FHE YIELD AND CHEMICAL COMPOSITION OF SOYBEANS AS AFFECTED BY WIDE'LY- VARYING ' NUTRiENT LEVElS Thesis for the boat» of Ph.‘ D. MiCHIGAN STATE UNIVERSITY Aminul Islam 1962 This is to certify that the thesis entitled THE YIELD AND CHEMICAL COMPOSITION OF SOYBEANS AS AFFECTED BY WIDELY VARYING NUTRIENT LEVELS presented by Aminul Is 1am has been accepted towards fulfillment of the requirements for Ph.D. degree in 8011 Science L. S. Robertson Major professor Date W 0-169 LIBRARY Michigan State University .3 YIELD AJD CnnulCnL chPcoi”lCL CF OCLQuATW Aflgk/lq.) 4.).Lr utLJgIJJ. VALill. ‘lG’ loJLLiLa—L.I.L LAVZJIJS by Aminul Islam (‘0 H: (D H 8030 ans Wnicn Wer tilizea witn wiuely varyin5 rates ana combinations of ritr05en, pnospnorus, potassium, calcium, and nia51esiun were 5rown on a Conover silt—loam ! soil in tne field in 1960. In aiaition to ~-'"-r-1r QT “—317? v» .g—EC-L‘JAJ LII...- ' I .L-~4"J-l—J V ‘ifll—hfllJ 5.1.4. " i . J A lIESIS 300303 CF PHI Department of Soil l—J kc- ON I'\) "‘~;". ~-r NW1 f, 4 ”ml-Va.\ \JJ. -v'C-‘-— yul fiI‘J to r ‘._1_. DW“~;I--r -w‘ \ *‘k-L-d-\ I“ Oi L g . *1 _.~_,._,. [*L r'T‘\ -I‘ " "’- .p-JA—JAA u ‘1 D S Bo hy Parents wnose unfailin5 interest anl constant encoura5ement have been a 5reat source of inspiration, this thesis is affectionately deuicatea. ii '7“ ":IWTVF ’1 F‘ ACI:~:C C; ‘. SJJ 3-; adj-J; I i b The author wishes to eXpress his sincere apprecia— tion to Dr. K. Lawton, under Whose supervision this work was initiated, for his interest, assistance, and 5uidance. The author is deeply indebted to Dr. L. S. Robertson for similar guidance and assistance in completin5 this work and pre— parin5 the manuscript. Grateful thanks are exten led to Dr. R. L. Cook who was entirely instrumental in 5ettin5 the forei5n student partial maintena 1ce scholarship for the years 1960—61 and 1961-62. His constant support, e1coura eme11t and valuable su55estions in the preparation of the manuscript are hi5hly appreciated. Special thaidcs are due to Dr. A. R. Wolcott for his helpful su55estions concernin5 certain analytical and sta— tistical procedures applicable to this study and to other members of t1e 5uidance committee, Prof. B. 3. Churchill, Dr. H. C. Beeskow and Dr. G. P. Stei11oauer (uecea we ) for their help and keen interest in the author's 5raduate pro— 5ram. H3 Life—lon5 indebtedness is owed to all the tea01ers o Richi5an State University from whom the author took courses. Their T'1i5h standard of teachin5, accompanied with unparal— leled patience, constancy, assistance, syn1pathy, affection and friendliness will always be remembered. iii The writer is thankful to Mr. C. Price for hi‘ assist- ance in conductin5 the field phases of this study and to his fellow graduate s.ddents for their cooperation and assistance at all times. Finally, the fellowship offered to the author by the ‘U. S. Fulbri5ht Foundation and the financial assistance received from various sources throu5h hichi5an State University are 5ratefully ackn wled5ed. iv P333 0.0.000... I1“! wqr w'ld --1"7-'\"*' ' ‘1. -I....:U.J\JNJ.~J-K."I..0.0.0.....00... V ~""7 ._ TI "- c 1.0 .’-‘, - -L«.ij.LJH OJ... .sJ-‘.u-a-IX--"4L 00.0.0000 00.0...0000 0000000.. 000000000 nitr05en......... 0000000 “‘If‘ P-LOQP£10I’JSOOooooooooooooooooooooooaoooo POJFQ rchgiz'v‘} .3 «1..ou—:-.ooooooooooooooooaoooooooooooooooooooo J D c) "I... '... UJlClL/Jilooooooooooooooooooo 0000000 00.00.0000 1-QL349‘IleSl‘v1—fllooooooooo090.000.000.000... A -.-.‘-t - V}: l -’4~ ,H' ', ‘. .‘A‘ . l 1 r _y- ‘ -l- {- -\ A .7 . r‘q . A '— JLnl,1 iflibLTLJBII 341a LALT.JO g/lltlte 1-0Ln1JCJJLsnl..o c‘ 90 by 00.0000 "' '1 "3":1‘.’«"‘.’1"‘ 1.-.;i.-1b.-0. o o o o o o o 0 ‘;1:3 1V1]: ' A—J‘a‘s A‘fid-‘h‘ VJ.1.:~A&—LJ I [\3 KC 0.00000 '1‘. " «_:_. _‘ - -0 field bbdaieSoaoooooooo u) C) 000.0000 0000.00.000 LabO‘atory Studies 0 0 LI.) u) HQ 301.]. AélalySisooooooo ooooo 00.0.000000 Plant Analysis . . . . . . . 33“ULJ3 AID :ISCJSCICJ.............................. 34 Soil jutrient Levels, Crop Yields, and the Chemical Composition of Soybean Plants as iffected by Three Levels of Complenchtary sociated with Five Levels of ........ 37 060.000. Jutrients Ass il';i.tlflo;;eiloooooooooooooooooooooo rient Contents..... Soil gut Clnop lrielC8000000000.00000.........0.0.00 37 00.0. 33 C 1 --1l cal 1101110051 tic 1. . . VA- 4?). R) Eiscussion............ m1~rfi -m cr‘““ (COlulu%vd) «.Jil-J-LJJNJ 'J- ..-.L.'-J-'- :3 Soil Jutrient Levels, Crop Yiells, and the C11e111icsl Composition of So, was Pls. 11ts as Affectec by Lures Levels of Coialeweqt ry gutrients Associate; t‘ Live Levels of "V'ri U.‘ 0.0.00000000000 fl 0.0.0.0...00000000... P1110 sp 110 111;. C) Soil Iatrient Contentso....o.oo......o... crop Yi 81430000000000ooooooooooooooooaooo 000 00.0.0000. 0.18 113.03.]. COLIlOOSiJCiOllo o o o o o o o 00.0.00...000.. JlSCL-LSSJ-0110000000000.0000. Soil Nitrient Levels, Ci rop lielos, anl tie C1‘1e::1icsl Co;-pos itio11 of So ozoean Plants es Affected by T4198 Levels of Co;-lement;1y gutrients Associatei wits Five Levels of Po see E“ L/WQOv4.0.0.0..000.00.0000000.00.00.00.000000 + 1; uGilUSooooooooooo Soil Nutrient Con crop Yiel\:-SOOOOOOOOOOO0.000000.0. Chemical Composition............. miovw -iooooooooooooooooooooooo Discuss Soil “ubr ent Levels, Crop Yielis, 3111 t1e Chemical Composition of Soybes1 Plants as Co: -plem ntsiy Affectei by Inree Levels of Nutrients Associateo wits lTive Levels 0: y“ W a“-'~ caiClMJoooooooooono.ooooooooooooooooooooooo tentsoo.......... Soil Jutrient Con 0.0.00.000 crop EurielJSOOOOOOOOOOOOOOO 00000.0... C11emic l Comloosition...o.o -Jib CLIS 310:1.000000000000.00.00.00000 vi \{1 U1 U7 \5 1 \fl U) 73 a N‘Tfl 11.11.14 . ” J-”1‘ Ell/l"; “he Soil Jutrient Levels, Crop Yielos, anemical Composition of Soybean Planus as V M Affect e; by luree levels of Co; 1p eoe111“J ive Levels of 104 Jutrients Ass ooiatel wita I'LvaSllleSimll...OOOOOOOOOOOOOOOO0.000000000000000. 104 Soil ;vtrient Contents....o.... 104 «.2301? Vie lUuSooooooooooooo .L. J. C-1e1.1ioal Conposi tion, . . . a 1, . 105 C 3isoussion.....ao....... .-.+,-. #31» ‘ W (W (‘1 S‘t-u"“'- LJ-f A$13 VL1ULJD 1-10.00000000000 '73-1—1fl‘fi-w-‘1« OOOOOOCOOOOOOCOOOOO LI :31.) L: :LTJlLu U .La...‘ 'vii LlS'l‘CI'1 AJL?‘ TAB :3 “ tes of elements usei in the field e: {perinerit .0 L‘suu 0:1 soybeanSOOOOOOOOOOO0.0.0.00.00.00.00.0000°... Avera5e soil test results as affecteu bJ t:ree levels of comple nen1tarJ “utIic1‘s associa with five levels of nItro5On..................... Avera :e leaI and stem Jiells of sOJbean at tnree sta5 es of O evelopm nt as aIIecte¢ by tnree levels of OOLpleLentarJ nutrients associated witn five levels of nitrO5en..o..................1......... Avera5e soybean seeu Jielas as affectel bJ tnree levels Of connlementa"v nutrients associa tea “Iii-Ill fiVe levels Of ni01058110000000...oooooocoooo Average nitro 5en content of SOJbean leaves ani stems at tnree sta5es of development as affectei bJ tnree levels of complementaIJ nutrients asso— ciated witn five levels of nitrO5en.............. Avera5e pnosphorus content of soybean leaves ana stems at t11ree sta5es of development as affects; OJ tnree levels OI complene terJ nutrients asso~ ciated wi tn Iive levels of nitrO5en............. Average potass um content of sOJoean leaves ar l stems at tllree sta5es of uevelopLent as aIfecte; bJ three levels OI conglenentary nitrients asso— ciatea witn five levels of nitrO5en............. Averare calcium content of SOVbe an leaves an; Q J stems at tnree sta5es of uevelopLe nt as aIfecteI by tnree levels of compleLentarJ nutrients asso— ciated witn five levels of nitrogen..