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July 24, 2012Environmental Science & Technology

Redox Properties of Structural Fe in Clay Minerals. 2. Electrochemical and Spectroscopic Characterization of Electron Transfer Irreversibility in Ferruginous Smectite, SWa-1

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Authors

CGChristopher A. GorskiPennsylvania State UniversityLKLaura KlüpfelETH ZurichAVAndreas VoegelinSwiss Federal Institute of Aquatic Science and Technology

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Gorski et al. (2012) studied this question.

synapsesocial.com/papers/6a016f4fbd6301933f5c94f5https://doi.org/10.1021/es302014u
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Also Consider

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  1. 1Spectroscopic Evidence for Interfacial Fe(II)−Fe(III) Electron Transfer in a Clay Mineral2010 · 172 citations
  2. 2Role of Structural Hydrogen in the Reduction and Reoxidation of Iron in Nontronite1985 · 71 citations
  3. 3Use of diffraction and Mössbauer methods for the structural and crystallochemical characterization of nontronites1983 · 90 citations