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Iron Isotope Fractionation during Pedogenesis in Redoximorphic Soils

Iron Isotope Fractionation during Pedogenesis in Redoximorphic Soils

https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_proquest_miscellaneous_19891413

Iron Isotope Fractionation during Pedogenesis in Redoximorphic Soils

About this item

Full title

Iron Isotope Fractionation during Pedogenesis in Redoximorphic Soils

Publisher

Madison: Soil Science Society

Journal title

Soil Science Society of America journal, 2007-11, Vol.71 (6), p.1840-1850

Language

English

Formats

Publication information

Publisher

Madison: Soil Science Society

More information

Scope and Contents

Contents

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 redistribution processes, and mass-dependent fractionation...

Alternative Titles

Full title

Iron Isotope Fractionation during Pedogenesis in Redoximorphic Soils

Authors, Artists and Contributors

Identifiers

Primary Identifiers

Record Identifier

TN_cdi_proquest_miscellaneous_19891413

Permalink

https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_proquest_miscellaneous_19891413

Other Identifiers

ISSN

0361-5995

E-ISSN

1435-0661

DOI

10.2136/sssaj2006.0379

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