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JOURNALS // Pis'ma v Zhurnal Èksperimental'noi i Teoreticheskoi Fiziki // Archive

Pis'ma v Zh. Èksper. Teoret. Fiz., 2006 Volume 83, Issue 6, Pages 271–276 (Mi jetpl1264)

This article is cited in 20 papers

CONDENSED MATTER

Structure of the intermediate high-pressure phases of ternary lead tellurides

V. V. Shchennikova, S. V. Ovsyannikovab, A. Yu. Manakovc, A. Yu. Likhachevad, A. I. Ancharove, I. F. Bergera, M. A. Sheromovf

a Institute of Metal Physics, Ural Division of the Russian Academy of Sciences
b The Institute for Solid State Physics, The University of Tokyo, Kashiwa, Chiba 277-8581, Japan
c Institute of Inorganic Chemistry, Siberian Branch of the Russian Academy of Sciences
d Institute of Mineralogy and Petrology, Siberian Branch RAS
e Institute of Chemistry of Solid State Siberian Branch RAS
f Institute of Nuclear Physics, Siberian Branch of Russian Academy of Sciences

Abstract: In chambers with diamond anvils, the structure of high-pressure phases of ternary lead tellurides Pb1−x SnxTe (x = 0.29) and Pb1−x MnxTe (x = 0.05) and nonstoichiometric crystals Pb0.55Te0.45, Pb0.45Te0.55 is analyzed by the synchrotron radiation diffraction method at pressures of P up to 14 GPa. The orthorhombic structure of the intermediate high-pressure phase (space group Pnma) is determined for all the samples above 6 GPa. Models of the phase transition in PbTe from the initial rock salt structure to the orthorhombic phase, which constitutes a distorted variant of NaCl, as well as the properties of this phase, are discussed.

PACS: 07.35.+k, 61.10.Nz, 61.50.Ks, 62.50.+p, 81.40.Vw

Received: 10.02.2006


 English version:
Journal of Experimental and Theoretical Physics Letters, 2006, 83:6, 228–232

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