USGA GREEN SECTION RECORD A Publication on Turf Management by the United States Golf Association USGA GREEN SECTION RECORD A Publication on Turf Management by the United States Golf Association © 1972 by United States Golf Association. Permission to reproduce articles or material in the USGA GREEN SECTION RECORD is granted to publishers of newspapers and periodicals (unless specifically noted otherwise), provided credit is given the USGA and copyright protection is afforded. To reprint material in other media, written permission must be obtained from the USGA. In any case, neither articles nor other material may be copied or used for any advertising, promotion or commercial purposes. VOL. 10, NO. 6 NOVEMBER 1972 Potassium, Calcium, Magnesium — How They Relate to Plant Growth by Carl Schwartzkopf............................................................................................... 1 Ten Years of Research on Winter Injury on Golf Courses: Causes and Prevention by Dr. James B. Beard............................................................................................... 3 Turfgrass Management in the Argentine by James B. Moncrief............................................................................................... 9 A Golf Superintendent should be A Golf Superintendent by Paul N. Voykin .................................................................................................... 12 Turf Twisters Back Cover Published six times a year in January, March, May, July, September and November by the UNITED STATES GOLF ASSOCIATION, 40 EAST 38th ST., NEW YORK, N.Y. 10016. Subscription: $2 a year. Single copies: 35c. Subscriptions and address changes should be sent to the above address. Articles, photographs, and correspondence relevant to published material should be addressed to: United States Golf Association Green Section, P.O. Box 567, Garden Grove, Calif 92642. Second class postage paid at New York, N.Y. and other locations. Office of Publication 40 East 38th Street, New York, N.Y. 10016. Editor: William H. Bengeyfield Managing Editor: Robert Sommers Art Editor: Miss Janet Seagle Green Section Committee Chairman: Edward L. Meister, Jr., 37841 Euclid Ave., Willoughby, Ohio 44094 Green Section Agronomists and Offices EASTERN REGION P.O. Box 1237 Highland Park, N. J. 08904 Alexander M. Radko, Director, Eastern Region and National Research Director William G. Buchanan, Eastern Agronomist Stanley J. Zontek, Eastern Agronomist (201) 572-0440 SOUTHERN REGION P.O. Box 4213 Campus Station, Athens, Ga. 30601 James B. Moncrief, Director, Southern Region (404) LI 8-2741 MID-CONTINENT REGION P.O. Box 592, Crystal Lake, III. 60014 F. Lee Record, Director, Mid-Continent Region Carl Schwartzkopf, Mid-Continent Agronomist (815) 459-3731 MID-ATLANTIC REGION P.O. Box 5563 Barricks Road Station, Charlottesville, Va. 22903 Holman M. Griffin, Mid-Atlantic Director (703) 296-5353 WESTERN REGION P.O. Box 567 Garden Grove, Calif. 92642 William H. Bengeyfield, Director, Western Region and Publications Editor (714) 638-0962 Potassium, Calcium, Magnesium— How They Relate to Plant Growth by CARL SCHWARTZKOPF, Mid-Continent Agronomist, USGA Green Section Potassium, calcium and magnesium play an important role in soil-plant relationships. These elements are not only essential to the complex biochemistry of plant growth, but their pres­ ence in the soil in adequate amounts and in suitable proportions to one another and to the other exchangeable cations, such as aluminum, hydrogen and NH4+, is necessary if the soil is to be a suitable medium for plant-root development. Should one element be in excess, it may “tie-up” or make it unavailable to the plant. POTASSIUM Potassium is absorbed by plants in larger amounts than any other mineral element except nitrogen and possibly calcium. This element plays an important part in many of the vital physiological processes in the plant; the exact mechanism by which potassium functions is not known. It is needed for the plant cell's metabolic processes and apparently has a role in influencing the uptake of certain other mineral elements, in regulating the rate of respiration, affecting the rate of transpiration and in influencing the action of enzymes, as well as in aiding the synthesis and translocation of carbo­ hydrates. Potassium also has a counterbalancing effect on the results of a nitrogen excess. It enhances the synthesis and translocation of carbohydrates, thereby encouraging the cell walls to thicken and help the plant to remain upright. Potassium plays a vital role in the winter survival of turfgrass, disease resistance, and in increasing the overall hardiness of the grass plant. Deficiency symptoms of potassium on turfgrass are yellow-streaked leaves, followed by browning and dying at tips and margins. SOURCES OF POTASSIUM Hardwood ashes supplied much of the potassium in the United States through the first part of the 19th Century. A decline in the potash industry resulted after the hardwood forests along the Atlantic Coast were depleted. The first factory that processed KCL (murate of potash) was in Germany, and the Germans monopolized the potassium market until World War I. The embargo placed on potassium exports forced development of the resources of the United States and of other countries as well. Most potassium today comes from New Mexico, California, and Utah. CALCIUM Calcium, as potassium, is absorbed by the turfgrass plant in the ionic form. The calcium in the soil other than what was added as lime or in fertilizer material originated in the rocks and minerals from which the soil was formed. Calcium is a part of many minerals, such as Injury to turf from the misapplication of plant nutrients. NOVEMBER 1972 dolomite, calcite and calcium feldspars. Upon their disintegration and decomposition, calcium is released. Calcium is an extremely important mineral in plant nutrition. Many soils, particularly in humid regions, contain this element in amounts so small that plant growth is limited. Turf­ grasses as a group are able to tolerate low levels of calcium; however, abnormal growth has been observed with extremely low levels. One of the primary roles assigned to calcium in the plant is the key role it plays in the cell walls. Calcium is also important in root development, since short roots are observed on calcium deficient plants. The first sign of calcium deficiency in older plants is the appearance of a reddish-brown discoloration in the tissue between the veins, along the margin of the blade. The most obvious