简介：TwoecotypesofElsholtzia,ElsholtziasplendensandE.Argyi,aredominantplantsgrowingonCuandPb-Znsmelters,respectively.SamplesofthetwoecotypesandthecorrespondingsoilsfromfieldsofacopperminingareaandaPb-ZnminingareaofZhejiangProvince,China,wereanalyzedtoinvestigateCuorZntoleranceofthesetwoecotypes.EffectsofnineCulevels(0,5,10,20,40,80,160,240and320mgCuL-1asCuSO4@SH20)ongrowthanduptake,translocationandaccumulationofCuinthesetwoecotypeswereexaminedinasolutioncultureexperiment.Theexperimentalresultsshowedthatdryweights(DW)ofshootsandrootsweredepressed,andgrowthofE.SplendenswaslessdepressedthanthatofE.Argyiwhentreatedwith≥5mgCuL-1.ConcentrationsofCuinshootsofE.SplendensandE.Argyiexceeded1000mgkg-1DWat≥40mgCuL-x.ThemaximumCuaccumulatedintheshootsofGu-treatedE.SplendensandE.Argyireached101and142μgplant-1.Furthermore,analysisofplantsamplesfromthefieldsshowedthatthesetwoecotypescantolerantexcessheavymetalsandproducedhighdrymatter,andE.Splendenscanaccumulate11.7mgCuplant-1grownontheCusmelter.Therefore,E.SplendensandE.Argyicouldbegoodplantsforphytoremediation.

简介：ElementcontentsoftreeringsandsoilsneartreerootscollectedfromDeodarcedar(Cedrusdeodara(Roxb.)G.Don)andMassonpine(Pinusmassonianalamb).weredeterminedtostudytherelationshipbetweentheangulardistributionofelementcontentsintreeringsandtheenvironmentalinformation.Thechemicalcompositionandpropertiesofsoilareverymuchcmoplicated,whichleadstothenon-uniformdistributionoftheelementcontentsintreerings.Thestatisticalmulti-varialberegressionmethodwasusedtogettheinformationofthetree-centereddistributionofelementcontentsintheenvironment(soil),(C'),C'(Z,θj),fromthedistribtuionofelementcontentsintreerings(C),C(Z,θi),whichdependsontheplaneazimuthangle(θi),i.e.,C=C(Z,θi),whereZistheatomicnumberoftheelement,withasatisfactoryresultthoughthisstudyisonlyaprimaryone.

简介：Thedistributionofrareearthelement(REE)formsinsoilsisgiveninthepresentpaperonthebasisofsequentialfractionationanddeterminationof34representativesurfacesoilscollectedfromallpartsofChina.ResultsobtainedshowthattheextractionrateofwatersolubleandexchangeableREEhadtheodd-evenphenomenonandthatoforganicallyboundREEfromLatoLutendedtoreducegraduallywiththeincreaseofatomicnumber.ThestabilityofScandtheactivityandenrichmentofTminsoilsareproposed.Furthermore,thepapermakesapreliminarydiscussiononthedifferencesintheconcentrationdistributionofvariousformsofindividualREEinsomesoils.

简介：Thedepletionrateofphosphateinthesoil-rootinterfacezoneincreasedalongwithgrowthandphosphateuptskeofwheatormaize,whichindicatedthatthephosphatedistributioninsoilneartherootsurfaceagreedwellwiththephosphatemovementinrhizosphereandphosphateuptakebyplant,Therelativeaccumulationzoneofphosphatewithin0.5mmapartfromtherootsurfacedevelopedatthe15thdayorsoaftercultivatingwheatormaizesincetherootphosphatesecretionincreasedgraduallyinthisstage.Thephosphatedistributioninthesoil-rootinterfacezoneagainstthegrowingtime(t)andthedistancefromtherootplane(x)couldbedescribedbythenon-linearregressionequationwiththethirdpowersofxandt.

