Relationship Between Soil Properties and Different Fractions of Soil Hg

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摘要 CorrelationandpathanalysismethodswereusedtostudytherelationshipbetweensoilpropertiesandthedistributionofdifferentsoilHgfractionswithninerepresentativesoilsfromChongqing,China.Resultsshowedthatclay(<2m)couldincreasewater-solubleHg(r=0.700*).Soilorganicmatter(OM)couldenhancetheincreaseofelementalHg(r=0.674*).Thehigherthebasesaturationpercentage(BSP),themoretheresidualHg(r=0.684*).OrganicHg,thesumofacid-solubleorganicHg.andalkali-solubleHg,waspositivelyaffectedbysilt(2~20μm)butnegativelyaffectedbypH,withthedirectpathcoefficientsamountingto1.0487and0.5121,respectively.ThepositiveeffectofOMandnegativeeffectofBSPonorganicHgwerethemostsignificant,withthedirectpathcoefficientsbeing0.7614and-0.8527,respectively.Theindirecteffectofclay(<2μm)viaBSP(pathcoefficient=0.4186)wasthehighest,showingthattherealinfluencingfactorintheeffectofclay(<2μm)onacid-solubleorganicHgwasBSP.SincetheavailableHgfraction,water-solubleHg,waspositivelyaffectedbysoilclaycontent,andthequiteimmobileandnotbioavailableresidualHgbysoilBSP,suitablereductionofclaycontentandincreaseofBSPwouldbeofmuchhelptoreducetheHgavailabilityandHgactivityinHg-contaminatedsoils.
机构地区 不详
出处 《土壤圈:英文版》 2001年3期
出版日期 2001年03月13日(中国期刊网平台首次上网日期,不代表论文的发表时间)
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