°.......... Avera5e ma5nesium content of SOJbean leaves an& stems at tnree sta5es of development as affectei by three levels of complenlentarJ nutrients asso— ciated witn five levels OI nitrO5e11.......o..... viii 1U :11. £1 1 33 47 \JT H t4 13111-3 I o . ll. 12° 13° 14. 17° 19. Ill-S: CF TI'LZLES (COI’I'ClllueI) Avera5e tota -l su5a r anI aLino nit rO5en content Of SOJ ean leaves 1? steIs (IlO/Gfll‘ sta5e) as affecteI bJ tniee levels of coIpleLentarJ nutrients associate; with five levels Of filtromo10oooooooooooooon...0.0090000090000000... Avera5e soil test results as affected bJ three levels Of complementa'J natrients associateI witi five levels Of phosphorus....a..ooo...oo.o. ” Avera5e leaf an; stem Jiel;s of SOJOeal'ls at tnree sta5es of IevelOpLent as effecteI OJ tnree levels of cor. ple;1ent‘;J nutrients essOOIIteI with five levels of osO110ras.....o.....o.....o...... 6C Average sOJoean seea JielIs as affectea by three levels of comple Len tzirJ Irtrients associate? witn five levels Of JhOSZjLOrJOoooooooooooooooooooooooo 65 Avera5e nitrO15 en conte W10 of so;oea n lee ves anI stems at tires sta es Of Ievelopme11t as affe cteI bJ t- as levels OI codalegentarJ nntiieius asso— ciate; witn five levels of phospgorus ooooooooooo 67 fixr311‘1~ort‘s cthent Of soyoean leav M ~ I AVGFEJe es 1 stems at tIree sta5es of IevelOQIIOI as aifecteI bJ tnree levels of complementar nicrIcnt asso— OiateI with five levels of phospnorus.........o. 58 Iverace potassian content Of sOJOean leav ves cni teLs at three sta5es Of IevclonI nt as affectea OJ three levels of 00*“I.“fle111,1t:1‘"\r nutrients asso— ciateI with five levels Of pnospnorus...o..o.... 69 Avera5 e calciIm content of sOJoee n leaves a :11- ster“;1s at tnree sta5es of LevelOpIInt as affe cteI OJ tMI ee levels of comnleienta IJ nutrients a 080- 70 Ciaa Me with five levels of pIosphorus........... Avera5e La5nesium content of sOJbean leaves anI stems at tnree sta5es of IevelOpLent as affectel OJ three levels of complementary nutrients as so- ciateI with five levels Ofn IOsnIorus........o.° 71 ar anI amino nitro 5en content of soybean leaves LII stems (floweri In5 sta 5e) as affecteI bJ ree levels Of complementary nutrients associateI with five levels of phosphoruso..oooo. Avera5e total SQ 72 ix m a 7“ .111111;.L 20. 21. 22. 23. 24. 26° 29. L133 0? EABLES (Contin1e1) Ave"a e soil test results as affecte1 by three levels of co:1ole1e1t rJ nutrients associa ate1 W1Ju11liVe leVelS OfllOUQSSiLAJloooooooooooooooooooo .1. Average le a” an1 stem 31e11s of soybeans at Lh1ee sta; es o1 aevelOpment as a1fecte1 bJ taree levels of complementary nutrients associate; with five levels of potassium.............................. Average soybean see1 3iel1s as affecte1 bJ taree levels of COAU18”810““J llutrients associate1 wit1 Iive levels Of DouaSSimmooooooooooooooooooooooooo ov_e n co:1tent of s03roean le1ves Avera e nitr 1 an; t-ems -t tnree sta’es of Cevel pment as affecte1 bJ t1ree levels of 00:; ple heuLarr n‘1trie1tasso— ciate1 with five levels OI pota ssiLL............. Average pnosj1oras content of sOJoean ler1ves a11 stems at three stages of 1evelowm eat as affecte1 bJ three levels of corple1c1t1rJ iatrient s asso- Late1 wit1 five levels of poiass11mo..o.oo.o.... Average potassium content of s0Joea1‘1 leaves an1 stems at tiree sta es of development a,s affecte1 by tnree levels of couple11eat1arJ n1tr1ents asso— 01ate1 witn five levels of poLas511“............L Averagec alci1L co;1te:1t of sonean leaves a::1 steals at tlree staL :es of 1ev elOpment as af1ecte1 bJ tAree levels 01 co; fle.e1LorJ nutrie:1ts asso— cia Le1 wits 11ve levels 0” pot assi1m.......o..... Average 1.,me1 um content of s0Jbean leaves ang stems at t1ree sta es of o-evelopment as affectei DJ three levels of comple1e31113 nr_trients asso- ciatei with five levels of poLassi1a............. Average total S1011 ani amino nitm°o e1 contei' 1t of sOJoean leaves an1 stems (flowerin stage) as C) 41 CO U1 CO ~J (33 CD affecte1 bJ taree levels of complementary ‘utrients ssociatei witn five levels of potassium......... m -. A Q (“a " C1 ' *QC‘J‘ 3r J‘m mr‘ ”'0 DD "13: w-l.’ -‘1‘ngg vcrabe Oll LesL rLs1 Ls as 11110111 :3 -1eL - 1 1.-. .1- \ . -- .3. lerels cf co1g>L1111LarJ n1L11ean a -0: 1- L¢Je le V'Sls I CMlCiwmooooooooooooooooooooooooooo 1 -:' .- 41' qu- 4L A '7»? (fl"‘7'“-‘ 1. .L .14"; «.LL J-L-d .4 30. Aver3;3 lae 3f 3n; sten Ji3l§s of soJUU3ns 3t three st:3 es of levelo1nent 3s 3ffecte1 by fi1ree levels of c 331: 1311t3 ry nutrients asso- ciatel Jitn five levels of C1lcium............... 3l. Aver3“e see; yiells as 3ffectei by three levels of comtlU1ent3rJ n3trie:1ts associstel with five levels of celc11m................................ \f.) ~3 32. Aver3ge nitrogen content of soybe3n le3ves 3n; stems at three st3e s of deve10pment 3s 3ffecte1 by t11ree levels of co plement ry 31Ur133U .3sso— ciatel witn five levels of ca lci1n............... So 33. Average phosphorus content of soybe3n le3ves 3n; stems at three st3 es of 1evelOpment as affected by t1ree levels of com.3le;'1ent3ry nutrients.3sso 018.1381 \fitil five le‘fels Of CCU Clcjlllooooooooooooooo KO 0 34. Aversge rotessic.1 content of soyoe3n leo 3ve 3 stems 3t tnree stsges of eevelopme;1t 33 3f133t33 by tnree levels of complementary nttrie1ts esso- ciatei with five levels of calcium............... lOO C3lciur11 content of soybe 3n leave Lu U1 0 k. V “ver3;3 3 3nd stens 3t t1ree stjges of develor tnez1t 33 effecte; by tnree levels of ““lenenU3rJ nUJrients 3sso— ci3t31 with five levels of calcium............... 101 35. Aver3ge magnesium COLtent of soybe3n leeves 3n; stems 3t tnree stages of levelos e1t as 3ff33U31 by Unree l vels of completenU1rJ n11trie1ts asso- 01.23.7391 \flt: fiV-e lGVGlS Of 01110.1: $11.00 0000000 00000 1.02 37. Average tot3l s 53r 3n; 3nino nitro en com1 3nt of soybe3n lesves 3‘.r11 stems (1101311n st393) 33 3ffect31 by tnree levels of connlenUnU3°J n1Uri— ents associate; witn five levels of 3lciam...... 103 r1 . » .1 -1. 30. ‘ver3ge 3011 test res1lts 3s 3ffeCt31 by tnree levels of conolel ntar nutrients 3ssociste1 with Live levels 0.1. 1:10. k#316511)..-11oo00:50:30030300000003011ch ll]- 39. Aver3ge 13 f 3n; stem yielns of sogbe3: s at tnree stages of 13v0103nenU 33 flche by t13ee levels of com lementsr’ HL rients associate1 wit1 Iive le‘fels Of 111:1,“HQSiLm1:ooooooooooooooooooooooooooooo 112 I ‘f’ .1 L r—B 40. 