19 20 AVG 19 20 GEN. AVG. 24 24 1 AVG 2 1 2 3 AVG 3 1 2 3 AVG 4 1 2 3 AVG 5 1 2 3 AVG 6 1 2 28 SOILS ppm PASTURES % DM SERUM mg/ 100 ml AVG WASHED N-WASHED AVG 426 381 735 3.00 2.30 3.47 3.26 2.37 4.07 2.92 3.23 2.31 1.76 2.17 2.12 240 245 1.88 3.18 200 1.98 2.49 2.03 2.24 1.83 1.77 2.23 2.03 2.01 2.38 2.03 2.83 2.21 2.41 2.92 2.31 2.44 2.45 2.87 3.18 2.76 2.40 2.94 1.76 1.66 20 1.76 1.66 1.71 175 24 2.31 2.64 2.47 373 25 23 22 26 26 23 3.07 2.23 514 229 364 301 486 2.02 2.02 384 372 327 450 3.30 3.25 2.66 383 381 352 859 2.67 531 175 3 II-5 MAGNESIUM SERUM mg/ 100 ml PASTURES % DM REGION FARM COWS YOUNG 1 2.94 2.98 3.85 3.31 0.27 0.33 2.21 0.22 0.22 2.95 0.25 0.24 3.26 2.83 0.25 0.26 3.06 2.51 3.13 3.05 3.04 3.24 0.21 0.20 0.21 0.30 0 .3 1 2.90 3.11 0.24 0.25 3.48 3.29 2.63 3.41 2.49 2.44 0.23 0.22 0.20 0.16 0.18 0.17 3.13 2.78 0.20 0.19 1 2 2.82 2.26 3.02 2.49 0.25 0.22 3 2.21 1.86 0.31 0 .3 1 0.25 0.38 2.43 2.46 0.26 0 .31 3.01 3.12 3.68 3.80 3.72 3.47 3.27 3.67 2.01 2.24 AVG 2.01 2.24 GEN. AVG. 2.93 2.92 1 2 3 AVG 2 1 2 3 AVG 3 1 2 3 AVG 4 AVG 5 1 2 3 AVG 6 1 2 AVG 3.04 3.00 2.96 2.44 SOILS ppm WASHED N-WASHED AVG 815 838 758 0.26 0.23 804 793 778 873 0.24 814 654 580 471 0.19 568 569 650 687 0.29 635 0.15 0.16 0.20 0.22 0.24 0.29 0.20 0.22 0.21 0.18 2.13 0.21 0.18 0.19 308 2.93 0.23 0.24 0.23 644 3.47 612 695 768 0.21 691 308 3 II-6 IRON SERUM ug/ 1 0 0 ml REGION FARM COWS YOUNG 462 522 444 388 489 356 476 411 418 388 361 558 411 423 389 464 507 451 423 383 440 469 460 431 433 313 404 368 392 444 383 401 385 336 323 438 516 448 348 467 297 353 AVG 297 353 J. AVG. 404 430 1 1 2 3 AVG 2 1 2 3 AVG 3 1 2 3 AVG 4 1 2 3 AVG 5 1 2 3 AVG 6 1 2 PASTURES ppm AVG SOILS ppm WASHED N-WASHED AVG 167 134 185 358 318 165 162 280 77 78 157 98 138 277 104 171 202 64 74 195 50 51 113 98 364 311 201 702 295 268 292 422 61 124 95 90 131 145 94 122 44 45 325 44 45 45 89 417 145 206 175 170 443 426 446 392 408 141 239 166 221 182 194 268 343 137 269 239 176 259 106 225 188 99 131 357 139 127 120 80 108 109 89 3 II-7 COPPER SERUM ug/ 1 0 0 ml SION FARM 1 3 4 4 .0 5.2 4 .2 3.2 4 .0 13.6 6.8 16.0 4 .5 4 .6 6.1 5.0 4 .0 5.1 3.7 4 .2 5.0 4.3 66 8.2 5 .9 8 .7 9 .4 5.8 9 .1 7 .6 8.1 6.4 6.5 7.6 7.4 6.4 7 .2 5.8 5.2 110 86 92 75 80 1 2 