基于oryza2000模型的北京地区旱稻农田水分平衡分析

基于oryza2000模型的北京地区旱稻农田水分平衡分析

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时间:2019-02-02

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1、AbstractInthispaper,thecropandsoilwaterbalancemodulesofORYZA2000werecalibratedandvalidated.accordingtoexperimentdata,whichwereconductedinBeijingfrom2003and2005。Andthentheanalysisaboutsoilwaterbalancecomponentsofaerobicricewasexecuted.BesidesWealsoexploredthee

2、ffectofgroundwatertableandsoiltextureonsoilwaterbalancecomponentsbytheuseofmodifiedmodel.ORYZA2000lowlanddeesimulationmodeIWaScalibratedbasedontheresultsofexperimentsin2004.AndthenthevalidationofmodelWaSexecutedintermsofthedynamicbiomass,yieldandsoilwatertens

3、ionbasedonresultin2003and2005.WefoundthattheoverallperformanceofmodifiedmodelwitlIrespecttobiom麟isgoodandthesimulationofyieldrankssecond。But,theevaluationofLAlisnotSOgoodasbiomassandyield;andthebiasofsoilwatertensionisliHle.Wesummarizodthecharacteristicsofsol

4、lwaterbalancein3years.Thewaterrequirementinwholegrowthseasonofaerobicricerangedfrom610mm-643mm,whichfocusedonemergencestagetoPIstage,accountingfor45%.Andanalysisaboutrelationshipbetweensoilwaterbalance,waterinputandcropgrowthwe糟made.Groundwaterplaysakeyrolein

5、thedeterminingofsoilwaterbalance.especiallyforcroptranspiration,soilpercolationandsoilwaterstorage.InChangpingsoil,theyreducewiththedecreaseofwaterinput;whereasforShangzhuangsoil,croptranspirationandsoilwaterstorage81"0notSOsignificantdifferenceasthoseinChang

6、ping,whichisaccountedforcapillaryrisewateratShangzhuangstation.Besides,Welll$detheanalysisabouttherelationshipofsoilwaterbalancecomponents.Finally,byuseofmodel,wee“xploredtheeffectofGroundWaterTable(GWT)andsoilcharacteristicsonsollwaterbalanceandrainfedyieldo

7、faerobicrice.Thesollwaterbalanceandrainfedyieldhavedifferentperformance,whenGWTkeepsaboveorunderneathlm,whichsuggestedthatlmGWTisacriticalpoint.Besides,itissoilwaterretentionabilityoftwosoilsthatbroughtaboutdifferentperformanceofsoilwaterbalanceandrainedyield

8、.ForquantilyingtheimpactofGWTandsoilcharacteristicsonsoilwaterbalanceandralnfedyield,WealsobuiltthefunctionrelationshipbetweenGWTandrelativeevapotranspirationundertwosoilconditions,whichh

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