Xy. Xue et Jf. Stebbins, NA-23 NMR CHEMICAL-SHIFTS AND LOCAL NA COORDINATION ENVIRONMENTS IN SILICATE CRYSTALS, MELTS AND GLASSES, Physics and chemistry of minerals, 20(5), 1993, pp. 297-307
In order to decipher information about the local coordination environm
ents of Na in anhydrous silicates from Na-23 nuclear magnetic resonanc
e spectroscopy (NMR), we have collected Na-23 magic angle spinning (MA
S) NMR spectra on several sodium-bearing silicate and aluminosilicate
crystals with known structures. These data, together with those from t
he literature, suggest that the Na-23 isotropic chemical shift correla
tes well with both the Na coordination and the degree of polymerizatio
n (characterized by NBO/T) of the material. The presence of a dissimil
ar network modifier also affects the Na-23 isotropic chemical shift. F
rom these relations, we found that the average Na coordinations in sod
ium silicate and aluminosilicate liquids of a range of compositions at
1 bar are nearly constant at around 6-7. The average Na coordinations
in glasses of similar compositions also vary little with Na content (
degree of polymerization). However, limited data on ternary alkali sil
icate and aluminosilicate glasses seem to suggest that the introductio
n of another network-modifier, such as K or Cs, does cause variations
in the average local Na coordination. Thus it appears that the average
Na coordination environments in silicate glasses are more sensitive t
o the presence of other network-modifiers than to the variations in th
e topology of the silicate tetrahedral network. Further studies on sil
icate glasses containing mixed cations are necessary to confirm this c
onclusion.