41. 420 43° 44. 45° ILST or LLsijs (Conn inu eQ) P1133 Average soyoea: seed yiele as affectei by three levels of complements ry nutrients asso- ciateQ with five levels of ma3nesiamo..oo..o.oo.. ll3 Average nitro 03en content of sogbea - leaves and stems at tAree sta3 es of QevelopHLe t as affects; by three levels of comp rleme ntary qaLrieLLs asso— ciated with five lev Lls of ma aesiwa...°......... ll4 Avera3e phosphorus cor L eLt of leaves anQ ster Ls at taree sta 3es of development as affecte; by taree levels of complemer tary natrient associatel 3;:; five levels of ma3nesium......................... 115 l .n.‘ Average potassiam content of leaves anQ Ste s at taree sta3es of Qevelop 1“ ant as affecte; Ly Lm ee three levels of 0013.:fl eie LLorJ nutrients as so— ciatea with five levels of LL31 sium............i ll6 Avera3e calcium content of lea es anQ stems at three sta3es of aevelopment as affecteQ by three levels of complement; try nutrients associatel wits levels Of InacglieSJ—J—iiiooooooooooooooooooooooooooooou ll? Avera3e ma3nesiam content of le elves aLiQ stezrs at three sta3es of leveloouclt as affeCLel oy “wires levels of comilementary naLrieaLs associate; A wits five levels of ma3> resiam.....oo..........oo. llb Average total sa3ar ans amino nitr03en contents OI soyoe an leaves anQ stezns (flows rin3 sta3 ) as affecteQ oy three levels of comple Wielldar3 nutri- ents associates with five levels of ma331esiam...o ll9 xi 3'. IJUXKLIJCTIGIT It is wiaely recognized that the response of soybeans to direct fertilization is inconsistent. Tne average yielu in the United States ducing the last 20 years shows little change. This is significant because other crops, especially corn, nave shown a remarkable increase in yield per acre. A linear regression analysis, for the 1939—1959 periou, indi- cates that corn yields increaseu one bushel per acre per year, while soybeans increased only one—fourth bushel for the same periou (72). As pointed out by Howell (45) and Onlrogge (72) con- siderable study has been carried out in soybean nutrition with respect to growth, dry matter production, yield, and uptake of nutrients. However, much less infocmation is avail- able relative to interactions between applieu fertilizers, F?) native soil nutrients, an& the root system characteristics 0 soybeans. Tnere is very little in the literature on tne effects of wiuely varying nutrient levels on the uevelOpment of tne soybean plant, especially Where the levels resultei in a physiologic unbalance and a growtn depression. Where nutrient level studies were conuucteu, the uata collectei were largely confined to absorption of mineral elements, anu except for isolated greenhouse experiments, the nutrient levels were relatively low. nitrogen applications seluom exceeueu lOO pounus per acre (56, 70, an& 100). Similarly, l 2 phosphate anu potash additions to mineral soils generally fell in the range of 50 to 200 pounus of P205 or K20 per acre. It is generally recognizeu by agronomists anu plant physiologists that high levels in a growth medium of any single nutrient may depress the uptake of other nutrients. This in turn may upset the physiological process of assimi- lation, metabolism, anu floral initiation (52). Accumulation of carbohydrates, proteins, and other organic constituents "y W t may oe urastically altered. As a result, they may be in direct contrast to a more balanced nutrient environment (64). Thus, the many instances of ionic interactions and antagonism that may be possible are great (55, 86, anu 9l). The purpose of this investigation was to study the effects of wiue variations in soil nutrient content upon the chemical composition of soybeans grown unuer the complex variable environment of fielu conuitions. Kore specifically, the research was designed to ueterm‘ne the infl‘ence of nitro— gen, phosphorus, potassium, calcium, and magnesium singly and in combination on the ury matter production anu the yielu of soybeans. A further anu more funuanental objective was to determine certain basic relationships which are operative in establishing variations in plant composition so that the result might be of value in interpreting data ron similar studies in the future. * 'r-N-r‘v "" :12. .L. 4 ‘W CF LITERATURE E Literature dealing with the effect of chemical fer- tilizers upon the accumulation of minecal elements and carbohydrate—nitrogen metabolism in crop plants is volumi- nous. This review, therefore, is restricted to the func— tions, interactions, accumulation, and redistribution of the elements nitrogen, phosphorus, potassium, calcium, and may- nesium in soybean plants. The review of literature is divided into six parts. The first five are related to each of the elements considered in this research, nitrogen, phosphorus, potassium, calcium, and magnesium. The sixth part deals with an no nitrogen and carbohyurate metabolism. nitrogen Differences in nitrogen content with respect to dif— ferent parts of the soybean plant at various stages of development were recognized in the early nineteenth centu y. webster (lOO) working on nitrogen metabolism of soybeans, reported that the leaves and stems, at an early stage of growth, contained as much as 8.0 per cent nitrogen. The concentration by blossom time decreased to 2.7 and 1.0 per cent, respectively, in the leaves and stems. Togari et al. (89) stated that for Japanese grown soybeans at the blooming stage, the leaves contained four times more nitrogen than the stems. Hurneek (65) observed that the leaves ani stems 4 of six-day old plants each contained about 9.0 per cent nitrogen. After 40 days of growth, these values decreased to 4.0 and 3.0, respectively, for leaves and stems. He aptly commented that the nitroge contents of leaves and stems de- creased with age. Erdman (26) working with inoculated soy- beans grown under field conditions, found that in the early stages, there was a gradual decrease in per cent nitrogen. After 95 days, the per cent nitrogen increased and usually reached a maximum at maturity. The concentration differences in the plant parts became largest in the pod—fillin; stape. Hammond et al. (34) working with a problem of nutrient uptake by soybeans on Iowa soils, observed in mature plants, that the distribution of total nitrogen was 4.0 per cent in the stems and roots, 12.0 per cent in the leaves, and 4.0 per cent in the pods and 80.0 per cent in the seed. Translocation of nitrogen from he cotyledons to the soybean seedlings is well understood. hcAllister et al. (58) concluded that the concentration of protein in the cotyledons decreased with time. At emergence time, the cotyledons con— tained 70 per cent of the protein. Nine days later they con— tained only 25 per cent. At a still later date the concen— tration dropped to 7 per cent. Yoshira et al. (106) also observed that most of the nitrogen in the cotyledons was translocated to the seedlings during