Jf. Stebbins et Bt. Poe, Pentacoordinate silicon in high-pressure crystalline and glassy phases of calcium disilicate (CaSi2O5), GEOPHYS R L, 26(16), 1999, pp. 2521-2523
We report Si-29 MAS NMR spectra for the monoclinic and triclinic crystallin
e phases of CaSi2O5. The latter, which is now known from single crystal x-r
ay diffraction to contain pentacoordinate silicon (SiO5 or Si-[5]) units, h
as an NMR peak for this group near to -150 ppm, for the first time definiti
vely confirming previous peak assignments in the spectra of ambient and hig
h-pressure glasses. This result, and new data on a CaSi2O5 glass quenched f
rom a liquid at 2300 degrees C, 10 GPa, demonstrate that Si-[5] groups, alo
ng with SiO6 (Si-[6]) units, form at high pressures in silicate liquids wit
h abundant non-bridging oxygens, and are thus likely to be important for th
e properties such as viscosity and density of mafic to ultramafic magmas in
nature.