Observation of a Pressure-Induced First-Order Polyamorphic Transition in a Chalcogenide Glass at Ambient Temperature

S. Sen, S. Gaudio, B. G. Aitken, and C. E. Lesher
Phys. Rev. Lett. 97, 025504 – Published 14 July 2006

Abstract

An apparently first-order polyamorphic transition has been observed with increasing pressure at ambient temperature in a molecular glass of composition Ge2.5As51.25S46.25. Raman spectroscopic measurements on pressure-quenched samples and in situ x-ray diffraction measurements indicate that this transition corresponds to a collapse of the ambient-pressure molecular phase to a high-pressure network phase. The high-pressure phase first appears at a pressure of 89GPa and the transformation becomes complete at 1415GPa. Calorimetric measurements indicate that the low- and high-pressure phases are thermodynamically distinct and that they coexist in the transition range.

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  • Received 22 April 2006

DOI:https://doi.org/10.1103/PhysRevLett.97.025504

©2006 American Physical Society

Authors & Affiliations

S. Sen1, S. Gaudio2, B. G. Aitken3, and C. E. Lesher2

  • 1Department of Chemical Engineering and Materials Science, University of California, Davis, California 95616, USA
  • 2Department of Geology, University of California, Davis, California 95616, USA
  • 3Glass Research Division, SP-FR-05-1, Corning Incorporated, Corning, New York 14831, USA

Comments & Replies

Comment on “Observation of a Pressure-Induced First-Order Polyamorphic Transition in a Chalcogenide Glass at Ambient Temperature”

Vadim Brazhkin
Phys. Rev. Lett. 98, 069601 (2007)

Sen et al. Reply:

S. Sen, S. Gaudio, B. G. Aitken, and C. E. Lesher
Phys. Rev. Lett. 98, 069602 (2007)

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Vol. 97, Iss. 2 — 14 July 2006

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