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当前位置:首页 > 商业/管理/HR > 管理学资料 > 氮素形态对中后期小麦根际土壤氮转化微生物及酶活性的影响王小纯
246201012JournalofSoilandWaterConservationVol.24No.6Dec.,2010 :2010-09-16 :(30771266);(200803028) :(1966-),,,,。E-mail:xiaochun.w@163.com :(1963-),,,,。E-mail:xinmingma@126.com王小纯1,李高飞1,安帅1,熊淑萍2,马新明2(1.,450002;2.,450002):、34。,,:。、、、,14,;,,14,。、。,,NO-3,,,。:;;;;:S512.1;S154.2;S154.3 :A :1009-2242(2010)06-0204-04EffectsofNitrogenFormsonRhizosphereMicroorganismsandSoilEnzymeActivityforNitrogenTransformofWheatCultivarduringElongationandGrainFillingStageWANGXiao-chun1,LIGao-fei1,ANShuai1,XIONGShu-ping2,MAXin-ming2(1.CollegeofLifeScience,Zhengzhou450002;2.CollegeofAgriculture,HenanAgriculturalUniversity,Zhengzhou450002)Abstract:Withpotexperiments,theeffectofthreenitrogenforms,nitrate(NaNO3),ammonia(NH4HCO3)andurea(NH2CONH2)onrhizospheremicroorganismsandsoilenzymeactivityfornitrogentransformofwheatcultivar(Yumai34)ofdifferentstagewasstudied.Theresultsindicatedasfollows:Therewereprominentdifferenceamongtheactivitiesofdifferentrhizospheremicroorganismsandsoilen-zymesfornitrogentransform,theactivityturnwas:Theactivityofbacterialofdenitrafication,nitrification,proteinase,sub-nitrificationandammonificationincreasedgraduallyfromelongationstage,wentuptomaxi-mumvalueonthe14thdayafterflowering,thenbegantodecrease.Incontrasttotheabove,theactivityofureasewasmaximumduringelongationstage,decreasedgraduallytotheminimumvalueonthe14thdayaf-terflowering,andthenincreasedalittle.Theeffectsofthreenitrogenformsonrhizospheremicroorganismsandsoilenzymeactivityfornitrogentransformweredependentonthephysiologicalspeciesofmicroorgan-ismsandthekindofenzyme.Basedonthecomprehensiveanalysis,ammoniacouldfacilitatethedecomposi-tionandutilizationoforganicnitrogen,facilitatethetransformofNH+4toNO-3,andinhibitedthelossnitro-geninducedbydenitrafication,andureahadabettereffects,nitratehadtheworsteffects.Keywords:wheat;nitrogenforms;rhizosphere;microorganismsfornitrogentransform;soilenzyme,40%[1]。,,,。[2-3]、[4];[5-6]。,,。,。。,、、[7-8]。--,,[9]。,()(),[10-11]。,、。,[12],,[13]。,,[14-15]。,(),、,。1 材料与方法1.1 2009-2010,。:14.29g/kg,1.50g/kg,57.17mg/kg,16.9mg/kg,195.95mg/kg。,30cm,38cm,20kg。34;(NaNO3)、(NH4HCO3)()。5.1g,K2O3.3g,P2O52.9g,、1,6∶4。1018,14,5,7。,。,15。1.2 1.2.1 土样采集 、、14d28d,10:00,5-25cm,。2mm,,,。1.2.2 微生物生理类群活性测定 ,()[16];()[26]。,3。1.2.3 根际土壤酶活性 4g,。5g,[17]。,3。1.3 ExcelSPSS。1 2 2 结果与分析2.1 (),。1,,14,。。,;,;1428。2.2 ,。2,,,14,,。,;14;28,。2056 :3 4 5 6 2.3 NO-2NO-3,。3,,;,14,,,,。2.4 N2N2O,,。4,,,14,1g6mg,,。,28。,1428。2.5 (、、)(Ni),,,。5,,1g1.6mg;,14,28,。,。,;14;28。2.6 、,N,。