Rietveld refinement study of the pressure dependence of the internal structural parameter u in the wurtzite phase of ZnO

Haozhe Liu, Yang Ding, Maddury Somayazulu, Jiang Qian, Jinfu Shu, Daniel Häusermann, and Ho-kwang Mao
Phys. Rev. B 71, 212103 – Published 27 June 2005

Abstract

The pressure dependence of the internal structural parameter u of the wurtzite phase of ZnO was studied using high resolution angular dispersive x-ray diffraction up to 12 GPa in a helium pressure medium. The u parameter increases with pressure up to about 0.430 at about 5.6 GPa, and then rapidly decrease to about 0.380 during the phase transition. Two models of the phase transition path were proposed recently by first-principles calculations [A. M. Saitta and F. Decremps, Phys. Rev. B 70, 035214 (2004); S. Limpijumnong and S. Jungthawan, Phys. Rev. B 70, 054104 (2004)]. These possible mechanisms responsible for the wurtzite-to-rocksalt phase transition under high pressure are experimentally evaluated based on our results. The bulk moduli of the wurtzite and rocksalt phase at zero pressure were estimated as 135.3±1.8 and 177.4±4.6GPa, respectively.

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  • Received 15 February 2005

DOI:https://doi.org/10.1103/PhysRevB.71.212103

©2005 American Physical Society

Authors & Affiliations

Haozhe Liu1,2, Yang Ding2, Maddury Somayazulu1,2, Jiang Qian3, Jinfu Shu2, Daniel Häusermann1,2, and Ho-kwang Mao1,2

  • 1HPCAT, Advanced Photon Source, Building 434E, Argonne National Laboratory, Argonne, Illinois 60439, USA
  • 2Geophysical Laboratory, Carnegie Institution of Washington, Washington, DC 20015, USA
  • 3Lujan Neutron Scattering Center, Los Alamos National Laboratory, MS-H805, Los Alamos, New Mexico 87545, USA

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Issue

Vol. 71, Iss. 21 — 1 June 2005

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