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Potential for Natural Zeolite Uses on Golf Courses - Zeolite Products

Potential for Natural Zeolite Uses on Golf Courses - Zeolite Products

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RESEARCH UPDATE:<str<strong>on</strong>g>Potential</str<strong>on</strong>g> <str<strong>on</strong>g>for</str<strong>on</strong>g> <str<strong>on</strong>g>Natural</str<strong>on</strong>g> <str<strong>on</strong>g>Zeolite</str<strong>on</strong>g> <str<strong>on</strong>g>Uses</str<strong>on</strong>g> <strong>on</strong> <strong>Golf</strong> <strong>Courses</strong>by A. MARTIN PETROVICAssociate Professor of Turfgrass Science, Cornell University, Ithaca, New YorkTHERE ARE MANY IMPORTANTcharacteristics of a desirable turfgrassroot z<strong>on</strong>e material, namely: minimumcompacti<strong>on</strong> tendency, good water infiltrati<strong>on</strong>and percolati<strong>on</strong> rates, adequate aerati<strong>on</strong> <str<strong>on</strong>g>for</str<strong>on</strong>g>deep rooting, high cati<strong>on</strong> exchange capacity(CEC), and adequate moisture retenti<strong>on</strong>.However, due to the heavy traffic that puttinggreens and tees receive, sand is themajor mix comp<strong>on</strong>ent. If properly chosen, itprovides <str<strong>on</strong>g>for</str<strong>on</strong>g> good drainage, resistance tocompacti<strong>on</strong>, and good aerati<strong>on</strong>. By itself,though, it generally lacks adequate cati<strong>on</strong>exchange capacity and water-holding capacity,and it allows excessive percolati<strong>on</strong>rates.Typically, sands are amended with some<str<strong>on</strong>g>for</str<strong>on</strong>g>m of organic matter to create a rootz<strong>on</strong>e mix, and peat is the most widely usedorganic amendment. In some situati<strong>on</strong>s,locally available organic matter sources areused. Rice hulls, sewage sludge, and lumberwaste materials are all possibilities. Theadvantages of amending sand with organicsinclude increased water retenti<strong>on</strong>, increasednutrient retenti<strong>on</strong> (cati<strong>on</strong>s), and some pesticidebinding (reduced pesticide leaching).On the down side, organic amendments decomposewith time and are of limited effectivenessin retaining nitrate from leaching.Though not routinely used, some inorganicamendments, including fIred clay, colloidalphosphate, sintered fly ash, vermiculite,perlite, and calcined clay have receivedsome attenti<strong>on</strong>. Inorganic amendments canincrease moisture retenti<strong>on</strong> to a limiteddegree, but generally do not improve nutrientretenti<strong>on</strong>. Some break down over time as aresult of weathering or traffIc. Thus, there isa need <str<strong>on</strong>g>for</str<strong>on</strong>g> an amendment that will increasewater-holding capacity and nutrient (especiallynitrogen) and pesticide retenti<strong>on</strong> whilestill remaining stable over time. A naturalzeolite like clinoptilolite may be such anamendment.<str<strong>on</strong>g>Zeolite</str<strong>on</strong>g>s are alumino-silicate minerals fIrstdiscovered in 1756 by Swedish mineralogistBar<strong>on</strong> Axel R Cr<strong>on</strong>stedt, who named theporous mineral from the Greek wordsmeaning "boiling st<strong>on</strong>es." There are morethan 40 natural zeolites, six of them in largedeposits: anacline, chabazite, clinoptilolite,eri<strong>on</strong>ite, mordenite, and phillipsite. Clinoptiloliteis of importance in agriculture becauseof its abundance and its chemicalproperties. Extensive deposits of clinoptiloliteare found in the western United States,the <str<strong>on</strong>g>for</str<strong>on</strong>g>mer Soviet Uni<strong>on</strong>, Bulgaria, Hungary,Yugoslavia, and Japan. It has a crystallinestructure with many minute internal poresthat retain water and nutrients such asamm<strong>on</strong>ium and potassium. It has a very highcati<strong>on</strong> exchange capacity (from 100 to 230cmol/kg). The pores are large enough toallow cati<strong>on</strong>s to pass in and out, but are toosmall <str<strong>on</strong>g>for</str<strong>on</strong>g> bacteria, especially bacteria thatc<strong>on</strong>vert amm<strong>on</strong>ium to nitrate. Water andnutrients held in the pores remain available.Thus, clinoptilolite amendment of sand actsas a mechanism <str<strong>on</strong>g>for</str<strong>on</strong>g> slowly releasingnutrients and water.As seen in Figure 1, clinoptilolite is a rockthat can be ground into sand-size particles.Figure 1. A piece of clinoptilolite zeolite be<str<strong>on</strong>g>for</str<strong>on</strong>g>e processing.It can be mixed with sand, as shown in Figure2, <str<strong>on</strong>g>for</str<strong>on</strong>g> the purpose of increasing both theefficiency of water uptake and nutrientutilizati<strong>on</strong> while reducing nitrate leaching.Other Research FindingsSeveral other researchers have studiedthe effects of clinoptilolite <strong>on</strong> creeping bentgrassgrowth and establishment. Researchc<strong>on</strong>ducted at Washingt<strong>on</strong> State University(Nus and Brauen, 1991)studied the effects ofvarious amendments (sawdust, sphagnumpeat, and a gravel-sized clinoptilolite) atseveral amendment volumes <strong>on</strong> the establishmentof creeping bentgrass <strong>on</strong> sandbasedputting greens. They added sawdust at5%,10%, and 20% by volume; peat at 20%to 33% by volume; and clinoptilolite at 33%JANUARY/FEBRUARY 1993 11


