The effect of redox state on the local structural environment of iron in silicate glasses: a combined XAFS spectroscopy, molecular dynamics, and bond valence study |
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Authors: | Franç ois Farges,Yannick Lefrè re,Sté phanie Rossano,Georges Calas |
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Affiliation: | a Laboratoire des géomatériaux, FRE CNRS 2455, Université de Marne-la-Vallée, Cité Descartes - Champs S/Marne, 77454 Marne la Vallée cedex 2, France b Surface and Aqueous Geochemistry Group, Department of Geological and Environmental Sciences, Stanford University, Stanford, CA 94305-2115, USA c Laboratoire de Minéralogie-Cristallographie, Universités de Paris 6 et 7, IPGP and UMR, CNRS 7590, 2 place Jussieu, 75252 Paris cedex 05, France d Saint Gobain Recherche, 39 quai Lefranc, BP 135, 93303 Aubervilliers cedex, France e Saint Gobain Vetrotex, 767 quai des Allobroges, BP 929, 73009 Chambéry cedex, France f Stanford Synchrotron Radiation Laboratory, SLAC, 2575 Sand Hill Rd., MS 69, Menlo Park, CA 94025, USA |
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Abstract: | A series of 27 silicate glasses of various compositions containing 0.2-2 at.% iron were synthesized at various oxygen fugacity values. The glasses were examined using X-ray absorption fine structure (XANES) spectroscopy at the Fe K-edge in order to determine iron oxidation state and first-neighbor coordination number. Spectral information extracted from the pre-edge region and principal component analysis (PCA) of the XANES region, together with a spectral inversion, were used to derive the end-member spectral components for Fe(II) and Fe(III). Linear trends in the pre-edge features were observed for most compositional series of the glasses examined as a function of Fe(II)/Fe(III) content. These linear trends are believed to be due to the similarity of average coordination numbers for both Fe(II) and Fe(III) end-members in each series. This result is consistent with model simulations of the XANES region and molecular dynamics (MD) simulations for the two end-member compositions which also show that Fe(II) and Fe(III) have similar average coordination numbers. These simulations also suggest the presence of five-coordinated Fe(III) in the melt phase. Based on a bond valence analysis of these MD simulations, a simple model is proposed to help predict the speciation of iron in oxide and silicate glasses and melts. |
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Keywords: | O160 S440 X120 M291 |
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