Observation of a Wurtzite Form of Gallium Arsenide

M. I. McMahon and R. J. Nelmes
Phys. Rev. Lett. 95, 215505 – Published 16 November 2005

Abstract

After a pressure decrease to ambient, the high-pressure SC16 phase of GaAs is found to transform to the hexagonal wurtzite structure. This has been suggested for GaAs in calculations but never previously observed experimentally. Wurtzite-GaAs is found to be stable at ambient pressures at temperatures up to 473 K, with a structure that is only slightly distorted from ideal. On recompression, the c/a ratio is constant with pressure and wurtzite-GaAs transforms to the orthorhombic Cmcm phase at 18.7(9) GPa.

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  • Received 10 June 2005

DOI:https://doi.org/10.1103/PhysRevLett.95.215505

©2005 American Physical Society

Authors & Affiliations

M. I. McMahon and R. J. Nelmes

  • SUPA, School of Physics and Centre for Science at Extreme Conditions, The University of Edinburgh, Mayfield Road, Edinburgh, EH9 3JZ, United Kingdom

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Issue

Vol. 95, Iss. 21 — 18 November 2005

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