The influence of temperature on the Ti4+ coordination in sodium titanosilicate melts: In-situ high-temperature Raman spectroscopy study

被引:3
作者
Osipov, Armenak A. [1 ]
Osipova, Leyla M. [1 ]
Liska, Marek [2 ,3 ]
机构
[1] RAS, Inst Mineral, South Urals Fed Res Ctr Mineral & Geoecol, Urals Branch, Miass 456317, Chelyabinsk Reg, Russia
[2] A Dubcek Univ Trencin, FunGlass, Studentska 2, SK-91150 Trencin, Slovakia
[3] FChPT STU, VILA Joined Glass Ctr IIC SAS, TnUAD, Studentska 2, SK-91150 Trencin, Slovakia
关键词
Melt structure; Titanium coordination; Raman spectroscopy; SILICATE-GLASSES; BEHAVIOR; SPECTRA; NA;
D O I
10.1016/j.vibspec.2021.103308
中图分类号
O65 [分析化学];
学科分类号
070302 ; 081704 ;
摘要
The structure of xTiO(2)-(100-x)[40Na(2)O-60SiO(2)] (x = 10, 15, 25 and 30 mol%) glasses and melts was studied in situ in the temperature range of 20-1150 degrees C using high-temperature Raman spectroscopy. The fraction of five-fold coordinated Ti4+ ions gradually decreases as temperature increases above similar to 600 degrees C in the samples with x <= 25 mol%. No similar changes were found for the sample with x = 30 mol%. The change in titanium coordination is related to the transformation of square-based TiO5 pyramids into TiO4 tetrahedra with the formation of additional non-bridging oxygen atoms (NBO) in the melt structure. This transformation can be described by [TiO4O](2-) + SiO3O- <-> TiO3O- + SiO2O22- and [TiO4O](2-) + SiO4 <-> TiO3O- + SiO3O- (O is bridging oxygen atom) disproportional reactions, which are shifted toward the right with increasing temperature. All studied melts exhibit a more uniform titanium distribution in comparison with glasses of corresponding composition.
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页数:6
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