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Title: Structural Evolution, Strain and Elasticity of Perovskites at High Pressures and Temperatures

Journal Article · · Journal of Mineral and Petrological Sciences

Analysis of pressure-temperature dependent monochromatic X-ray powder diffraction data yield the bulk modulus [KT = 180.2(28) GPa] and thermal expansion coefficients [{alpha}0 = 2.841(34) x 10-5 K-1; {alpha}1 = 3.37(48) x 10-9 K-2] of CaIrO3, the structure model for post-perovskite MgSiO3. CaIrO3 is orthorhombic (Cmcm, space group 63, Z = 4) with best-fit unit-cell parameters, a = 3.14147(5) Angstroms, b = 9.87515(19), c = 7.29711(11), and V = 226.3754(78) Angstroms 3 at 1 bar and 300 K. The c-axis of CaIrO3 has a small compressibility and a large thermal expansion when compared to the other principal axes. Rietveld structure refinement reveals changes in CaIrO3 as a function of temperature in terms of IrO6 octahedra distortion. Dissociation of CaIrO3 at high temperature has possible implications for the post-perovskite MgSiO3 structure, Earth's lower mantle, and D' layer.

Research Organization:
Brookhaven National Lab. (BNL), Upton, NY (United States). National Synchrotron Light Source
Sponsoring Organization:
Doe - Office Of Science
DOE Contract Number:
DE-AC02-98CH10886
OSTI ID:
960062
Report Number(s):
BNL-83048-2009-JA; TRN: US201016%%1206
Journal Information:
Journal of Mineral and Petrological Sciences, Vol. 101
Country of Publication:
United States
Language:
English