Polarized EXAFS, distance-valence least-squares modeling (DVLS), and quantitative texture analysis approaches to the structural refinement of Garfield nontronite

被引:133
作者
Manceau, A [1 ]
Chateigner, D
Gates, WP
机构
[1] Univ Grenoble 1, LGIT IRIGM, Environm Geochem Grp, F-38041 Grenoble 9, France
[2] CNRS, F-38041 Grenoble, France
[3] Univ Grenoble 1, CNRS, Lab Cristallog, F-38042 Grenoble 9, France
关键词
D O I
10.1007/s002690050125
中图分类号
T [工业技术];
学科分类号
08 ;
摘要
This paper reports on the new application of polarized extended X-ray absorption fine structure (P-EXAFS) spectroscopy to fine-grained layer silicates taking the Garfield nontronite as a case study. Up to now application of P-EXAFS to structural studies of layer silicates has been restricted to single phyllosilicate crystals (Manceau et al. 1988; Manceau et al. 1990), but we show here that P-EXAFS can rigorously be applied to self-supporting clay films without loss of spatial resolution. The quantitative analysis of P-EXAFS requires however the preparation of highly oriented clay films, the orientation distribution of which can be assessed by texture goniometry. The Fe K-edge linear dichroism measurements were simulated by ab initio EXAFS modeling performed on a nontronite cluster whose structure was refined by distance-valence least-squares calculations. It is shown that nb initio modeling quantitatively accounts for the angular dependence of experimental EXAFS spectra. These calculations allowed for the identification of the fundamental character of single-and multiple-scattering paths of the photoelectron, and the structural interpretation of all spectral features observed up to 6.5 Angstrom for the in-plane and out-of-plane radial structure functions of nontronite. In practice, P-EXAFS measurements allow the determination of the flattening angle of Fe(O,OH)(6) octahedra, cations distribution in the octahedral sheet with an enhanced sensitivity, and differentiation between dioctahedral and trioctahedral structures.
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页码:347 / 365
页数:19
相关论文
共 53 条
[41]   THEORETICAL X-RAY ABSORPTION FINE-STRUCTURE STANDARDS [J].
REHR, JJ ;
DELEON, JM ;
ZABINSKY, SI ;
ALBERS, RC .
JOURNAL OF THE AMERICAN CHEMICAL SOCIETY, 1991, 113 (14) :5135-5140
[42]   HIGH-ORDER MULTIPLE-SCATTERING CALCULATIONS OF X-RAY-ABSORPTION FINE-STRUCTURE [J].
REHR, JJ ;
ALBERS, RC ;
ZABINSKY, SI .
PHYSICAL REVIEW LETTERS, 1992, 69 (23) :3397-3400
[43]   NMR APPLIED TO MINERALS .5. THE LOCALIZATION OF VACANCIES IN THE OCTAHEDRAL SHEET OF ALUMINOUS BIOTITES [J].
SANZ, J ;
DELACALLE, C ;
STONE, WEE .
PHYSICS AND CHEMISTRY OF MINERALS, 1984, 11 (05) :235-240
[45]  
Stern E. A., 1983, Handbook on synchrotron radiation, P955
[46]   THICKNESS EFFECT ON THE EXTENDED-X-RAY-ABSORPTION-FINE-STRUCTURE AMPLITUDE [J].
STERN, EA ;
KIM, K .
PHYSICAL REVIEW B, 1981, 23 (08) :3781-3787
[47]  
Stohr J., 2013, NEXAFS SPECTROSCOPY
[48]  
STUCKI JW, 1988, NATO ASI SER, V217, P625
[49]  
TAKEDA H, 1975, AM MINERAL, V60, P1030
[50]   THE DISTRIBUTION OF OCTAHEDRAL CATIONS IN THE 2-1 LAYERS OF DIOCTAHEDRAL SMECTITES STUDIED BY OBLIQUE-TEXTURE ELECTRON-DIFFRACTION [J].
TSIPURSKY, SI ;
DRITS, VA .
CLAY MINERALS, 1984, 19 (02) :177-193