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American Mineralogist; October; v. 93; no. 10; p. 1654-1658; DOI: 10.2138/am.2008.2938
© 2008 Mineralogical Society of America
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Raman spectroscopy of CaIrO3 postperovskite up to 30 GPa

Justin Hustoft1,*, Sang-Heon Shim1,{dagger}, Atsushi Kubo2 and Norimasa Nishiyama2,{ddagger}

1 Department of Earth, Atmospheric, and Planetary Sciences, Massachusetts Institute of Technology, Cambridge, Massachusetts 02139, U.S.A.
2 Center for Advanced Radiation Sources, University of Chicago, Chicago, Illinois 60637, U.S.A.

Correspondence: {dagger} E-mail: sangshim{at}mit.edu

We have measured Raman spectra of the postperovskite (PPv) phase in CaIrO3 up to 30 GPa to constrain the Grüneisen parameter ({gamma}). We identified a total of 4 strong modes between 200 and 650 cm–1, which is in contrast with the Raman spectra of Mn2O3 and MgGeO3-PPv where at least nine different modes have been detected. We found no sign of a phase transition in the Raman spectra of PPv CaIrO3, which supports the stability of the PPv phase up to 30 GPa and room temperature in CaIrO3. The spectroscopic Grüneisen parameter, {gamma}sp,0 = 1.66~1.72, constrained from our Raman data, is in excellent agreement with the thermodynamic Grüneisen parameter, {gamma}th,0 = 1.75 ± 0.05, calculated from recent XRD measurements (Martin et al. 2007) on CaIrO3-PPv synthesized at high pressure and temperature similar to our starting material. Our result suggests that {gamma}sp constrained by Raman measurements provides a reasonable estimate on the {gamma}th of the PPv phase in CaIrO3.

Key Words: Postperovskite • CaIrO3 • Gruneisen parameter • Raman sepctroscopy • thermal equation of state




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R. Zucker and S.-H. Shim
In situ Raman spectroscopy of MgSiO3 enstatite up to 1550 K
American Mineralogist, November 1, 2009; 94(11-12): 1638 - 1646.
[Abstract] [Full Text] [PDF]




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