6,,,14(512.3~555.6μg/g·d),,。,。;1428。3 结语与讨论3.1 ,:(3675.8μg/g·d)(729.3μg/g·d)(637.6μg/g·d)(350.4μg/g·d)(127.2g/g·d)(93.1μg/g·d)。、NH+4,NO-3,,NH+4NH+4NO-3,,NO-3,。[18],,NH+4。NO-3,;,。,。NO-3N2206 24N2O,,N2O、。5,39.5,。3.2 ,、、、,14,,NO-3-N(10mg/g),,。[15],。,;14,,、,;28,,,。,,(5mg/g),,14,28。3.3 。,:(4816.9μg/g·d)(4810.7μg/g·d)(473.5μg/g·d);:(745.5μg/g·d)(744.6μg/g·d)(710.6μg/g·d);:(1044.8μg/g·d)(999.8μg/g·d)(946.1μg/g·d);:(371.8μg/g·d)(365.1μg/g·d)(314.2μg/g·d);:(142.2μg/g·d)(128.2μg/g·d)(110.5μg/g·d);:(76.1μg/g·d)(69.7μg/g·d)(64.5μg/g·d)。,、;,NO-3,;,。,,NO-3,,。、,28,5cm(15±2)℃,15-25cm(14.5±0.2)℃,2~3℃,[19]。,,、NO-3[23]。,,,,;。:[1] ZhuZ.LossoffertilizerNfromtheplant-soilsystemandthestrategiesandtechniquesforitsreductioninChina[J].SoilEnvironmentalScience,2000,9:1-6.[2] GilesJ.Nitrogenstudyfertilizesfearsofpollution[J].Nature,2005,433:791.[3] BemanJM,ArrigoK,MatsonPM.Agriculturalrunofffuelslargephytoplanktonbloomsinvulnerableareasoftheocean[J].Nature,2005,434:211-214.[4] ,.[J].,1995,1(2):80-87.[5] RamosC.Effectofagriculturalpracticesonthenitrogenlossesintheenvironment[M].TheNetherlands:KluwerAcademicPublishers,1996:355-361.[6] StulenI,Perez-SobaM,DeKokLJ,etal.Impactofgaseousnitrogendepositiononplantfunctioning[J].NewPhytologist,1998,139:61-70.[7] WalleyF,YatesT,vanGroeningenJW,etal.Relationshipsbetweensoilnitrogenavailabilityindices,yield,andnitrogenaccumulationofwheat[J].SoilScienceSocietyAmericanJournal,2002,66:1549-1561.[8] BurgerM,JacksonLE.Plantandmicrobialnitrogenuseandturnover:rapidconversionofnitratetoammoniuminsoilwithroots[J].PlantandSoil,2004,266:289-301.[9] ,,.[J].,1999,8(3):203-207.[10] ,,,.[J].,2008,16(4):321-327.[11] ,,,.[J].,2006,17(6):1060-1064.下转第245页2076 ::[1] ,,,.[J].,2008,24(7):25-28.[2] AdelZT,AnyojiH,YasudaH.Fixedandvariablelightextinctioncoefficientsforestimatingplanttranspirationandsoile-vaporationunderirrigatedmaize[J].Agriculturalwatermanagement,2006,84:186-192.[3] .[J].,1990,9(4):94-103.[4] .[J].,2007,38(2):374-378.[5] ,,,.[J].,2006,29(4):523-526.[6] ,,,.[J].,1996,32(1):170-174.[7] BerndtssonR,NcdomiK.Soilwaterandtemperaturepatternsinanariddesertdunesand[J].JournalofHydrology,1996,185:221-240.[8] BerndtssonR,ChenH.Variabilityofsoilwatercontentalongatransectinadesertarea[J].JournalofAridEnviroment,1994,27:127-139.[9] ,,,.[J].,2005,25(2):243-248.[10] ,,,.[J].,2008,22(1):162-166.[11] ,,,.[J].,2005,25(2):243-248.[12] ,,.[J].,2007,15(6):44-47.[13] ,·,.[J].:,2005,22(1):87-90.[14] ,,,.[J].,2004,35(8):114-118.[15] ,,,.[J].,2007,23(10):6-13.[16]
本文标题:氮素形态对中后期小麦根际土壤氮转化微生物及酶活性的影响王小纯
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