The coordination environment of 20-200 ppm Pt in yellowish glasses from the CaO-Al 2 O 3 -SiO 2 (CAS) ternary was studied using X-ray absorption fine structure spectroscopy at the Pt-L III edge. Analysis of the Pt-L III edge region suggests that Pt in these glasses is mainly tetravalent and sixfold-coordinated by O (with a mean Pt-O distance of 2.08+ or -0.02 Aa). No evidence for Pt (super 2+) or Pt (super 6+) was found in any of the glasses studied, suggesting that one can not derive valence information easily from solubility data. No second-neighbor contribution was observed around Pt (super 4+) O 6 polyhedra. However, bond-valence modeling suggest that these polyhedra are likely to bond mostly to (super [VI]) Ca (super 2+) , which should promote high positional disorder of second-neighbor cations around Pt. This particular bonding arrangement may explain the relatively high solubility of Pt in these relatively depolymerized melts, as CaPtO 3 -type units.
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October 01, 1999
Structural investigation of platinum solubility in silicate glasses Available to Purchase
Francois Farges;
Francois Farges
Universite de Marne-la-Vallee, Marne-la-Vallee, France
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Daniel R. Neuville;
Daniel R. Neuville
Institute de Physique du Globe de Paris, France
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Gordon E. Brown
Gordon E. Brown
Stanford University, United States
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Francois Farges
Universite de Marne-la-Vallee, Marne-la-Vallee, France
Daniel R. Neuville
Institute de Physique du Globe de Paris, France
Gordon E. Brown
Stanford University, United States
Publisher: Mineralogical Society of America
First Online:
02 Mar 2017
Online ISSN: 1945-3027
Print ISSN: 0003-004X
GeoRef, Copyright 2004, American Geological Institute.
American Geological Institute
American Mineralogist (1999) 84 (10): 1562–1568.
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First Online:
02 Mar 2017
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CitationFrancois Farges, Daniel R. Neuville, Gordon E. Brown; Structural investigation of platinum solubility in silicate glasses. American Mineralogist 1999;; 84 (10): 1562–1568. doi: https://doi.org/10.2138/am-1999-1009
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