method of correcting this deficiency is by the application of calcitic or dolomitic lime. Should calcium be required without changing the pH that would result from the use of lime, gypsum may be used. Liming is the addition to the soil of any calcium-containing compound that is capable of reducing acidity. The correct use of lime refers only to calcium oxide (CaO), but the term almost universally includes such materials as calcium hydroxide, calcium carbonate, cal- cium-magnesium carbonate and calcium silicate slags. A description of various liming materials describing their availability and manufacture follows: Calcium Oxide — Calcium oxide (CaO), also known as unslaked lime, burned lime, or quicklime, is a white powder that is quite disagreeable to handle. It is manufactured by heating calcite limestone in an oven or furnace. The carbon dioxide is driven off, with calcium oxide remaining. This product is most fre­ quently handled in paper bags because of its powdery and caustic nature. This material reacts quickly when added to the soil. When unusually rapid results are desired, either calcium oxide or calcium hydroxide should be used. Calcium Hydroxide — Calcium hydroxide (Ca(OH)2) is commonly referred to as slaked lime, hydrated lime or builder’s lime. It is similar to calcium oxide in that it is a white powdery substance, difficult and unpleasant to handle. Slaked lime is prepared by the hydra­ tion of calcium oxide. A large amount of heat is generated; upon completion of the reaction, the material is dried and packaged. Calcium and Mixed Calcium-Magnesium Carbonates — The carbonates of calcium and magnesium occur widely in nature and in many different forms. Crystalline calcium carbonates are referred to as calcite or calcitic limestone. Crystalline calcium-magnesium is known com­ monly as dolomite. MAGNESIUM Magnesium is also absorbed by plants in the ionic forms. This absorption takes place from the soil solution or possibly by contact exchange. Magnesium plays a vital role in photosyn­ thesis, as it is. the central atom in the chlorophyll molecule. It is involved in many enzyme reactions. It reacts with phosphorus in uptake and transport. Magnesium is also quite mobile in the plant, and yellow deficiency symptoms first appear on the older leaves, as it moves to the younger plants. SOURCE OF MAGNESIUM Magnesium in the soil originates in the decomposition of rocks containing minerals such as brotite, dolomite and olivine. Upon decomposition, these minerals set magnesium into the surrounding soil solution. Once in the soil solution, magnesium may be 1) leached, 2) absorbed by living organisms, and 3) adsorbed by surrounding particles. MAGNESIUM IN THE SOIL The coarse-textured soils of the humid region are those in which a magnesium defi­ ciency is generally manifested. These soil types usually contain small amounts of exchangeable magnesium. This condition is aggravated by the addition of large quantities of fertilizer salts which contain little or no magnesium. The magnesium in the soil is released by ion exchange when these fertilizers are added; the larger quantities of chlorides and sulphates speeds its removal by leaching. Magnesium can be supplied in dolomitic limestone, or as magnesium sulphate, if soil pH is to remain the same. A deficiency of magnesium is less of a problem on finer-textured soils and on soils found in the arid regions. In some semi-arid locations, magnesium compounds may actually be precipitated in the soil profile. When the appearance of a plant and environmental factors indicate a nutritional disorder, steps should be taken to verify the problem before attempting to correct it hap­ hazardly with nutrients that are not needed. Since nutrient deficiencies on turfgrasses are difficult to visually diagnose, a suspected deficiency should be verified with soil or tissue tests before trying to correct the problem. A most important criterion for a soil test is that it should measure the nutrient in the soil that is available to the plant. Many times nutrients in the soil are held tightly and are unavailable. 2 USGA GREEN SECTION RECORD Complete kill of the leaves, crowns, and rhizomes of a Kentucky bluegrass turf resulting from a 160-pound man shuffling uniformly over the wet, slushy area just prior to a severe freeze to below 20°F. Ten Years of Research on Winter Injury on Golf Courses: Causes and Prevention by DR. JAMES B. BEARD, Michigan State University VVnter injury of turf is difficult to under­ stand because it results from the interaction of a number of environmental, soil, and cultural factors. Before a golf course superintendent can initiate the appropriate cultural program to prevent winter injury, he must determine the particular type or types of winter injury that occur most frequently at various locations on the golf course. This involves a study of the particular symptoms, including time of occur­ rence, soil type, topography, drainage charac­ teristics, traffic patterns, and the probability of environmental stress. Such information is as­ sembled over a period of years, and a specific program is established on the golf course in order to minimize the probability of winter injury. CAUSES OF WINTER INJURY The four major types of turfgrass winter injury that most commonly occur are presented in Table 1, along with the symptoms and causes of injury. This information has been assembled over a 10-year period of extensive research at Michigan State University. The major types of winter injury are: Desiccation Direct low temperature kill Low temperature diseases Traffic effects. Note that ice sheet damage caused by oxygen suffocation or toxic gas accumulations underneath an ice cover are not listed. Detailed investigations at Michigan State . University indicate that this type of winter injury rarely occurs. This is in contrast to the many articles by individuals indicating that this is a serious problem. Unfortunately, these earlier writers had essentially no information on which to base their comments other than data from research with alfalfa. The winter injury most commonly associated with extended periods of ice cover­ age occurs during freezing or thawing periods when standing water increases the crown tissue hydration and subsequent injury of the turf­ grass plants when temperatures drop rapidly below 20°F. NOVEMBER 1972 3 f r u t e s r u o c f l o g n o r u c c o y l n o m m o c t s o m t a h t y r u j n i r e t n i w f o s e s u a c d n a , s m o t p m y s , s e p y T . 1 e l b a T 4 USGA GREEN SECTION RECORD