Iron Oxides and Their Relations to Colors in Some Soils of Southern China

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    摘要 Ironoxidesfrom33samplesof25soilsderivedfromvariousparentmaterialsinthesouthernChinawerestudiedusingNaOHselectivedissolutiontechniqueandX-raydiffraction(XRD).GoethitandhematiteweretheonlytwocrystallineFeoxidesocurringinasignificantquantity,Thegoethite/(goethite+hematite)ratiosrangedfrom0to1,beingthehighestinyellowsoil,someyellow-redsoilsandsaprolitesamplesandthelowestinsoilsderivedfrompurplesandstonewhereonlyhematitewaspresent.Alsubstituioningoethiterangedfrom6.6to29.9mol%withameanvalueof16.7mol%,whilesubstitutionofAlinhematiterangedfrom0to12.1mol%,ThevaluesofAlsubsitutionofhematiteincoexistinggoethiteandhematitewerecloselyrelatedwithcorrespondingvaluesofgoetheite(r=0.7292,P<0.01,n=27),Therednessratingofsoilsincreasedlinearlywithincrasingamountofhematite(r=0.8109,P<0.01),Itwassuggestedthatrenessratngcouldbeusedtocrudelyestimatehematitecontentsofsoils.
    机构地区 不详
    出处 《土壤圈:英文版》 1998年1期
    出版日期 1998年01月11日(中国Betway体育网页登陆平台首次上网日期,不代表论文的发表时间)
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