Am. George et al., Cation dynamics and premelting in lithium metasilicate (Li2SiO3) and sodium metasilicate (Na2SiO3): A high-temperature NMR study, AM MINERAL, 83(11-12), 1998, pp. 1277-1284
Premelting effects are common in silicates and have been mostly observed as
significant heat capacity anomalies beginning 100 to 200 degrees C below c
ongruent melting points. To assess the role of cation dynamics in this phen
omenon, we collected nuclear magnetic resonance (NMR) spectra and relaxatio
n time data to within 20 to 50 degrees C of the melting points of sodium me
tasilicate (Na2SiO2), which displays a large premelting effect, and isostru
ctural lithium metasilicate (Li2SiO3), which displays little premelting. Fr
om Li-7 NMR, Li+ site hopping is clearly observed in Li2SiO3 by a partial a
veraging of the Li-7 quadrupolar peak shape, requiring exchange among a few
, ordered orientations of LiO4 tetrahedra. From Na-23 NMR, Na+ site hopping
in Na2SiO3 appears to involve a more liquid-like behavior, implying exchan
ge among many sites with different orientations in a disordered fashion. Fo
r this phase, Si-29 spectra indicate that in an oxidizing environment, no l
iquid phase is present at 20 degrees C below the melting point, well within
the calorimetric premelting regime. However, partial averaging of the low-
temperature, biaxial chemical shift powder pattern (typical of Si sites in
chain silicates) occurs, suggesting some kind of extensive, librational mot
ion of SiO4 tetrahedra that is possibly linked to rapid Na+ diffusion near
the melting point. In contrast to the simple Li+ diffusion in Li2SiO3, this
process may require considerable non-vibrational energy and may thus be re
lated to the heat capacity anomaly just prior to melting.