K. Suito et al., THERMAL-EXPANSION STUDIES OF STISHOVITE AT 10.5 GPA USING SYNCHROTRON-RADIATION, Physics of the earth and planetary interiors, 93(3-4), 1996, pp. 215-222
The thermal expansion of stishovite has been studied in situ under pre
ssure at 10.5(8) GPa and in the temperature range from 20 degrees C to
1000 degrees C using a cubic type apparatus combined with synchrotron
radiation. The linear thermal expansivities along the crystallographi
c a- and c-axes at 10.5(8) GPa and 20 degrees C are alpha(a) = 0.4978(
1) x 10(-6) K-1 and alpha(c) = 3.155(2) x 10(-6) K-1, respectively. Th
e volume thermal expansivity for the same pressure-temperature conditi
ons is alpha(v) = 4.080(4) x 10(-6) K-1. The Anderson-Gruneisen parame
ter, delta(T), at 10.5(8) GPa decreases with increasing temperature fr
om 55 at 20 degrees C to 15 at 1000 degrees C, and approaches five whe
n extrapolated to 1500 degrees C.