66 53 91 3 80 68 75 71 1 2 96 83 3 112 85 70 73 97 76 1 2 73 67 3 100 48 79 80 64 83 73 86 72 28.6 35.2 29.7 9.9 9.3 31.2 11.8 4.6 13.8 12.3 14.3 12.4 4 .7 13.0 21.3 26.5 21.5 7.8 23.1 1 2 73 68 4 .8 102 8.0 3 97 73 94 90 78 95 85 95 85 90 5.8 5.2 5.5 2.7 87 74 80 6 .5 6.6 6.6 17.1 AVG 6 9.2 3 AVG 5 9 .5 66 72 AVG WASHED N-WASHED AVG 11.1 6.6 68 99 AVG AVG SOILS ppm 10.9 5.7 11.9 1 2 AVG 2 COWS YOUNG PASTURES ppm 1 2 84 17.2 20.4 13.6 6.8 17.0 2.7 3 AVG AVG. II-8 ZINC SERUM ug/ 1 0 0 ml REGION FARM COWS YOUNG PASTURES ppm AVG 135 187 219 168 193 180 187 205 161 137 180 186 159 167 175 196 152 151 177 147 183 166 169 152 133 192 175 158 215 159 183 178 174 178 142 158 158 176 152 163 153 AVG 163 153 158 GEN. AVG. 169 172 171 . 1 1 2 3 AVG 2 1 2 3 AVG 3 1 2 3 AVG 4 1 2 3 AVG 5 1 2 3 AVG 6 I 201 184 171 167 171 164 SOILS ppm WASHED N-WASHED AVG 55 34 42 45 24 49 4 .6 4 .6 44 39 29 56 48 32 34 44 44 37 26 38 29 26 38 29 31 31 49 26 37 50 19 44 38 38 38 65 49 28 36 26 51 30 6 28 6 28 17 3 .7 39 34 37 7 .7 10.2 41 6 .5 15.9 9 .9 10.1 40 12.0 7 .5 8 .5 10.9 31 9 .0 5 .6 4 .9 4 .8 38 5 .1 10.6 14.4 3 .5 41 9 .5 3.7 2 3 II-9 MANGANESE SERUM ug/ 1 0 0 ml JION FARM 1 7.23 1.65 3.41 5.69 5.13 3.76 4.10 4.86 0.96 0.95 0.67 0.98 1.52 0.95 0.86 1.15 1 2 4.28 4.52 3 0.88 2.03 0.92 0.90 3.23 1.28 0.58 0.93 0.63 0.85 0.95 0.66 0.71 0.82 1.90 1.37 1.93 1.31 4.33 4.99 1.73 3.54 3.54 3.35 3.54 3.35 2.21 2.40 1 2 3 AVG 2 1 2 3 AVG 3 AVG 4 1 2 3 AVG 5 1 2 3 AVG 6 COWS YOUNG 1 2 PASTURES ppm AVG SOILS ppm WASHED N-WASHED AVG 30 39 28 43 43 29 32 38 24 27 54 34 30 50 35 38 48 58 36 35 54 58 47 49 60 27 42 54 25 45 43 41 19 39 18 19 56 14 25 30 46 45 3.45 46 45 46 60 2.30 37 40 38 73 4.48 1.01 2.26 0.77 2.64 91 107 144 35 114 53 77 64 36 65 65 31 102 48 66 99 63 71 42 78 59 61 43 27 54 60 3 AVG «. AVG. 1 1 -10 SELENIUM SERUM ug/ 1 0 0 ml REGION FARM COWS YOUNG 1 1.07 3.20 4.40 1.19 3.00 2.83 2.89 2.34 3.75 1.31 4.76 1.31 2.49 2.72 3.27 2.18 8.29 8.77 7.40 3.22 3.22 15.98 8.15 7.47 1 2 6.52 3 4.56 5.31 1.90 4.26 4.36 3.82 4.86 3.94 8.99 3.60 5.43 8.56 5.93 5.86 9.73 13.58 AVG 9.73 13.58 GEN. AVG. 5.72 4.91 1 2 3 AVG 2 1 2 3 AVG 3 1 2 3 AVG 4 AVG 5 1 2 3 AVG 6 1 2 2.01 SOILS ppm PASTURES ppm AVG WASHED N-WASHED AVG 0.42 0.59 0.35 0.50 0.47 