V oxidation state and coordination number in silicate glasses by XAS

被引:76
作者
Giuli, G [1 ]
Paris, E
Mungall, J
Romano, C
Dingwell, D
机构
[1] Univ Camerino, Dipartimento Sci Terra, Camerino, Italy
[2] Univ Toronto, Dept Geol, Toronto, ON, Canada
[3] Univ Roma 3, Dipartimento Sci Geol, Rome, Italy
[4] Univ Munich, Dept Earth Sci, Munich, Germany
[5] Univ Camerino, Unit Ist Nazl Fis Mat, Camerino, Italy
关键词
D O I
10.2138/am-2004-11-1208
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
The local structure of vanadium (V) in synthetic glasses of basaltic composition has been Studied by means of high-resolution V K-edge X-ray absorption near-edge structure (XANES) and extended X-ray absorption fine structure (EXAFS) spectroscopy to obtain quantitative dataon <V-O> distances, V coordination number (CN), and oxidation state. The compositions and experimental conditions were chosen so as to verify the effect of bulk-glass composition (using a diopside-anorthite composition, a sodium disilicate glass, and an iron-titanium-bearing basaltic glass) and V content (from 0.1 to 5 V2O5 wt%) on the structural role of V in these glasses. The combined analysis of high-resolution XANES spectra and EXAFS data indicate that on average, the Fe-free glasses synthesized in air show vanadium in the V5+ state, mainly in tetrahedral coordination (less than 20% V-[5](5+)) and with <V-O> distances of 1.697 ( +/- 0.020) Angstrom, in agreement with the values found for tetrahedral V in minerals. In contrast, the Fe-bearing basaltic glasses display a mixture of V5+ in fourfold and fivefold coordination, 40% V-[4](5+)-60% V-[5](5+) in proportion, and the EXAFS-derived distances and coordination numbers are in agreement with this interpretation. No significant changes in the V local structure were found in the glasses analyzed as a function of V-contents in the 0.1 to 5 V2O5 wt% range. The data obtained suggest that the structural role of vanadium in these melts is rather insensitive to bulk composition, in terms of V and alkali content, but can be strongly affected by the presence of other transition elements, e.g., Fe3+ competing with V to enter the tetrahedral framework.
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页码:1640 / 1646
页数:7
相关论文
共 30 条
[1]   EMPIRICAL CORRECTION FACTORS FOR ELECTRON MICROANALYSIS OF SILICATES AND OXIDES [J].
BENCE, AE ;
ALBEE, AL .
JOURNAL OF GEOLOGY, 1968, 76 (04) :382-&
[2]  
Borisov A. A., 1987, Geochemistry International, V24, P15
[3]  
Brown GE, 1995, REV MINERAL, V32, P317
[4]  
Burns R. G., 1970, MINERALOGICAL APPL C
[5]   COORDINATION OF IRON IN OXIDE GLASSES THROUGH HIGH-RESOLUTION K-EDGE SPECTRA - INFORMATION FROM THE PRE-EDGE [J].
CALAS, G ;
PETIAU, J .
SOLID STATE COMMUNICATIONS, 1983, 48 (07) :625-629
[6]   STRUCTURE OF OXIDE GLASSES - SPECTROSCOPIC STUDIES OF LOCAL ORDER AND CRYSTALLOCHEMISTRY - GEOCHEMICAL IMPLICATIONS [J].
CALAS, G ;
PETIAU, J .
BULLETIN DE MINERALOGIE, 1983, 106 (1-2) :33-55
[7]   Vanadium partitioning between orthopyroxene, spinel and silicate melt and the redox states of mantle source regions for primary magmas [J].
Canil, D .
GEOCHIMICA ET COSMOCHIMICA ACTA, 1999, 63 (3-4) :557-572
[8]   Vanadium partitioning and the oxidation state of Archaean komatiite magmas [J].
Canil, D .
NATURE, 1997, 389 (6653) :842-845
[9]   Vanadium in peridotites, mantle redox and tectonic environments: Archean to present [J].
Canil, D .
EARTH AND PLANETARY SCIENCE LETTERS, 2002, 195 (1-2) :75-90
[10]  
CARMICHAEL ISE, 1990, REV MINERAL, V24, P191