Negative PT slopes characterize phase change processes: Case of the Ge1Sb2Te4 phase change alloy

B. Kalkan, S. Sen, B. G. Aitken, S. V. Raju, and S. M. Clark
Phys. Rev. B 84, 014202 – Published 29 July 2011

Abstract

The crystalline, liquid and amorphous phase stabilities and transformations of the Ge1Sb2Te4 (GST124) alloy are investigated as a function of pressure and temperature using synchrotron diffraction experiments in a diamond anvil cell. The results indicate that the solid-state amorphization of the cubic GST124 phase under high pressure may correspond to a metastable extension of the stability field of the GST124 liquid along a hexagonal crystal-liquid phase boundary with a negative P-T slope. The internal pressures generated during phase change are shown to be too small to affect phase stability. However, they may be important in understanding reliability issues related to thermomechanical stress development in phase change random access memory structures.

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  • Received 13 June 2011

DOI:https://doi.org/10.1103/PhysRevB.84.014202

©2011 American Physical Society

Authors & Affiliations

B. Kalkan1, S. Sen2,*, B. G. Aitken3, S. V. Raju1, and S. M. Clark1,4

  • 1Advanced Light Source, Lawrence Berkeley Laboratory, Berkeley, California 20015, USA
  • 2Department of Chemical Engineering and Materials Science, University of California, Davis, California 95616, USA
  • 3Glass Research Division, SP-FR-05, Corning Incorporated, Corning, New York 14831, USA
  • 4Department of Earth and Planetary Sciences, University of California, Berkeley, California 94720, USA

  • *Corresponding author. sbsen@ucdavis.edu

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Vol. 84, Iss. 1 — 1 July 2011

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