0.47 0.45 0.48 0.66 0.35 0.51 0.59 0.39 0.82 0.51 0.60 0.48 0.35 0.41 0.33 0.49 0.37 0.42 0.40 0.45 0.60 0.47 0.43 0.64 0.48 0.51 0.52 0.43 0.50 0.66 0.40 0.47 0.73 0.53 0.54 0.21 0.17 11.65 0.21 0.17 0.19 0.41 5.32 0.46 0.48 0.47 0.85 2.62 2.72 7.81 4.09 5.90 0.20 0.54 1.18 0.46 0.64 0 .4 5 0.46 0.06 0.55 0.32 5.72 4 .2 1 0.30 0.41 3.41 0.06 0.06 0.14 0 .5 1 0.09 0.39 0.07 0.08 0.53 0.18 0.41 3 11-11 COBALT SERUM ug/ 1 0 0 ml SOILS ppm PASTURES ppm AVG COWS YOUNG 1 1 2 2.52 3 1.00 1.17 1.71 0.17 1.76 1.01 0.87 1.38 1.13 0.44 0.11 1.13 0.27 0.38 0.77 1.63 1.14 1.38 0.99 0.93 1.17 0.64 1.40 1.62 0.95 1 .7 2.1 1.12 1.2 2.1 1 .5 2.3 1.22 1.19 1 .7 2.0 1.06 0.33 1.07 0.90 0.42 0.53 2.2 2 .5 2 .5 2.9 3.1 2.7 0.82 0.62 2.4 2.9 1.56 0.91 1 .5 1.4 AVG 1.56 0.91 1.23 1 .5 1 .4 1 .5 0.67 GEN. AVG. 1.16 0.89 1.02 1 .9 2.2 2.1 1.72 AVG 2 1 2 3 AVG 3 1 2 3 AVG 4 1 2 3 AVG 5 1 2 3 AVG 6 1 2 AVG WASHED N-WASHED REGION FARM 1.39 0.70 2.7 2.4 1.8 2.8 2.1 3 .3 2 .4 2.6 1.4 1.3 1.6 2.00 1.2 1.5 1.9 1.58 2.43 1.3 1.7 2.2 1.9 2.3 1.28 1.8 1.49 2.4 1 .5 1.05 1.50 1.20 0.72 2.0 2.0 1.46 2.73 3.40 2 .5 1.5 2.53 2.00 1.11 2.0 1.29 2.63 2.28 1.63 1.8 2.18 1.71 1.53 1.19 2.6 1.48 0.67 3 1 1 -1 2 MOLYBDENUM PASTURES ppm REGION FARM WASHED N-WASHED SOILS ppm AVG 0.53 0 .5 7 0.36 0.73 0.64 0.41 0.49 0.59 1.09 0 .7 1 1.14 0.87 1.64 0.98 1.21 0.67 2.94 2.49 0 .5 0 3.19 1.76 2.03 1.82 0.86 1 .1 3 ' 0.89 1.33 0.88 1.03 1.15 1.83 1 .8 1 0 .7 5 2.56 0 .5 2 2.98 1.47 2.02 0.19 0 .1 7 AVG 0 .1 9 0 .1 7 0 .1 8 0.52 GEN. AVG. 1 .1 2 1 .2 7 1.20 0.24 1 1 2 3 AVG 2 1 2 3 AVG 3 1 2 3 AVG 4 1 2 3 AVG 5 1 2 3 AVG 6 1 2 0.05 0.04 0.05 0.54 0.05 0.33 0.26 0.19 1.12 1.10 0.26 0.17 0.30 0.37 1.93 0.28 0.14 0.15 0.19 1.44 1.09 0.16 0.36 0.18 0.15 1.74 0.23 0.52 3 1 1 -1 3 PASTURES ASH (% DM) CRUDE FIBER (% DM) REGION FARM WASHED N-WASHED AVG 1 13.8 13.1 13.7 16.2 13.2 13.0 14.3 1 2 11.3 10.7 3 12.8 12.4 11.9 17.1 11.6 13.8 14.1 10.7 9 .6 14.3 11.5 11.5 1 2 14.5 3 13.0 19.0 12.9 14.6 13.4 15.5 1 2 9 .9 12.3 11.5 3 10.2 11.7 10.8 11.6 5.0 6.2 5.0 6.2 1 2 3 AVG 2 AVG 3 1 2 3 AVG 4 AVG 5 AVG 1 2 12.2 12.8 13.7 12.7 10.8 9 .5 11.5 14.5 11.6 11.2 WASHED N-WASHED AVG 39.4 33.6 34.5 37.9 31.5 35.8 35.8 35.1 27.9 30.4 34.6 24.2 27.6 30.5 31.0 27.4 33.7 33.9 37.3 32.5 35.0 