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CHARACTERIZATION OF A TOPOSEQUENCE WITH FRAGIPAN: THE LEEDS–STE. MARIE–BROMPTON SERIES OF SOILS, PROVINCE OF QUEBEC
[摘要] ThissequenceofsoilsdevelopedintheAppalachianHighlandsfromglacialtill,ofwhichthemajorcomponentwasslate.Thebedrockoccurredat1.75 mbelowthesurfaceandlargelyinfluencedtheprofiledevelopment.ThefirstprofilewasaPodzolunderwhichthefragipanwascharacterizedbymorphologicalandphysicalcriteria.ThesecondprofilewasaFeraGleysolwherethefragipanwasalsopresent,butlesswelldefinedthaninthePodzolbecauseofamoresandytextureinthedeposit.Finally,thethirdprofilewasanOrthicHumicGleysolwherethepersistenceofhighhumidityconditionsformostoftheyearwasnotfavorabletotheformationofthecharacteristicgraystreaksofafragipan.Itwasfoundfrommineralogicalanalysesthatillitewasthemajorconstituentoftheclayfractioninallthehorizons.However,expandingmineralswerealsopresentandweatheringsequencesweredetectedbutbecauseofthenatureofthedeposit,theweatheringprocessesappearedtobeslow.
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[效力级别]  [学科分类] 农业科学(综合)
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