Spectroscopic Evidence for Fe(II)–Fe(III) Electron Transfer at Clay Mineral Edge and Basal Sites-Reference-Cited by-同舟云学术

Spectroscopic Evidence for Fe(II)–Fe(III) Electron Transfer at Clay Mineral Edge and Basal Sites

Published:2013-03-21 Issue:13 Volume:47 Page:6969-6977
ISSN:0013-936X
Container-title:Environmental Science & Technology
language:en
Short-container-title:Environ. Sci. Technol.

Author:

Neumann Anke¹,Olson Tyler L.¹,Scherer Michelle M.¹

Affiliation:

1. Civil and Environmental Engineering, The University of Iowa, Iowa City, Iowa 52242, United States

Publisher

American Chemical Society (ACS)

Subject

Environmental Chemistry,General Chemistry

Link

https://pubs.acs.org/doi/pdf/10.1021/es304744v

Reference75 articles.

1. Amonette, J. E.InElectrochemical Properties of Clays;Fitch, A., Ed.CMS Workshop Lectures; The Clay Minerals Society:Aurora, CO, 2002; Vol.10, pp89–146.

2. Stucki, J. W.InIron in Soils and Clay Minerals;Stucki, J. W., Goodman, B. A., Schwertmann, U., Eds.D. Reidel:Dordrecht, The Netherlands, 1988; pp625–675.

3. Oxidation-reduction Mechanism for Structural Iron in Nontronite1

4. Effects of Reduction and Reoxidation of Structural Iron on the Surface Charge and Dissolution of Dioctahedral Smectites

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