38.4 35.0 35.3 32.8 34.6 34.7 29.8 32.9 32.4 34.0 31.7 37.4 34.3 36.3 34.4 33.6 34.0 36.0 34.0 29.4 30.7 29.4 30.7 35.4 29.2 35.1 32.9 35.0 3 AVG 5.6 30.0 1 1 -1 4 PASTURE PROTEIN (% DM) SOIL NITRATENITROGEN (ppm) REGION FARM WASHED N-WASHED AVG I 14.0 9 .4 16.6 16.0 1 0.7 1 7.1 13.3 14.6 16.7 13.6 13.0 18.4 14.4 1 6 .5 14.5 16.4 1 2 11.7 9 .1 3 10.1 12.7 9 .3 9 .8 10.3 10.6 1 2 14.1 3 12.3 16.8 12.4 14.3 12.7 14.5 12.6 13.8 18.5 13.5 13.5 16.1 15.0 14.4 14.1 14.0 AVG 14.1 14.0 14.0 15.9 I. AVG. 13.2 14.1 13.7 12.3 1 2 3 AVG 2 1 2 3 AVG 3 AVG 4 AVG 5 1 2 3 AVG 6 1 2 11.6 9.9 12.1 13.8 14.0 11.9 10.9 12.7 15.0 15.4 12.8 18.3 6.0 7 .5 10.4 10.6 8.0 4.2 5.9 1 3.6 6.0 14.8 20.4 15.3 14.7 16.8 15.9 3 1 1 -16 SOIL TEXTURE % DM SAND CLAY 46 58 63 21 20 16 22 21 56 19 25 53 55 48 11 17 17 36 28 34 52 15 33 1 2 61 72 11 27 20 3 66 9 9 66 10 24 56 61 62 14 14 13 30 26 25 60 14 27 56 69 69 14 30 10 9 20 22 65 11 24 55 22 23 AVG 55 22 23 GEN. AVG. 59 15 26 REGION FARM 1 1 2 3 AVG 2 1 2 3 AVG 3 AVG 4 1 2 3 AVG 5 1 2 3 AVG 6 1 2 SILT 32 25 3 1 1 -1 7 SOIL REGION FARM 1 1 2 3 pH ORGANIC NITRATEMATTER NITROGEN % DM PPM 6.64 6.60 6.88 3 .1 4 .5 3 .8 9 .9 12.1 13.8 6 .7 1 3.8 11.9 6 .1 8 6 .5 5 6.16 13.5 7.6 10.8 10.9 12.7 15.0 6.30 10.6 12.8 6.05 5.86 5.43 9 .5 10.2 12.8 18.3 6 .0 7 .5 5.78 10.9 10.6 7 .1 8 6 .9 6 7.36 3 .1 6 .1 5 .5 8 .0 4 .2 5.9 7.17 4 .9 6 .0 6.33 5.52 7.90 9 .7 12.0 2 .5 14.8 20.4 15.3 6 .5 8 8 .1 16.8 5.97 2.3 15.9 AVG 5.97 2.3 15.9 GEN. AVG. 6.43 6.9 12.3 AVG 2 1 2 3 AVG 3 1 2 3 AVG 4 1 2 3 AVG 5 1 2 3 AVG 6 1 2 3 APPENDIX I I I B o t a n i c a l c o m p o s i t i o n s i p a s t u r e s f r o a f i v e r e g i o n s is t h e C h i a b o r a z o p r o v i n c e e l E c u a d o r a n d o e e r e g i o n in S h i a a a s s e e c o u n t ) , M i c h i g a n ALFALFA RE6I0N FARM CORN FESCUE ITALIAN RYEGRASS KIKUYO 6RASS SAMPLE NEEDLE OATS ORCHARD PERENNIAL RYE6RASS RYE SWEET VERNAL VELVET 6RASS WHITE CLOVER WEEDS percent of fresh saople 1 2 3 4 5 82 S3 90 88 94 3 10 t 2 3 4 S 3 90 87 4 98 1 2 3 4 5 98 99 99 83 9 4 24 8 12 9 13 2 i 7 to 3 100 86 4 6 2 2 1 1 29 IS 24 30 -III Table III.I. T i t l e 111.1 . (C o at'd .) N iehlgii B otaaical ALFALFA REGION FARM SAMPLE 2 1 1 2 3 4 5 3 1 2 3 4 S 1 2 3 4 5 CORN FESCUE