简介：

简介：Amini-plotfieldexperimentwasconductedonaloamyclayOxisoltocompareandevaluatePabsorptionandtransferinplantorgansandPmovementinsoilprofileatthreePapplicationdepthsunderthesoybean-citrusintercroppingversusthemonocultureusinga32Ptracertechnique.TotalPabsorption(Pt)bysoybeanandPaccumulation(Pa)insoybeanorgansdecreasedsignificantly(P<0.05)undertheintercroppingincontrasttothemonoculture.Withintercropping,when32Pwasappliedintopsoil(15cmsoillayer),total32Pabsorption(32Pt)insoybeanswassignificantlylower(P<0.05),butwhen32Pwasappliedtodeepersoillayers(35or55cmsoillayer),32Ptinsoybeanswassignificantlygreater(P<0.05).ThepercentageofPinleavestototalP(Pa/Pt)and32Pinleavestototal32P(32Pa/32Pt)forsoybeanwere(?)25%andthoseofroot(?)12%.WhenPwasappliedintopsoiland55cmsoillayer,nosignificantdifferenceswerefoundbetweenintercroppingandmonocultureforPtofcitrus.ThePabsorbedbycitruswastransferredrapidlytothegrowingorgansofabovegroundduringtheexperiment,andthespeedoftransferringtothegrowingorgansslowedwhenPwasappliedtothedeepersoillayers.Inintercropping,Pmobilitywasheightenedinthesoilprofile,andPindeepersoillayersmoveduptotopsoilmorerapidly.

简介：节省水的灌溉方法逐渐地在温室或塑料电影房子为蔬菜耕作被使用了。然而，有关土壤磷(P)行为上的节省水的灌溉方法的效果有有限信息。在这个实验，滴下并且表面下的灌溉方法被使用，与是的沟灌溉方法控制，在MollicGleysols。在整个深度的土壤P分发被灌溉方法显著地影响。全部，Olsen，器官、无机的P内容比在心土(20–30，30–40，40–50和50–60厘米)在表层土(0–10和10–20厘米)是更大的。在整个0–60厘米层在下面的OlsenP内容滴下并且表面下的灌溉处理在沟灌溉处理下面是比那低的。然而，全部、器官、无机的P从20～60厘米满足在下面滴灌溉处理比或近到在沟灌溉处理下面的那些高，但是比在沟灌溉处理下面在表面下的灌溉处理下面是更低的。在表面下的灌溉处理下面，在0–10厘米层的全部、器官、无机的P的内容是78.0%，1.3%和3.7%比那些大在10–20厘米层分别地。但是在10–20厘米层的OlsenP内容是5.7%比那大在0–10厘米层。这些建议那土壤P行为能被土壤水管理操作到某程度。

简介：Co,Ni,CrandVin25typicalsoilsofChinawerefractionatedintoexchangeable,carbonatebound(calcareoussoils),Mnoxidebound,organicallybound,amorphousFeoxidebound,crystallineFeoxideboundandresidualformsusingaseven-stepsequentialextractionprocedure,soastostudythedistributionofchemicalformsofthesemetalsaswellastheeffectsofsoilproipertiesonthedistribution.TheresultsshowedthatmostofsoilCo,Ni,CrandVwerepresentinresidualforms,andthedistributionratioaveraged48.2%forCo,53.0%forNi,81.5%forCrand68.7%forV.Thespeciationofheavymetalswasgreatlyinfluencedbysoilphysico-chemicalpropertiesandthechemistryofelements.Theresultsalsoindicatedthattherecoveryofmetalelementsbythesequentialextractionprocedurewassatisfactory,withtherelativedifferencebetweenthesumofsevenformsandthetotalcontentinsoilsaveraging9.5%forCo,12.8%forNi,6.6%forCrand7.2%forV.

