DOES 6-COORDINATE GERMANIUM EXIST IN NA2O-GEO2 GLASSES - O-17 NUCLEAR-MAGNETIC-RESONANCE MEASUREMENTS

Citation
R. Hussin et al., DOES 6-COORDINATE GERMANIUM EXIST IN NA2O-GEO2 GLASSES - O-17 NUCLEAR-MAGNETIC-RESONANCE MEASUREMENTS, Journal of non-crystalline solids, 234, 1998, pp. 440-445
Citations number
25
Categorie Soggetti
Material Science, Ceramics
ISSN journal
00223093
Volume
234
Year of publication
1998
Pages
440 - 445
Database
ISI
SICI code
0022-3093(1998)234:<440:D6GEIN>2.0.ZU;2-1
Abstract
Sodium germanate glasses of compositions Na2O . 9GeO(2) and 2Na(2)O . 9GeO(2) have been studied using solid-state O-17 nuclear magnetic reso nance (NMR). Quartz-type and rutile-type GeO2 were used as examples of oxygen connected to 4-fold and 6-fold coordinated germanium. The O-17 spectra yielded nuclear quadrupole coupling constants, (e(2)qQ/h), as ymmetry parameters, (eta) and isotropic chemical shifts, (delta(i)): f rom line shape simulations. The chemical shifts of oxygen in [GeO4] an d [GeO6] units in germania are 70 +/- 5 and 160 +/- 5 ppm, respectivel y, with only a small difference in the quadrupole coupling constant bu t a larger difference in the asymmetry parameter. In the Na2O-GeO2 gla sses, the quadrupole coupling constant decreases with addition of Na2O to the glass with no evidence for any oxygen with a smaller electric field gradient, indicating that there are very few non-bridging oxygen s (NBOs) present-The O-17 chemical shift in Na2O . 9GeO(2) is similar to that in [GeO6] while in 2Na(2)O . 9GeO(2) the chemical shift is clo se to that of [GeO4]. (C) 1998 Elsevier Science B.V. All rights reserv ed.