Low temperature, non-stoichiometric oxygen-isotope exchange coupled to Fe(II)–goethite interactions-Reference-Cited by-同舟云学术

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Low temperature, non-stoichiometric oxygen-isotope exchange coupled to Fe(II)–goethite interactions

Published:2015-07 Issue: Volume:160 Page:38-54
ISSN:0016-7037
Container-title:Geochimica et Cosmochimica Acta
language:en
Short-container-title:Geochimica et Cosmochimica Acta

Author:

Frierdich Andrew J.,Beard Brian L.,Rosso Kevin M.,Scherer Michelle M.,Spicuzza Michael J.,Valley John W.,Johnson Clark M.

Funder

National Science Foundation

NSF

Geosciences Research Program at PNNL

U.S. Department of Energy (DOE), Office of Basic Energy Sciences, Division of Chemical Sciences, Geosciences, and Biosciences

U.S. Department of Energy, Office of Science, Office of Basic Energy Sciences

Publisher

Elsevier BV

Subject

Geochemistry and Petrology

Reference80 articles.

1. Rates of ligand exchange between >FeIII−OH2 functional groups on a nanometer-sized aqueous cluster and bulk solution;Balogh;Inorg. Chem.,2007

2. Oxygen isotope fractionation in ferric oxide-water systems: Low temperature synthesis;Bao;Geochim. Cosmochim. Acta,1999

3. Paleocene-Eocene climatic variation in western North America: evidence from the δ18O of pedogenic hematite;Bao;Geol. Soc. Am. Bull.,1999

4. Oxygen isotopic composition of ferric oxides from recent soil, hydrologic, and marine environments;Bao;Geochim. Cosmochim. Acta,2000

5. Application of Fe isotopes to tracing the geochemical and biological cycling of Fe;Beard;Chem. Geol.,2003

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