简介：AleachingexperimentwasCarriedoutwithrepackedsoilcolumnsinlaboratorytostudytheleachingprocessofaredsoilderivedfromsandstoneasaffectedbyvariousfertilizationpractices.ThetreatmentswereCK(asacontrol),CaCO3,CaSO4,MgCO3,Ca(H2PO4)2,Urea,KCl,Multiple(amixtureoftheabovementionedfertilizers)andKNO3,Thefertilizerswereaddedtothebaresurfaceofthesoilcolumns,andthenthecolumnswereleachedwith120mLdeionizedwaterdailythroughperstalticpumpsoveraperiodof92days,Attheendofleachingprocess,soilsweresampledfromdifferentdepthsofthesoilprofiles,i.o.,of92days,Attheendofleachingprocess,soilsweresampledfromdifferentdepthsofthesoilprofiles,I.e.0-5cm,5-10cm,10-20cm,20-40cm,and40-60cm,TheresultsshowedwhenapplyingCa,Mg,andKtothebaresurfaceofthesoilcolumns,exchangeableCa^2+,Mg^2+,andK^+intheupperlayerofthesoilprofileincreasedcorrespondingly,withanextentdependingmainlyontheapplicationratesofCa,Mg,andKandshowingadownwardtrend,CaCO3,CaSO4,MgCO3,andCa(H2PO4)2treatmentshadscarcelyandeffectonmovementofexchangeableK^+,whileCaCO3,andCaSO4treatmentssingnificantlypromotedthedownwardmovementofexchangealbleMg^2+althoughthesetwotreatmentshadnoobviouseffectonleachinglossesofMg,ThefactthatunderUreatreatment,exchangeableCa^2+andMg^2+,werehigherascomparedtoCKtreatmentshowedureacouldpreventleachingofexchangeableCa^2+andMg^2+,theobviousdownwardmovementofexchangeableCa^2+andMg^2+wasnoticedinKCltreatment,InMultipletreatment,thedownwardmovementofexchangeableCa^2+andMg^2+wasevident,whilethatofK^+waslessevident,ApplicationofKNO3stronglypromotedthedownwardmovementofexchangeableCa^2+andMg^2+inthesoilprofile.

简介：ThedistributionandtransformationofaddedandnativeNiinpurplesoilswereinvestigatedwithbothsequentialextractionprocedureandisotopictracertechnique.ThedistributionofaddedandnativeNiwasgreatlydependentonsoilproperties.LowsoilpHwasfavorableforsolubleplusexchangeable(EX)Fraction,whileFe/MnoxidesandclayforFe/Mnoxidebound(OX)andresidual(RES)fractions.TheaddedNi,however,hasnotyetreachedthedistributionequilibriumuptothe150thdayafterincubation.ThiswasreflectedinthefactthattheproportionofEXfractionfromaddedNiwas150%-600%asmuchasthatofnativeNi,whilethatofRESfractionwasonlyabout80%,Onceenteringsoil,theappliedsolubleNiwasrapidlytransformedintootherfractions,buttheorganiccomplexe(OM)fractionofaddedNiwasrelativelystableduringincubation.Thecarbonatebound(CAB)fractionshowedaprogressiveincreaseandattainedapeakvalueafter0-14dofincubationandthereafterdecreasedgradually.TheoccurrencetimeofthispeakadvancedasinitialsoilpHincreased.butthepeakwoulddisappearwheninitialsoilpHwashigherthan7.5(orcontainingfreeCaCO3).ThetransformationprocessesoftheEX,OXandRESfractionscouldbedescribedbyElovichandtwo-constantrateequations,andtheratewerepositivelycorrelatedwithsoilpH,CECandclay.ThesefindingcouldexplainwhytherearedifferencesinecologicalandenvironmentaleffectsofNiindifferentsoilsandatvariousintervals.

简介：TheverticaldistributionandmigrationofCu,Zn,Pb,andCdintwoforestsoilprofilesnearanindustrialemissionsourcewereinvestigatedusingahighresolutionsamplingmethodtogetherwithreferenceelementTi.One-metersoilprofilewassectionedhorizontallyat2cmintervalsinthefirst40cm,5cmintervalsinthenext40cm,and10cmintervalsinthelast20cm.Themigrationdistanceandrateofheavymetalsinthesoilprofileswerecalculatedaccordingtotheirrelativeconcentrationsintheprofiles,ascalibratedbythereferenceelementTi.Theenrichmentofheavymetalsappearedintheuppermostlayeroftheforestsoil,andthesoilheavymetalconcentrationsdecreaseddowntheprofileuntilreachingtheirbackgroundvalues.ThecalculatedaveragemigrationratesofCd,Cu,Pb,andZnwere0.70,0.33,0.37,and0.76cmyear-1,respectively,whichwerecomparabletoothermethods.Asimulationmodelwasproposed,whichcouldwelldescribethedistributionofCu,Zn,Pb,andCdinnaturalforestsoils.

