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
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.