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...
Main Authors: | Wiederhold, J, Teutsch, N, Kraemer, S, Halliday, A, Kretzschmar, R |
---|---|
Format: | Journal article |
Jezik: | English |
Izdano: |
2007
|
Podobne knjige/članki
-
Iron isotope fractionation during soil formation - comparison of ligand and redox controlled processes
od: Wiederhold, J, et al.
Izdano: (2004) -
Iron isotope fractionation during goethite dissolution by oxalate
od: Wiederhold, J, et al.
Izdano: (2005) -
Iron isotope fractionation in oxic soils by mineral weathering and podzolization
od: Wiederhold, J, et al.
Izdano: (2007) -
Iron isotope fractionation during proton-promoted, ligand-controlled, and reductive dissolution of Goethite.
od: Wiederhold, J, et al.
Izdano: (2006) -
Iron isotope fractionation in groundwater
od: Teutsch, N, et al.
Izdano: (2002)