the first three weeks. Hammond et a1. (34) observed that during the period from the eighty-seventh day to the one hundred thirty—fifth 5 day of maturity, the total nitrogen content of the plant in- creased 48 pounds per acre. dowever, the nitrogen content of the seed and pods increased to 121 pounds per acre. The nitrogen in the remainder of the plant decreased to 73 pounds per acre. The rate of uptake of nitrogen by a soybean plant varies with the stage of growth. Analyses made by Hammond et a1. (34) indicated that maximum absorption rate of 4.4 pounds per acre occurred during the seven—day interval be— tween 94 and 101 days after planting. Hampton et a1. (35) working with the problem of influence of variable supplies of potassium and calcium on nitrosen fixation by soybeans found that plant growth and fixation of nitrogen were affected by the addition of both potassium and calcium. higher levels of calcium stimulated nitrogen fixation to a nreater extent than potassium. Potas— sium functioned chiefly in the production of carbohydrates. The influence of calcium on nitrogen fixation was more pro- nounced at lower than at higher levels of potassium. A low rate of potassium to calcium was necessary for maximum nitrogen fixation. The need for applying nitrogenous fertilizers for higher yields is mucn debated. Investigators in Japan (106) reported that additional nitrogen, if needed, would be needed only during he first five weeks. They concluded that appli— cations of nitrogen did not increase yields. Data from the I?“ V l v investigations of Lathewell and Evans (50) showed that for maximum yields high levels of available nitrogen were neces— sary during the bloom period. The yield of beans was closely correlated with the amount of nitrogen accumulated throughout the life cycle. Allos et al. (4) studied the influence of increasing applications of available nitrogen (5—15) on growth and development. They observed that the fixation processes never supplied sufficient nitrogen for maximum growth and exhibited an apparent capacity to supply only one-half to three—fourths of the total nitrogen that could be used by the plant. The influence of seasonal variations in response of soybeans to additional nitrogen was observed by Lyons and Early (56). In 1947, which was warm and dry, marked yield responses to added nitrogen were obtained. The nrmber of nodules per plant decreased 80 to 90 per cent, but there were appreciable increases in seed yields and in the nitrogen con- tent of the seed. A year later with adequate rainfall, moderate temperatures, and 30 to 40 additional growing days, there was little to no response from added nitrogen. The number of nodules per plant on the untreated plot was larger than the previous year. The largest application of ammonium nitrate resulted in a 35 per cent decrease in the number of nodules. The investigations carried out by Hederski et al. (61) and Lyons et al. (56) indicated that the use of lower rates of nitrogen resulted in an increase of two to four bushels 7 of seed per acre, while the use of higher rates resulted in a yield depression. Phosphorus Extensive work has been completed on the utilization of phosphorus by soybeans. Phosphorus serves as a building material in the formation of nucleoproteins, flowers, and seeds. In greenhouse studies with sand cultures hederski (60) showed that soybean leaves, stems, and total tops con— tained 0.69, 0.58, 0.65 per cent phosphorus, respectively. Forty days after planting, the upper leaves contained 0.74 per cent phosphorus and the lower leaves contained 1.6 per cent. At the same time the stem contained 0.76 per cent phosphorus, while the total aerial portion contained 1.05 per cent. At blossom time the concentrations were equal to 0.74 per cent in the upper leaves, 1.64 per cent in the lower leaves, 0.67 per cent in the stems, and 1.14 per cent phos- phorus in the entire aerial portion of the plant. The per cent phosphorus for the same parts of the plant during the pod—filling stage were 0.76, 0.90, 0.53, 0.34, and 0.54. Hederski (60) reported that the concentration of phosphorus varied greatly between various parts of the soybean plant. The lower leaves acted as storaée oryans where excessive mounts of phosphorus were absorbed by the roots. In a greenhouse experiment where magnesium levels were extremely low, Webb et al. 99) found the highest per cent phosphorus in mature plants. The leaves contained 1.03 per 8 cent, the petals, 0.75 per cent, the stem, 0.96 per cent, the roots 1.32 per cent, and the pods, 1.84 per cent phosphorus. haximal concentrations of phosphorus in field grown soybeanpausually are much lower and frequently are equal to f, about one—half of those concentrations measured in nutrient solution studies. Wilkinson (104) using a band application of 40 + 160 + 0 in the field, found 0.5 per cent phosphorus in the tops of 42—day old soybean plants. The investigations carried out in the field by Borst et a1. (10) in Ohio, Welch et al. (102) in dorth Carolina, hammond et a1. (34) in Iowa, Bureau et a1. (15) in Ohio, and Togari et al. (89) in Japan, revealed that the most general range of concentration of phosphorus in soybean tops at the prebloom stage was between 0.25 and 0.30 per cent. From fertilizer tests with soybeans in Kichigan, Austin (6) reported the highest value of 0.3 per cent phosphorus in the total tops of 73—day old plants. Studies made by Merdeshi (60) with solution culture experiments, indicated that minimal concentrations in the pre- bloom stage were 0.30, 0.15, and 0.25 per cent phosphorus for the leaves, stems, and total tops, respectively. Phos— phorus concentrations decreased to ‘07 per cent in the upper leaves, 0.06 in the lower leaves, 0.03 in stems, 0.07 in the pods, and 0.05 in the total tops of soybeans at the mature stage. hederski concluded that these would represent minimum values. Kinimal concentrations in field-grown soybeans may be 9 much lower. Bureau et al. (l5) stated that with phosphorus deficient field—grown soybeans the concentration of phos— phorus in the total tops uuring the prebloom stage was often less than 0.02 per cent. hatrone et al. (57) reported that at the blossom bud stage of field—grown soybeans the phos- phorus concentrations ranged from 0.06 to 0.08 per cent in the stems and from 0.16 to 0.18 per cent in the leaves of plants grown on the "minus phosphate" plots. Ohlrogge (72) in his article, "mineral Nutrition of Soybeans" made a review of the cardinal concentrations of phosphorus in soybean plants. He stateu, "Examination of numerous data suggests an optimum range for the total tops of between 0.25 and 0.45 per cent phosphorus for the prebloom stages. Higher concentrations would represent accumulations resulting from other factors limiting growth, and lower con— centrations would represent inadequate phosphorus supplies or interference in phosphorus absorption." Ohlrogge (72) indicated that the most common concentrations reported at the bloom stage for soybeans grown on fertile soil was about 0.25 per cent phosphorus. He commented, "Consideration of all of the reported values indicates that concentrations be- tween 0.25 and 0.35 per cent represent Optimal nutrition, with values found above or below representing luxury con— sumption and deficiencies, respectively." Further, the critical concentrations for the tops exclusive of the seeds for mature soybeans, were 0.05 minimum, 0.25 to 0.35 optimum, '_ - ~- w Aug y-g-g-‘M _ _ .yq. _.._.