Phase relations and hardness trends of ZrO2 phases at high pressure

Yahya Al-Khatatbeh, Kanani K. M. Lee, and Boris Kiefer
Phys. Rev. B 81, 214102 – Published 3 June 2010

Abstract

We use high-resolution synchrotron x-ray powder diffraction and density-functional theory (DFT) to investigate the phase stability, equations of state (EOSs), and mechanical hardness of zirconia (ZrO2) up to 54 and 160 GPa, respectively. For the equilibrium phase at ambient conditions (MI), we provide an experimental EOS that is comparable to results obtained from room-pressure Brillouin scattering experiments and bulk modulus-volume systematics but different from previous high-pressure experiments. The experimental second-order Birch-Murnaghan EOS parameters of MI-ZrO2 are: ambient-pressure volume (V0) of 35.15(±0.03)Å3/f.u. with an ambient-pressure bulk modulus K0 of 210(±28)GPa. For the high-pressure OI phase, we find that the K0=290(±11)GPa, which is 19%–32% higher than previously determined, and V0=33.65(±0.07)Å3/f.u. The small volume decrease of 3.4% across the MIOI transition at 10GPa is associated with a 38% increase in the bulk modulus consistent with our DFT calculations that predict a 36% and 39% increase in K0 for the generalized gradient and local density approximations, respectively. In contrast to the EOS of MI and OI, we find that our experimental EOS for the high-pressure OII phase is in good agreement with previous measurements. The large volume decrease across the OIOII phase transition as obtained from both our experiments and calculations is 10%. Our estimates, using scaling relations, indicate that this phase, while dense and quenchable, may have a comparatively low mechanical hardness of 10GPa.

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  • Received 28 December 2009

DOI:https://doi.org/10.1103/PhysRevB.81.214102

©2010 American Physical Society

Authors & Affiliations

Yahya Al-Khatatbeh1, Kanani K. M. Lee1,2, and Boris Kiefer1

  • 1Department of Physics, New Mexico State University, Las Cruces, New Mexico 88003-8001, USA
  • 2Department of Geology and Geophysics, Yale University, New Haven, Connecticut 06511, USA

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Vol. 81, Iss. 21 — 1 June 2010

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