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Journal article

Adsorption as a cause for iron isotope fractionation in reduced groundwater

Abstract:

Iron isotopes were used to investigate iron transformation processes during an in situ field experiment for removal of dissolved Fe from reduced groundwater. This experiment provided a unique setting for exploring Fe isotope fractionation in a natural system. Oxygen-containing water was injected at a test well into an aquifer containing Fe(II)-rich reduced water, leading to oxidation of Fe(II) and precipitation of Fe(III)(hydr)oxides. Subsequently, groundwater was extracted from the same well...

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Publication status:
Published

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Publisher copy:
10.1016/j.gca.2005.04.007

Authors


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Institution:
University of Oxford
Department:
Oxford, MPLS, Earth Sciences
Role:
Author
More by this author
Institution:
University of Oxford
Department:
Oxford, MPLS, Earth Sciences
Role:
Author
Journal:
GEOCHIMICA ET COSMOCHIMICA ACTA
Volume:
69
Issue:
17
Pages:
4175-4185
Publication date:
2005-09-01
DOI:
ISSN:
0016-7037
URN:
uuid:61c0b70f-af9c-4bde-9c10-909c0d07b1a0
Source identifiers:
82634
Local pid:
pubs:82634
Language:
English

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