PropertyTABLE!Physical properties of clinoptilolite zeolite-amended sand(CZ-sand) and sand used in the greenhouse experimentHydraulic c<strong>on</strong>ductivity, cm hr- ITotal porosity, % (by v)Water availability, %(between -0.003 and -0.1 MPa)Aerati<strong>on</strong> porosity, % (at -0.003 MPa)Bulk density, g cm- 3Particle density, g cm- 3Particle size analysisGravelTotal sand:SiltClayVery coarseCoarseMediumFineVery Finemm>22 ~ 0.052~11 ~ 0.50.5 ~ 0.250.25 ~ 0.10.1 ~ 0.050.05 ~ 0.002


with Pencross creeping bentgrass <str<strong>on</strong>g>for</str<strong>on</strong>g> thegreenhouse studies. The green profiles werefertilized with amm<strong>on</strong>ium sulfate as thenitrogen source at yearly rates of 2, 4, and 6lbs. N/I,OOO sq. ft. Unfertilized profileswere used as check treatments. Amm<strong>on</strong>iumwas selected as the nitrogen source becauseit is easily retained <strong>on</strong> the zeolite. The profileswere 1)properly watered and 2) wateredto excess (to produce leachate) <strong>on</strong> a weeklybasis. To track the applied fertilizer nitrogenin the putting green system, the profiles weremowed weeky at Yi-inch and the amountof fertilizer nitrogen retained in the clippingswas determined. The weekly leachatesamples were analyzed <str<strong>on</strong>g>for</str<strong>on</strong>g> c<strong>on</strong>centrati<strong>on</strong>sof nitrate and amm<strong>on</strong>ium.As seen in Figure 3, the amount offertilizer N that accumulated in the clippingsvaried with the N applicati<strong>on</strong> rate and zeoliteamendment. As the amount of N appliedincreased, the percentage of applied N thataccumulated in the clippings decreased. Forthe sand profiles, the percentage of appliedfertilizer N that was recovered in the clippingsranged from 62% to 70%. The additi<strong>on</strong>of zeolite to the sand resulted in a greateramount of the fertilizer N ending up in thebentgrass clippings (75% to 93% of theapplied N). This difference was most noticeableat the lower N applicati<strong>on</strong> rate.As seen in Figures 4 and 5, adding zeoliteto sand also resulted in substantially lessnitrate leaching. The c<strong>on</strong>centrati<strong>on</strong> of nitratein the leachate from the putting green profiles,as shown in Figure 5, reveals that inno case was the nitrate level in excess ofthe drinking water standard (10 mg/I) whenthe sand was amended with zeolite. However,water with much higher nitrate levels wasnoted leaching from the sand-<strong>on</strong>ly puttinggreen profiles at all N applicati<strong>on</strong> rates,especially at the highest N rate (6 lbs.N/I,OOO sq. ft.). In this case, the leachatehad nitrate c<strong>on</strong>centrati<strong>on</strong>s in excess ofdrinking water standards at least <strong>on</strong>e thirdof the time.Water Use StudiesIn the same greenhouse experimentdescribed above, the amount of water usedby the creeping bentgrass plants was determinedthree times per week by measuringthe change in weight of the lysimeters. Asseen in Figure 5, applying N to creepingbentgrass increased the shoot growth ratenearly ten times with little or no effect <strong>on</strong>the water use rate. Shoot growth was alsoincreased by the additi<strong>on</strong> of clinoptilolite tosand, without a substantial increase in theamount of water used by the plant. Thus,better shoot growth can be achieved in puresand putting greens with the additi<strong>on</strong> ofclinoptilolite, and this can be accomplishedwith less water and less total N.Summary and C<strong>on</strong>cernsAmending sand putting greens with azeolite like clinoptilolite was shown, fromEil.l10080Zil.l a 60:::l ~CZl.~ ~~ Z..... 40;80~2002FIGURE 3these studies, to result in several importantadvantages. First, nitrate leaching from sandbasedputting greens can be reduced. Sec<strong>on</strong>d,the shoot growth rate and the amountof fertilizer N that ended up in the clippingswas enhanced by the additi<strong>on</strong> of clinoptiloliteto sand. Third, the improved growth ofSand• CZ-sand mixtureTotal N applicati<strong>on</strong> rate, Ibs/1000 ftzFigure 3. The influence of clinoptilolite amendment of sand and nitrogen applicati<strong>on</strong> rate <strong>on</strong> theamount of nitrogen accumulate in the clippings of creeping bentgrass.108il.l~ "'d...l:: .~Co)0..6c\l~ 0..c\l.s Z~~..... 40~20FIGURE 4Figure 4. The influence of clinoptilolite amendment of sand and nitrogen applicati<strong>on</strong> <strong>on</strong> thepercentage offertilizer nitrogen leached from putting greens.4Sand• CZ-sand mixture2 4 6Total N applicati<strong>on</strong> rate, Ibs/1000 ftz6JANUARY/FEBRUARY 1993 13