ITALIAN RTE6RASS KIKUTO 6RASS NEEDLE OATS ORCHARD PERENNIAL RYE6RASS RTE SWEET VERNAL VELVET 6RASS county. WHITE CLOVER WEEDS p e r c e a t of f r e s h s a a p le 5 22 4 5 4 4 32 56 7 1 25 15 60 100 too 17 25 22 II 90 100 i 5 42 60 45 6 S 8 to 2 5 86 4 2 85 5 2 4 3 2 92 50 2 43 3 2 100 93 1 3 III-2 2 c o a p o s i t i o a ef p a s t u r e s f r o a f i v e r e g i o n s ia th e C h ia b o ra z o p r o v i a c e of Ecuador aad one r e g i o a is S h ia w a s s e e (Coat'd.) Michigan Botaaical ALFALFA REGION FARM SAMPLE 3 1 1 2 3 4 5 2 3 CORN FESCUE ITALIAN RYEGRASS KIAUYO GRASS NEEDLE OATS ORCHARD PERENNIAL RYEGRASS RYE SWEET VERNAL VELVET GRASS WHITE CLOVER 65 70 6 4 7 4 6 county, WEEDS percent of fresh saaple t oo 4 t 2 3 4 5 t 2 3 4 5 c o a p o s i t i o a o f p a s t u r e s f r o a f i v e r e g i o n s in t h e C h i a b o r a z o p r o v i n c e o f E c u a d o r a n d o n e r e g i o n in S h i a w a s s e e 15 83 4 52 80 12 39 2D 10 90 100 7 94 20 21 95 86 30 3 3 5 3 75 17 14 9 85 5 to -III Table III.I. Table III.I. (Coat'd.) Michigan Botaaical ALFALFA REGION FARM SAMPLE 4 1 1 2 3 4 5 3 CORN FESCUE ITALIAN RYEGRASS R ix u r o NEEDLE OATS ORCHARD PERENNIAL RYEGRASS RYE SWEET VERNAL VELVET GRASS WHITE CLOVER 63 12 4 2 2 1 3 53 4 12 10 6RASS county, WEEDS percent of fresh saaple 27 69 2 3 27 25 25 t 2 3 4 5 4 52 54 49 4 3 12 2 21 6 6 3 5 40 1 2 3 4 S 9 86 1 22 62 46 4 2 70 41 2 82 1 10 41 30 36 8 3 55 4 7 4 13 III- 2 c s a p o s i t i o n o f p a s t u r e s f r o a f i v e r e g i o n s la t h e C h i a b o r a z o p r o v i n c e o f E c u a d o r a n d o a e r e g i o a in S h i a v a s s e e Table III.I. (Coet'd.) Michigan Botaaical ALFALFA c o m p o s i t i o n o f p a s t u r e s f r o a f i v e r e g i o n s io t h e C h i a b o r a z o p r o v i n c e o f E c u a d o r a n d o a e r e g i o n is S h i a m a s s e e CORN FESCUE ITALIAN RTE6RASS KIKUYO 6RASS t I 1 2 3 4 S 30 34 57 tl to 1 2 3 4 S 2 12 50 t 2 3 100 tOO tOO 4 22 77 5 24 74 I too 2 3 4 tOO 5 6 OATS ORCHARD PERENNIAL RYEGRASS RYE SWEET VERNAL VELVET 6RASS WHITE CLOVER 8 10 5 4 36 2 5 8 4 13 2 39 38 3 35 40 34 1 WEEDS p e rc e n t of f r e s h sample SAMPLE 3 NEEDLE county, tOO tOO too 100 50 7 78 55 33 40 SO 91 5 1 M 2 21 t 10 V •9 I 2