— ..—_ wu- _.~..-.— . 10 and 0.60 maximum (72). The mobility of phosphorus in the plant was recognized early in the mid—1920's. Though Borst et al. (10) observed a decline in phosphorus concentration in leaves, stems, and pods of soybeans at the mature stage, they indicated that phosphorus moved only from the pod into the seed. hcAllister et al. (58) reported that at emergence, 40 per cent of the phosphorus had translocated to the seedling from the cotyle— dons within the first 15 days. After 38 dayS, 75 to 90 per cent had migrated into the plant. A greenhouse study by Chlrogge (72) indicated that low levels of mineral nutrition were correlated with early yellowing of the cotyledons, while high fertility levels delayed the yellowing. Investigations carried out by hederski (60), Hammond et al. (34), Topari et al. (89) clearly indicated that 40 to 75 per cent of the phOSphorus in the seed translocated from the pods, leaves, and stems. Hammond et al. (34) observed that the largest migration took place at low soil phosphorus levels. From an investigation on the effect of magnesium from phosphorus absorption and translocation in soybeans, Webb et al. (99 stated, "Omission of magnesium from nutrient solutions did not retard phosphorus absorption, but did have a significant effect upon the movement and final location of phosphorus in the plants. The chemical composition of the component parts revealed that magnesium deficient plants contained a higher percentage of phosphorus in the vegetative organs and a lower 11 percentage in the seeds than in normal plants. A definite positive relationship existed between the magnesium and phos— phorus content of the seed and a definite negative relation- ship between the content of these two elements in the leaflets. This finding offers support to the theory that magnesium acts as a carrier of phosphorus." A different picture of phosphorus uptake by soybeans exists between field and nutrient culture experiments. The findings of hedershi (60) suggested an increased rate of up- take up to 50 days from planting and then a fairly constant rate until the leaves became yellow. Field experiments by Welch et al. (102), Hammond et a1. (34), Bureau (15), and Wilkinson (104) demonstrated that a constantly increasing rate of phosphorus uptake occurred after the initial seedling lag and that a maximum rate of uptake of 0.40 pounds of phos— phorus per day occurred during the pod filling stage. hammond et a1. (34) stated that the increasing rate of phosphorus uptake was a result of higher demands by the seeds. With the advent of P32, the contribution of fertilizer phosphorus could be easily estimated. however, the problem of not being able to consistently increase soybean seed yields with the application of phosphorus even on soils known to be low in available phosphorus still remains. Colwell (18) in 1944 and helson et al. (67) in 1947, reported that soybeans responded to applications of phos— phorus on many soils in the southeastern part of the United 12 States. The magnitude of yield increase was related to the level of available phosphorus in the soil. From a study on the utilization of fertilizer and soil phosphorus, using radioactive tracer techniques, Welch et al. (102) observed that the percentage of phOSphorus derived from fertilizer was inversely related to the level of soil phosphorus and di- rectly related to the rate of application. The total u~take was greater from high phosphorus soils. E-rly absorption of phosphorus was much higher when phosphorus was placed in bands than when it was broadcast and dished into the soil. Phos- phorus applied to a previous crop was available to soybea.s which were grown as a second crop. Increased production of dry matter, and in some instances of seed, was brought about by applications of phosphorus. Krantz et al. (49) also found similar results. Kuch of the applied phosphorus was utilized in the later stages of growth. Bureau et al. (15) from a study involving the use of P32, made the following conclusions: "The phosphorus content of the plant was found to increase with an increase in the level of soil phosphorus and with the application of phos— phatic fertilizers. The residual phosphate level appeared to influence the phosphorus content of the plant to a greater degree than did the application of phospnatic fertilizers. An increase in the level of soil phosphorus tended to produce larger quantities of dry matter, but showed an apparent de- pressing effect upon soybean yields." 13 Wilkinson et a . (104) in 1957 and 1958 noticed a con— C’ sistent decline in the per cent of iertilizer derived phos— .1. U E: of yrowth. ’here was no Q (D phorus taken up during each s a; sipnificant increase in seed yields, although a significant early response in dry weight and total phosphorus content of plants was obtained. On reviewing the effect of phosphorus fertilizers on soybean yields and growth characteristics, Ohlrogpe (72) aptly commented, "Certainly, a large part of the phosphorus can be derived from the fertilizer. Also, the total uptake of phosphorus may be and frequently is increased somewhat. There is, however, no assurance of an increase in yield. Thus, phosphorus does not appear to provide the exclusive key to unlocking the soybean mystery." Potassium There has been a great amount of research both in the field and in the greenhouse on the role that potassium plays in the nutrition of soybeans. From a greenhouse study hutchings (46) reported that the total tOps of soybeans at the prebloom stage contained as high as 5.70 per cent potassium. A study of the effect of varying concentrations in a nutrient medium led Allen (3) to report that total tops of the Virginia and horse variety at the prebloom stage contained 2.7 and 3.5 per cent potas- sium. Evans et al. (27) observed a wide range of potassium concentrations in different parts of a flowering soybean 14 plant grown in sand cultures. The maximum concentration was 1.75 per cent potassium in the upper leaves. When the nutri— ent solution contained no magnesium the upper and lower leaves of soybean plants grown on complete solutions con— tained 0.84 and 0.60 per cent potassium, respectively. Field studies carried out in Japan by Togari et al. (89) indicated that stems and leaves of soybeans at the pre- bloom stage contained more than 4.0 and 2.5 per cent potas— sium, respectively. At the onset of blooms, the total