Stable Cu isotope fractionation in soils during oxic weathering and podzolization

Copper stable isotope ratios are fractionated during various biogeochemical processes and may trace the fate of Cu during long-term pedogenetic processes. We assessed the effects of oxic weathering (formation of Cambisols) and podzolization on Cu isotope ratios (δ 65Cu). Two Cambisols (oxic weathere...

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Bibliographic Details
Published inGeochimica et cosmochimica acta Vol. 75; no. 11; pp. 3119 - 3134
Main Authors Bigalke, Moritz, Weyer, Stefan, Wilcke, Wolfgang
Format Journal Article
LanguageEnglish
Published Elsevier Ltd 01.06.2011
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