Abstract
IR reflectance and absorbance spectra obtained from polycrystalline and single-crystal perovskites of MgSiO3 and (Mg0.9Fe0.1 )SiO3 compositions yielded virtually all the expected fundamental modes. Near-IR absorbance spectra indicate that the polycrystals were anhydrous, whereas the single crystal contained about 0.06 wt% H2O. A Kieffer-type model was used to calculate heat capacity, entropy, and Debye temperature for the orthorhombic perovskite phase. -from Authors
| Original language | English |
|---|---|
| Pages (from-to) | 11,795-11,804 |
| Journal | Journal of Geophysical Research: Biogeosciences |
| Volume | 99 |
| Issue number | B6 |
| State | Published - 1994 |