con- centration of the top varied from 2.0 to 3.5 per cent potas— sium. Hammond et al. (34) reported a range between 1.0 and 1.5 per cent potassium in total tops at the prebloom stape. In the bloom stage the potassium concentration of the total tops ranged from 0.80 to 1.0 per cent while in the pod—filling stage the concentrations were between 0.5 and 0.7 per cent. Borst and Thatcher (10) after six years' investigation found that at the prebloom stage the leaves and stems contained 2.3 and 3.6 per cent potassium respectively. At the bloom stage total potassium concentration ranged between 0.9 and 1.2 per cent for the total tops. In the pod—filling stage the leaves declined from 1.0 per cent to 0.3 per cent, while the stem decreased from 0.8 to 0.3 per cent. They stated that the leaves and stems decreased in per cent potassium as the plants approached maturity. From a nutrient culture experiment, Allen (3) reported a minimal concentration of 0.3 per cent potassium in the tops 15 of plants at the prebloom stage. Evans et al. (27) reported a minimum.of 0.18 per cent potassium in the lower leaves of soybeans at the blooming stage when plants were grown in solutions with toxic levels of magnesium. From a field study in Kichigan, Austin (6) found that total tops of 35—day old plants contained 0.5 per cent potassium. Ohlrogge (72) reviewed the cardinal concentrations of potassium in soybean plants. He stated that the data for the prebloom stage would suggest a minimum of 0.3 per cent, optimum range 1 to 4.0 and an upper limit of 5.7 per cent potassium for the total tOps. For the blooming stage minimal optimal and maximum concentration in the tOps of 0.3, 0.7 to 2.0, and 4.5 per cent potassium were su tested. During pod— filling stage the potassium in the stems ranged from over 3.0 to less than 0.3 per cent. The leaves ranged from 0.4 to 3.0 per cent and the pods from 0.8 to 3.0 per cent potas— sium. The concentration of potassium at the onset of foliar deficiency symptoms was reported by Ielson et a1. (66) from field experiments in fiorth Carolina on a Coxville very fine sandy loam soil which was low in exchangeable potassium. The potassium content of the blade and petiole of leaves which showed foliar deficiency symptoms were 0.48 and 0.7 per cent. The levels in the normal leaves from the plots that received 120 pounds per acre of K20 were 2.1 and 1.6 per cent in the blade and petiole respectively. 16 The influences of cations upon the absorption of other cations represents a very complex phenomenon. hany plant cation relationships have been proposed. Evans et a1. (27) observed that a deficiency of potassirm in the nutrient so— lutions caused a decrease in potassium. A deficiency of mag— nesium increased the potassium conten of soybean leaves twofold, whereas magnesium in toxic amounts caused the potas- sium contents of the leaves to decrease to near trace levels. A deficiency of phosphorus had a marked effect on increasing the potassium content of the leaves. Allen (3) noticed that with increasing supplies of calcium in the nutrient medium there was an increasing percentage of calcium and a de— creasing percentage of potassium in the foliage. With an increasing supply of magnesium the per cent magnesium in— creased in the foliage and the potassium levels decreased. The phenomenon of potassium translocation has been studied in detail. hcAllister et al. (58) observed that a rapid loss of potassium from the colytedons occurred from planting until emergence. Then the rate decreased to the final level. One half of the potassium moved out of the cotyledons 15 days after planting. After 30 days, only 20 per cent of the original potassium remained in the cotyle- dons. From a nutrient free medium in a darkroom Von 0hlen (94) observed that in 25 days all of the potassium moved out of the cotyledons. Chlrogge (72) commented that the extent of translocation would probably be dependent upon the potas— l7 sium availability to the roots of the seedling. Differences with respect to rate of uptake of potas- sium by soybeans exist in the literature. Hammond et al. (34) observed a peak rate of potassium uptake of l.7 pounds per acre per day during a week period between 87 and 94 days after planting. They reported that potassium had shown more week to week variations in uptake rate than calcium, ma nesi- um, nitrogen, or phosphorus. Togari's (89) results expressed on a per plant basis showed a much more constant trend. Re- sults from six years' field experiments at Ohio by Borst and Thatcher (l0) indicated a constantly decr asing rate of up- take during the pod~filling period. Some of the most striking responses to fertilization have been obtained with potassium salts. Consistently large grain yield increases were obtained from potassium fertiliz— ers on almost all of the potassium deficient soils of the south—eastern part of the United States when good production methods were used. In the hidwest, response has not been so consistent. Most of the responses were obtained on the sandier soils and on those prairie soils high in orpanic matter. The poorly drained light colored silt loams have not responded consistently to potassium applications even when potassium deficiencies were prevalent. Both broadcast and band applications of potassium resulted in increased levels Of potassium in plants (72). From a field experiment on a sandy loam soil low in C}? l exchangeable potassium Nelson et al. (6’) made the following summary: 1. Additions of potassium more than doubled the number of pods per plant of each variety, exerted a beneficial in— fluence in retaining pods until harvest, resulted in an in— crease in the number of two—cavity sized pods and a decrease in the number of three—cavity sized pods. A significant influence was that of increasing the degree of filling. 2. Potassium marked y improved the seed quality by reducing the number of shriveled, shrunken, moldy, and off— colored seeds. 3. haturity was retarded by additions of potassium. 4. Potassium increased seed weight of all varieties and the oil conten of the seeds of two varieties out of three. 