摘要
Mineralogical,physicalandchemicalanalysesofthesoilsderivedfromXiashuloesswerecarriedout.Theprimarymineralsofthesesoilswerefoundtobemainlycomposedoflightminerals,suchasquartz,feldsparandmica,withtracesofheavyminerals.Clayminerals,morecomplicateincomposition,weredominatedbyhydromica,accompaniedbysmectite,vermiculite,chlorite,kaolinite,2:1/1:1randomlyinterstratifiedmineralsandsmallamountsofquartz,goethite,lepidocrociteandhematite,Claymineralswerecharacterizedbylowcrystallinityandfineparticlesize.Inlightofthequartz/feldsparsratioofthe0.01-0.05mmsiltfraction,andtheclaymineralcomposition,thefreenessofironoxide,andthesilica/sesquioxideandsilica/aluminaratiosin<0.002mmclayfraction,itisconcludedthattheweatheringintensityofthesesoilswaslowerthanthoseofredsoilandyellowearth,buthigherthanthatofbrownearth,andthatthesoilallitization,depotassicationandhydroxylationofclaymineralsincreasedfromwesttoeastandfromnorthtosouthgeographically.However,thisgeneraltendencedidnotcoincideexactlywiththegradualalterationofthegeographiccoordinates,andinsomeplaces,areversetendencyalsoappeared,whichcouldbeattributedtotheinfluenceofsomesoilformingfactorssuchasparentmaterialandmicrotopography.
出版日期
1992年02月12日（中国期刊网平台首次上网日期，不代表论文的发表时间）
