Structure of the intermediate phase of PbTe at high pressure

G. Rousse, S. Klotz, A. M. Saitta, J. Rodriguez-Carvajal, M. I. McMahon, B. Couzinet, and M. Mezouar
Phys. Rev. B 71, 224116 – Published 29 June 2005

Abstract

The evolution of PbTe with pressure has been reexamined using synchrotron x-ray diffraction. The phase transition at 6 GPa is not to the GeS (B16) or TlI (B33) type structures, as previously reported, but to an orthorhombic Pnma structure, with cell parameters a=8.157(1), b=4.492(1), and c=6.294(1)Å at 6.7 GPa. This structure corresponds to a distortion of the low-pressure NaCl structure with a coordination intermediate between the sixfold B1 (NaCl) and the eightfold B2 (CsCl) structure. We discuss the stability of this new structure with respect to other proposed phases using numerical methods. These results may modify the admitted paths of phase transitions between the B1 and B2 structures.

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  • Received 19 November 2004

DOI:https://doi.org/10.1103/PhysRevB.71.224116

©2005 American Physical Society

Authors & Affiliations

G. Rousse1,*, S. Klotz1, A. M. Saitta1, J. Rodriguez-Carvajal2, M. I. McMahon3, B. Couzinet1, and M. Mezouar4

  • 1Physique des Milieux Denses, Institut de Minéralogie et de Physique des Milieux Condensés, CNRS UMR 7590–Universités Paris 6-Paris 7-IPGP, Campus Boucicaut, 140 Rue de Lourmel, 75015 Paris, France
  • 2Laboratoire Léon Brillouin (CEA-CNRS), CEA/Saclay, 91191 Gif sur Yvette Cedex, France
  • 3School of Physics and Centre for Science at Extreme Conditions, The University of Edinburgh, Kings Buildings, Edinburgh EH9 3JZ, United Kingdom
  • 4European Synchrotron Radiation Facility, Boîte Postale 220, 38042 Grenoble, France

  • *Corresponding author. Email address: gr@pmc.jussieu.fr

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Vol. 71, Iss. 22 — 1 June 2005

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