5. As an average of all varieties the addition of 60 pounds of K20 increased the yield fourfold. Calcium The beneficial effects of adequate quantities of calci‘n upon the structure of the soil, microbial activity, and the availability of other essential nutrients has been known for some time. The effect of various calcium levels upon soybean growth characteristics, however, is complex. The investigations of harston et al. (37), hampton et al. (35), Allen (3), Graham et al. (30) and Brown et al. (14) with clay and sand cultures indicated that the calcium con- 19 tent of the total soybean plant at the prebloom stage ranged between 0.25 and 0.75 per cent. Siegel (84) reported a range of 0.7 to 1.25 per cent calcium in soybeans that were grown in nutrient solutions. At the prebloom stage Evans et a1. (27) observed that the calcium concentration in the leaves of nutrient solution grown beans varied from near 0 to 6.5 per cent. The lower leaves contained 5.0 per cent while the upper leaves con— tained only 1.0 per cent. Studies in Japan by Hashimoto (40) showed that ranges in calcium content of the leaves and stems were between 0.5 and 1.5 and 0.3 and 1.14 per cent re— spectively. During the pod—filling staée as reported by Hashimoto (40) the leaves ranged between 2.0 and 2.4 and the stems between 0.7 and l.6 per cent calcium. Field studies by Austin (6) showed that the calcium concentration of the total tops of soybean plants after 30 days from planting varied between 2.0 and 2.75. Hammond et a1. (34) recorded concentrations of 1.9 and 1.25 per cent calcium in the total plant 22 and 55 days respectively after planting. In the study of Hashimoto et al. (41) the calcium concentrations ranged from 2.3 to 2.6 and 1.6 to 1.9 per cent in the leaves and stems of soybean plants at the preblossom stage. Wilkinson (104) reported that at the onset of flowers the calcium concentration of soybean tops varied from 0.5 to slightly higher than 1.0 per cent. Austin's (6) 73-day old plants ranged between l.7 and 2.0 per cent calcium. hashimoto 20 et al. (42) reported a range of between 2.2 and 3.3, and 1.5 and 1.9 per cent calcium, respectively for leaves and stems at the blooming stage. In the pod-filling stage, Austin (6) found a range of between 1.2 and 2.0 per cent. Wilkinson (104) from a nutritional survey of farmers' fields found a range of between 0.9 and 4.5 per cent calcium. Ohlrogge (72) stated, "Here again, as is true for many other nutrients, the widest range in calcium content is found in the youngest plants." The effect of complementary nutrients on the uptake of calcium has been studied. Evans et a1. (27) noticed that a deficiency of potass um in a nutrient solution caused an in- crease in the uptake of calcium. Deficiencies of magnesium did not produce any change in the calcium concentration in the leaves whereas toxic quantities of magnesium caused the cal— cium content to decrease to a mere trace amount. Graham et al. (31) observed that the use of magnesium resulted in an increase in the uptake of calcium. Allen (3) found that an inverse relationship existed between the percent of potassium and calcium in the foliage, and with an increasing supply of magnesium there was little change in the calcium concentra- tions. Translocation of calcium from cotyledons is almost absent. The investigation carried out by hcAllister et al. (58) led to the conclusion that the calcium content did not change appreciably during seed germination. However, during 21 the 20 days after emergence, the calcium content of the coty— ledons increased 300 per cent. The only discussion found on the rate of uptake was that made by hammond et a1. (34). He observed that the rate gradually increased, reaching a peak of 2.8 pounds of calcium per day for a week interval between 73 and 80 days after planting. The immobility of calcium in soybean plants as stated by Ohlrogge (72) is well recognized. "This immobility lends increasing importance to gaining a complete understanding of the day-to—day requirements of the plant. The abundance and low cost of calcium has apparently discouraged research in calcium nutrition, but this does not preclude the possibility of a vital role for it as a factor limiting yields of soybean." 0h1rogge (72) further commented, "Soybeans at low yield levels are unusually tolerant to soil acidity but do respond markedly to lime applications. A constant supply of calcium is required by the plant because of its immobility in the soybean. There are many other positive effects of limin;, in addition to making calcium available to the plant. Since liming is a widespread practice on acid soil areas of the soybean belt, little work has been done to evaluate calcium as a nutrient in field soils." Kagnesium Numerous greenhouse and field experiments have been designed to solve the mystery of the soybean yield plateau. Some of the research involved evaluations of the role of 22 magnesium in the nutrition of soybeans. From a nutrient culture study Allen (3) reported a range of 0.09 to l.5 per cent magnesium in the leaves at the prebloom stage. Webb et al. (99) reported that at the onset of blooms the concentrations of magnesium in the total tops varied between 0.08 and 0.63 per cent. During the pod-filling stage Hashimoto (39) observed an equal concen ration range for maénesium in the stems and leaves. The range varied be— tween 0.2 and 0.6 per cent. The distribution and range of magnesium concentration in mature plants were evaluated by Webb et al. (99). They found that leaves varied between 0.05 and 0.68 per cent mapnesium. Petioles varied between 0.03 and 0.56 per cent. The stems varied between 0.2 and 0.45 per cent. The roots varied between 0.06 and 0.53 per cent. The pods varied between 0.05 and 0.88 per cent. The seeds varied between 0.14 and 0.36 per cent and the whole plant varied between 0.06 and 0.53 per cent maénesium. The field investigations of Austin (6) and jammonl et al. (34) showed a range of 0.27 and 0.80 per cent mapnesium in the total tops of the soybeans at the prebloom stage. The highest concentration was l.0 per cent magnesium in the tops Of 73-day old plants (6). The effect of complementary nutrients on the uptake of magnesium by soybeans has been noted. Studies on the chemi— cal composition of soybeans grown under various nutrient con— ditions by Evans et al. (27) indicated that a deficiency of 23 calcium in nutrient solutions caused an increase in the up— take of maénesium while increases in calcium in the nutrient solution apparently did not effect the magnesium uptake. Allen (3) noticed that with an increasing supply of calcium in the nutrient solution there was a decreasing percentage of mag— nesium in the foliage and also an inverse relationship be— tween the percentages of potassium and r ghesium. The content of m~5nesium associated with the onset of foliar deficiency symptoms was reported by a number of inves— tigators. Webb et al. (99) observed a concentration of 0.09 per cent magnesium in the tops of soybean plants which showed I magnesium deficiency symptoms at the prebloom stage. Hashimoto (39) suggested that at the onset of foliar deficiency symptoms field grown soybean plants contained 0.10 per cent magnesium. Webb et al. (99) further suggested that the onset of defi- ciency symptoms in the leaves of flowerin; plants was associ- ated with a magnesium concentration of 0.25 per cent for all of the leaves of the plant. The leaves of the normal plant had a concentration of more than 0.3 per cent mapnesium. The translocation of magnesium from cotyledons is mucn less than for nitrogen, phosphorus, and potassium. McAllister et al. (58) observed that from germination to emergency only one-fourth of the magnesium moved out of the cotyledons. This was in contrast with almost