简介：Assessmentofsoilqualityisimportantforoptimumproductionandnaturalresourcesconservation.AgriculturalandpasturesoilqualitiesofDeh-SorkhregionlocatedatsouthofMashhad,northeasternIranwereassessedusingtheintegratedqualityindex(IQI)andNemeroqualityindex(NQI)modelsincombinationwithtwodatasets,i.e.,totaldataset(TDS)andminimumdataset(MDS).Inthisstudy6soilpropertiesconsideredasMDSwereselectedoutof18propertiesasTDSusingprinciplecomponentanalysis.Soilsamplesweredividedinto3groupsbasedonoptimumrangesof8soilphysicalqualityindicators.Soilsampleswiththemostindicatorsatoptimumrangewereselectedasgroup1andthesampleshavingfewerindicatorsatoptimumrangewerelocatedingroups2and3.Optimumrangesofsoilporesizedistributionfunctionswerealsodeterminedassoilphysicalqualityindicesbasedon8soilphysicalqualityindicators.Poresizedistributioncurvesofgroup1wereconsideredastheoptimumporesizefunctions.Theresultsshowedthatrelativelyhighorganiccarboncontentscouldimproveporesizedistribution.Meancomparisonsofsoilphysicalqualityindicatorsdemonstratedthatmeanweightdiameterofwetaggregates,structuralstabilityindex,theslopeofmoistureretentioncurveatinflectionpoint,andplantavailablewatercontentinagriculturallandusedecreasedsignificantlyinrelationtopasturelanduse.Inaddition,theresultsdemonstratedthatthestudiedMDScouldbeasuitablerepresentativeofTDS.78%ofpasturesoilshadtheoptimumporesizedistributionfunctions,whilethisparameterforagriculturalsoilswasonly13%.Ingeneral,thesoilsofthestudiedregionshowedhighlimitationsforplantgrowthaccordingtothestudiedindicators.

简介：印射土壤硝酸盐氮(NO3-N)的空间分发是重要的指导氮申请以及估计沥滤进地下水的NO3-N的环境风险。我们采用了univariate和混合geostatistical方法在东北佛罗里达越过一处风景印射土壤NO3-N的空间分发。土壤样品从四深度增长被收集(030，3060，60120和120180厘米)基于土壤，土地使用和举起阶层从用成层的随机识别并且嵌套采样的147个采样地点设计。在二层是的顶的土壤NO3-N分布空间地，汽车相关并且印射使用木头正常kriging。为NO3-N预言的环境关联模型用线性、非线性的回归方法被导出，并且采用了开发NO3-N趋势地图。陆地使用和它从卫星形象导出的相关变量作为重要变量被识别用环境关联模型预言NO3-N。当木头正常kriging生产了顺利变化的地图时，从环境关联模型导出的趋势地图产生了空间地异构的地图。趋势地图与趋势模型剩余的平常的kriging预言被相结合开发回归kriging预言地图，它给了最好的NO3-N预言。因为土地使用和遥远地察觉到的数据是容易地可得到的并且有大部分，与地相比的更好的空间分辨率取样了土壤，我们的调查结果基于为风景的使用和遥远地察觉到的数据放大土壤NO3-N印射的土地建议了环境关联模型的功效。实现的方法论为在另外的风景土壤NO3-N印射是可转让的。

