Iron isotope fractionation during pedogenesis in redoximorphic soils

Stable Fe isotopes provide a potential new tool for tracing the biogeochemical cycle of Fe in soils. Iron isotope ratios in two redoximorphic soils were measured by multicollector inductively coupled plasma mass spectrometry to study the relationships between pedogenic Fe transformation and redistri...

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Détails bibliographiques
Auteurs principaux: Wiederhold, J, Teutsch, N, Kraemer, S, Halliday, A, Kretzschmar, R
Format: Journal article
Langue:English
Publié: 2007

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