Iron isotope fractionation in oxic soils by mineral weathering and podzolization
Stable iron isotope ratios in three soils (two Podzols and one Cambisol) were measured by MC-ICPMS to investigate iron isotope fractionation during pedogenic iron transformation and translocation processes under oxic conditions. Podzolization is a soil forming process in which iron oxides are dissol...
| Main Authors: | , , , , |
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| Formato: | Conference item |
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2007
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