complete removal of potas— sium and phosphorus and no removal of calcium. Again, like calcium the cotyledons gained magnesium from the 28th to the 24 37th day, but the magnitVde was much lower than for calci‘m. hammond et al. (34) noticed a gradual increase in the uptake of magnesium which reached a maximum absorption rate of 1.5 pounds per acre per day during the interval of 37 to 80 days after planting. Data from the nutrient culture experiment of Webb et al. (99) indicated a peak uptake of five milligrams per plant per day for a five-day period between the 65th and 70th day after plantins. From a study of chelated,exchanpeable and readily sol— uble magnesium as factors in the nutrition of soybeans Graham et al. (31) concluded that on ll of the 15 soils yield increases occurred when magnesium was added to the soil. The highest correlation between the amount of m gnesium shown by soil tests and per cent increase in crop yield was obtained when the soil was extracted with 0.05 normal hvdrochloric acid. In general, the soils with less than 10 per cent ma;— nesium sa uration of the total exchange capacity were the ones where yield responses to the nutrient were obtained. This fact re-enforced the suggestion that the 10 per cent level would be a helpful guide when attempting to determine a desirable magnesium level in the soil. Kelson et al. (66) obtained an increase of seven bushels per acre by the use of 36 pounds of magnesium oxide per acre on a soil low in exchangeable magnesium. 25 _ .r, 4_ . A 1 h A _ N. . - Amino nitrogen and carbonyirate nethOllSJ There are not as many publications on amino nitrogen and carbohydrate metabolism in soybeans as there are on direct utilization of mineral ele-e1 s by this crop. There— fore, this section include s comments on research completed on other crops as well as soybeans. Scruti (79) determined that phosphorus played an impor- tant role in the formation of amino acids. In studying the effects of various mineral deficien— cies on nitrogen metabolism, Burrell (16) observed that the leaves and stems of maynesium deficient plants contained smaller amounts of star01 a1d insoluble nitro en as well as lar er quantities of soluble nitrogen than did the leaves and stems of the control plants. With potassium Lefici we t plants, he ooserved that the leaves accg‘ uleted StQPC‘ amino nitrogen was usually hiyh. is concluded, ”Potassimn seerms‘to flnictiryi irl the inminslrxnati041zaud ..urli4‘antass jinn: l. Potass um appears to be directly or indirectly - —v essential for carbon dioxide assinilation anu therefore 26 Concentratiornscxf carsoiyurates may be low in potassium deficient pla.;ts. 22. Carbohydrates frequently'accumulate in pctassium deficient plants apparently becadse tne rate or nitrate assi1nilzj tion is retarded. 3. Potassium appears to be directly or indirectly esseerLLl for ‘tne idriti:-:J_:3ta;e i111ritrate IYHEACCiOflJ 4. Potassium 's directly essentie l for tne synthesis of protein in tne rerist 1iati c ti- Q SL8. U} Janssen et al. (47) working witn cowpeas grown in nu- gorted t11L1b 111: ts grown witl low levels 7 I .L J. ‘ . _ I trient solutions r' (D ‘1‘: r- 1— J, - . ‘2 '1 P“ '-‘ r1 '~ ‘ r r“ V' ' - 1" of‘jpotnissi 1-31 coi1tai;1 l1orue reWbLCiibJ s91-i‘wa‘is .1eld. as 'to All (D nfiwex C .ji—pfinel n r 139 . 1 71' .L" d *0 (vi—1.1111" U»; ’J Oil bL-‘aphJ-L \A. “3 AC]: L‘ 'notassioa13n1 ale leaves ana steix.oi soybeans. An anuc“o1istic relationsnip between -‘- —: - -, -;- H. n Aa‘n‘ ~ ~ 9 "‘ potassiia ans ma esian was observea. Zne ass of m onesi in n3im10 cine nan a ocneral eliect . - , . ‘ .,‘ q. -t- a .1- - .0 .1.‘ .3. of increasinQ total saw: a“ conte ts cl bJe leaves ana stexms. CO o 10. 11. 12. "T .'.1 ‘1 r13 r171“ .LJA. lgi'lilulufi v.1. .41) Albrecht, Em. A. Sone Soil Factors in nitro; ” ation by 1e3unes. Tram1 . Tnira Com. Int 1 Soc. Soil Sci. Azfl-o4. 1939 . Potassiun in tne soil colloil con- plex ani plant nutrition. Soil Sci. 55:13—21. 1943. Allen, D. I. s111e°e1tia1 “cowun response of certain varieties of soyoeans to var ea mineral nutrient conaitions. Iissonri A3r. Ei3. Sta. Researcn Sal. 361. 1943. Allos, A. 3., ani Bartnolonew, W. V. Replacement of symbiotic fixation b3 availaole nitrogen. Soil Sci. 87:6l*66o 1959 Arnon, 3. I. The pn3 1010‘ ani oioc1er. Sb try of phos— pnorus in green plants. rono.3 4:1—44. 953. Austin, R. H. Efie cts of soil type anl 'ertilizer treatment on the composition of soybean plant. Jr. Amer. Soc. Agon. 2:136—156. 1930. Bass 11am, J. A., Benson, A. A., Ka3 ,L.3., Larris, A. Z., Jilson, A. T., an' O alvin, n. 1ne pa‘n of car son in pflOtOOVltueSlo. ine C3clic regeneration of tne carbon lioxile acceptor. Jr. Amer. Cnem. Soc. 76:1760—177 . 1954. Lenson, A. A., an; Calvin, n. Carbon i tion by 3ree11 plants Ann. Rev. Pla;1 1:25—42. 19 50. o: iie fixa- t P1ysiold Beeson, K. C. The effect mi1erL11 svpply on tne mineral concentration ans nitritione a.1 qaality of plants. Eot. Rev. 12: 424-155. 1946. 3 1 st, H. L., and Thatcher, L. E. Life history ani composition of the soybean plant. 0110 A3ric. Exp. 31.1.10 4'94. .1931. Loynton, 3., and Barrel, A. 3. Potassium inimcei ma3nesinm deficiency in tne ficlntosn Apple tree. Soil Sci. 58:441-454. 1944. Bray, R. 5., ana Kurtz, L. T. Determinatinn of total, organic anl available forms of phosphoras in soils. Soil Sci. 59:39—45. 1945. 127 16. 20. 21. 23. 24. Lrooks, S. C. Tne accanIlatIon of Ions I llVlA“ cells. Protoplasma. 8:369—412. 1929. ' grown, I). A., an; Albrecnt, ’.’.";11. A. Pl ant natrition ana ny1ro3en ion. Calcium Car oonat ' ' fertility factor in soils. Soil Sci Soc. Amer. Proc. 12:342-347. 1947. Bareaa, L. 3., Keaerski, H. J., a1 E’ans, C. 3. fine effect of pIospnatic fertilizer naterial an; soil pnos pnorus level on tne yielLi. ana pnospnoraS‘aptake oy soy oea1s A3r. Jr. 45: 150—154. 1973. Dari ell, R. C. Eerct of certain neficieJCIes on nitro we'1 metabolism of plants. Lot. Caz. 62:320—323. 1926. Carolus, R. L. Effect of La3IeSII“ Aeficie1cy In t1e oil 01 tne yiela, appeaIa.ce an; conpOSItion of ve 3etaole crops. Proc. Amer. Soc. Lort. Sci. 32:610—614. 1934. 1'.- ~1 ‘3 - IL; .: ' ., -. -, . -' - ’ 1.1;. I.“ I' .1, Colzell, u. I. xertIlIZIn3 so3 sea:.s II Ior'- CanlIna. 1 - rw ' O J' - ("""‘L -1‘,‘ '\ 5 P setter Ciops Vita plant IooI. 269 26(6 Cooil, 3. J., an1 Slattery, L. C. Effects of potas— siur1inafiiciency’zILi excess upor1cm23:311 caroo131rate ana nitr03enous constituents of 33a.11e. Plant Pnysiol. 23:425-439. 1948. J. o 1. ~11 A .4, 7‘13, ‘1,]_ ( l ...1‘, :- 1.1.1 CIl . AQLA 0 $11.1) . b L13 0 55580 9 -Jv-l O 3 )3 Cook, L. L., an1 Lillar, C. 3. Plan ' 'es. (revisei). 1953. Stake, L., Ven3ris, J., an; Colby, U. G. Cation ex— cnan3e capacity of p1a1t roots. Soil Sci. 72:139—148. 1951. Lrosloff , L., ani I arpass, 51 G. Qaantitative micro aeter:1i;1ation of ma3ncsIU plaI' tissues ana soil extrIa cts. Analytical C‘““l tr3. 20:673-674. 1946. .Dancan, 3. 3. 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