Q).....co:ll--,~ co:ll-< "0100003.53.02.52.0E-- 8 1.5~ 81.00FIGURE 6246expense of using more water. The creepingbentgrass plants were more efficientin usingwater and N to produce growth.With such str<strong>on</strong>g findings, coupled withthe results from previously published research,it appears that clinoptilolite couldmake an excellent amendment of sand <str<strong>on</strong>g>for</str<strong>on</strong>g>putting greens. Some words of cauti<strong>on</strong>should be noted, however. To my knowledge,<strong>on</strong>ly a handful of golf courses haveused clinoptilolite to either amend newgreens or to use as a topdressing <strong>on</strong> existinggreens. To date the results have beenencouraging. The l<strong>on</strong>g-term stabilityof thecrystalline structure is <strong>on</strong>e major questi<strong>on</strong>that stillneeds to be addressed. If the zeoliteweathersor is crushed by traffic,will itremain a sand-size particle or become silt/clay size, clogging the highly pervioussand? We are initiating several short- andl<strong>on</strong>g-term studies to answer these questi<strong>on</strong>s.L<strong>on</strong>g-term evaluati<strong>on</strong> <strong>on</strong> actual golf courseswith clinoptilolite-amended sand greens isnecessary.Another point to c<strong>on</strong>sider is that theproperties of clinoptilolitecan vary between,and possibly within, deposits. There aresome deposits that are naturally high insodium, potassium, or amm<strong>on</strong>ium, and somecan c<strong>on</strong>tain some clay.High-sodium-c<strong>on</strong>tentclinoptiloliteshould be leached to removethe sodium be<str<strong>on</strong>g>for</str<strong>on</strong>g>e using it with low-salttoleratinggrasses. The hardness of theclinoptilolitealso varies with each deposit.Some are very hard and would be lesslikely to be damaged by traffic,whereasothers are soft and are more easily crushed.The results of the next series of studieswill help establish guidelines in selecting asource of clinoptilolitebased up<strong>on</strong> measurableproperties.LITERATURECITEDFergus<strong>on</strong>, G. A., 1. A. Pepper, and W. R. Kneeb<strong>on</strong>e.1986. Growth of creeping bentgrass <strong>on</strong> anew medium <str<strong>on</strong>g>for</str<strong>on</strong>g> turfgrass growth: c1inoptilolitezeolite-amended sand. Agr<strong>on</strong>. J. 78: 1095-1098.Huang, Z. T. 1992. Clinoptilolite zeolite as anamendment of sand <str<strong>on</strong>g>for</str<strong>on</strong>g> golf green root z<strong>on</strong>es.Ph.D. Thesis. Cornell Univ., Ithaca, NY.Nus, 1. L., and S. E. Brauen. 1991. Clinoptilolitezeolite as an amendment <str<strong>on</strong>g>for</str<strong>on</strong>g> the establishmentof creeping bentgrass <strong>on</strong> sand media. HartSci.26:117-119.Sand• CZ-sand0.50.002 4N rate, Ibs/1000 ft26(Above left)Figure 5. The influence ofclinoptiloliteamendment of sand and nitrogenapplicati<strong>on</strong> rate <strong>on</strong> the c<strong>on</strong>centrati<strong>on</strong> of nitratein the water draining from putting greens.(Left) Figure 6. The influence of clinoptiloliteamendment of sand and nitTvgen applicati<strong>on</strong>rate <strong>on</strong> the shoot growth rate and evapotranspirati<strong>on</strong>(ET) rate of creeping bentgrass.14 USGA GREEN SECTION RECORD

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