简介：植物有多样的策略应付磷(P)缺乏。更好理解玉米怎么对P缺乏作出回应，有二P的一个地实验铺平，0和100kgP2O5ha1(P0和P100，分别地)，作为长期的P化肥地试用的部分被执行。植物和土壤分析证明那P缺乏的玉米减少了它的生长率，增加了P使用效率，并且形成了有在连接和silking的不到0.6公里上演的直径的更多的薄根，与与P100对待的植物相比。进一步，在每收获在在rhizospheric和体积土壤之间的主要无机的P部分(Ca2-P，Ca8-P，高山，Fe-P，堵塞P和Ca10-P)没有差别，甚至当土壤Olsen-P仅仅是1.38mgkg1时。这些结果建议那玉米由由在低碳的词法改变花费了的有利的根为生长和增加的P获得能力减少内部P需求对P缺乏作出回应。

简介：Atotalof400surfacesoil(0–15cm)sampleswerecollectedfromcultivatedsoilsrepresentingfoursoilseries,namely,Hariharapur,Debatoli,RajporaandNeeleswaraminOrissa,Jharkhand,HimachalPradeshandKeralastatesofIndia,respectively,andwereanalyzedtomeasurethecontentsoftotalandextractableMnandFe,toestablishtherelationshipamongtotalandextractableMnandFeandsoilproperties,andtocharacterizethespatialdistributionpatternofMnandFeinsomecultivatedacidsoilsofIndia.ThecontentsoftotalaswellasextractableMnandFevariedwidelywithextractantsandsoilseries.However,theamountsofMnorFeextractedbydiethylenetriaminepenta-aceticacid(DTPA),Mehlich1,Mehlich3,0.1molL-1HClandammoniumbicarbonateDTPA(ABDTPA)weresignificantlycorrelatedwitheachother(P<0.01).BasedontheDTPA-extractablecontentsandthecriticallimits(2mgMnkg-1soiland4.5mgFekg-1soil)publishedintheliterature,MnandFedeficiencieswereobservedin7%–23%and1%–3%ofthesoilsamples,respectively.Thecontentofsoilorganiccarbon(SOC)hadgreaterinfluenceontotalandDTPA-extractableFethandidsoilpH.GeostatisticalanalysisrevealedthattotalandDTPA-extractableMnandFecontentsintheacidsoilswereinfluencedbysoilpH,SOCcontent,andexchangeablecationslikepotassium,calciumandmagnesium.SpatialdistributionmapsoftotalandDTPA-extractableMnandFeinsoilindicateddifferentdistributionpatterns.

简介：Apotexperimentwithtworice(OrizasativaL.)genotypesdifferingininternalpotassiumuseefficiency(IKUE)wasconductedunderdifferentsodium(Na)andpotassium(K)levels.AddingNaC1ataproperlevelenhancedricevegetativegrowthandincreasedgrainyieldandIKUEunderlowpotassium.AdditionofhigherrateofNaC1hadanegativeeffectonthegrowthoftheK-efficientricegenotype,butdidnotfortheK-inefficientgenotype.Underlow-Kstress,higherNaC1decreasedIKUEoftheK-efficientricegenotypebutincreasedIKUEfortheK-inefficientgenotype.Attilleringstageandunderlow-Kstress,addingNaClincreasedKandNacontentsanddecreasedtheratioofK/Naforbothgenotypes.Atharvestingstageunderlow-Kstress,addingNaG1increasedKandNacontentsandK/NaratiofortheK-efficientgenotypebutdecreasedtheK/NaratiofortheK-inefficientgenotype.TheaccumulatedNawasmostlydepositedintherootsandsheaths.Attilleringstage,theKandNacontentsandtheK/Naratiosindifferentpartsforbothgenotypesdecreasedinthefollowingsequence:K+insheaths＞K+inblades＞K+inroots;Na+inroots＞Na+insheaths＞Na+inblades;andK/Nainsheaths》K/Nainroots.TheK-efficientgenotypehadalowerK/NaratioinrootsandsheathsthantheK-inefficientgenotypeunderlow-Kstress.Atharvestingstage,KandNacontentsingrainswerenotaffected,whereasK/NaratiointhericestrawswasincreasedfortheK-efficientgenotypebutdecreasedfortheK-inefficientgenotypebyNaaddition.However,thiswasnotthecaseunderKsufficientcondition.