The effect of redox state on the local structural environment of iron in silicate glasses:: a molecular dynamics, combined XAFS spectroscopy, and bond valence study

被引:189
作者
Farges, F
Lefrère, Y
Rossano, S
Berthereau, A
Calas, G
Brown, GE
机构
[1] Univ Marne La Vallee, CNRS, Lab Geomat, FRE 2455, F-77454 Marne La Vallee 2, France
[2] Stanford Univ, Dept Geol & Environm Sci, Surface & Aqueous Geochem Grp, Stanford, CA 94305 USA
[3] Univ Paris 06, Lab Mineral Cristallog, F-75252 Paris 05, France
[4] Univ Paris 07, IPGP, F-75252 Paris 05, France
[5] CNRS, UMR 7590, F-75252 Paris 05, France
[6] St Gobain Res, F-93303 Aubervilliers, France
[7] St Gobain Vetrotex, F-73009 Chambery, France
[8] Stanford Synchrotron Radiat Lab, SLAC, Menlo Pk, CA 94025 USA
基金
美国国家卫生研究院; 美国国家科学基金会;
关键词
D O I
10.1016/j.jnoncrysol.2004.07.050
中图分类号
TQ174 [陶瓷工业]; TB3 [工程材料学];
学科分类号
0805 ; 080502 ;
摘要
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. (C) 2004 Elsevier B.V. All rights reserved.
引用
收藏
页码:176 / 188
页数:13
相关论文
共 57 条
[1]   Real-space multiple-scattering calculation and interpretation of x-ray-absorption near-edge structure [J].
Ankudinov, AL ;
Ravel, B ;
Rehr, JJ ;
Conradson, SD .
PHYSICAL REVIEW B, 1998, 58 (12) :7565-7576
[2]   X-RAY MICROPROBE ANALYSIS OF IRON OXIDATION-STATES IN SILICATES AND OXIDES USING X-RAY-ABSORPTION NEAR-EDGE STRUCTURE (XANES) [J].
BAJT, S ;
SUTTON, SR ;
DELANEY, JS .
GEOCHIMICA ET COSMOCHIMICA ACTA, 1994, 58 (23) :5209-5214
[3]   The effect of dissolved water on the oxidation state of silicic melts [J].
Baker, LL ;
Rutherford, MJ .
GEOCHIMICA ET COSMOCHIMICA ACTA, 1996, 60 (12) :2179-2187
[4]   Computer simulation of non-crystalline oxides MeO and Me(2)O(3) [J].
Belashchenko, DK .
JOURNAL OF NON-CRYSTALLINE SOLIDS, 1996, 205 (pt 1) :212-215
[5]   Iron oxidation states in silicate glass fragments and glass inclusions with a XANES micro-probe [J].
Bonnin-Mosbah, M ;
Simionovici, AS ;
Métrich, N ;
Duraud, JP ;
Massare, D ;
Dillmann, P .
JOURNAL OF NON-CRYSTALLINE SOLIDS, 2001, 288 (1-3) :103-113
[6]  
Borisov A.A., 1990, Geochem. Int., V27, P111
[7]  
Brown GE, 1995, REV MINERAL, V32, P317
[8]   BOND-VALENCE PARAMETERS OBTAINED FROM A SYSTEMATIC ANALYSIS OF THE INORGANIC CRYSTAL-STRUCTURE DATABASE [J].
BROWN, ID ;
ALTERMATT, D .
ACTA CRYSTALLOGRAPHICA SECTION B-STRUCTURAL SCIENCE, 1985, 41 (AUG) :244-247
[9]  
Brown Jr G. E., 1978, PROG GEOL SOC AM ANN, V10, P373
[10]  
BUGAEV LA, IN PRESS PHYS SCR