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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Published in | Geochimica et cosmochimica acta Vol. 75; no. 11; pp. 3119 - 3134 |
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Main Authors | , , |
Format | Journal Article |
Language | English |
Published |
Elsevier Ltd
01.06.2011
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Subjects | |
Online Access | Get full text |
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