Abstract
Although it has been well accepted that F-Al linkages dominate in F-bearing alkali aluminosilicate glasses, the possibility of F-Si linkages remains unresolved. Recent 19F NMR results have been interpreted as indicative of not only the presence of the Al-F-Na(n) linkages but also of the presence of Si-F-Na(n) linkages. High level ab initio NMR calculations were performed to investigate the nature of possible species contributing to the 19F spectra. The B3LYP/6-31G * level was used to optimize structures and a scaling technique applied to the calculation of NMR properties using both HF and B3LYP methods at the 6-311 +G(2df,p) level. The applicability of this scaling method was checked by comparing calculated results against experimental data on several crystalline materials: the results are improved over HF or DFT methods alone. The calculation results show that none of the F-Al species investigated can produce the - 147 ppm peak of Schaller et al. (1992). However, several species in which F is bonded to fourfold-, fivefold-, and sixfold-coordinated Si produce a19F chemical shift of approximately - 147 ppm. These results verify the assignments of this peak by Zeng and Stebbins (2000) to tetrahedral Si-F and NaSiF6-like species, and rule out may other possible species. Several additional species such as a fivefold coordinated Si-F species may further contribute to the - 147 ppm 19F peak.
| Original language | English |
|---|---|
| Pages (from-to) | 339-346 |
| Number of pages | 8 |
| Journal | American Mineralogist |
| Volume | 87 |
| Issue number | 2-3 |
| DOIs | |
| State | Published - 2002 |
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