Pre-melting hcp to bcc Transition in Beryllium

ORAL

Abstract

Beryllium (Be) is an important material with wide applications ranging from aerospace components to x-ray ray equipment. Yet a precise understanding of its phase diagram remains elusive. We have investigated the phase stability of Be using a recently developed hybrid free-energy computation method that accounts for anharmonic effects by invoking phonon quasiparticles. We find that the hcp → bcc transition occurs near the melting curve at 0 < P < 11 GPa with a positive Clapeyron slope of 41(4) K/GPa, a result that is more consistent with recent experimental measurements. This work also demonstrates the validity of this theoretical framework based on the phonon gas model and phonon quasiparticle to study phase transitions in strongly anharmonic materials.

Presenters

  • Renata Wentzcovitch

    Department of Applied Physics and Applied Mathematics and Department of Earth and Environmental Sciences, Lamont Doherty Earth Observatory, Columbia University, Applied Physics and Mathematics, Columbia University, Columbia Univ, Applied Physics and Applied Mathematics, Columbia University, Columbia University, Department of Applied Physics and Applied Mathematics, Department of Earth and Environmental Sciences, Lamont Doherty Earth Observatory, Columbia University

Authors

  • Dong-Bo Zhang

    Condensed Matter, Beijing Computational Science Research Center, Condensed Matter , Beijing Computational Science Research Center, Beijing Computational Science Research Center

  • Peihong Zhang

    Physics, State University of New York, State Univ of NY - Buffalo, State Univ of New York at Buffalo

  • Renata Wentzcovitch

    Department of Applied Physics and Applied Mathematics and Department of Earth and Environmental Sciences, Lamont Doherty Earth Observatory, Columbia University, Applied Physics and Mathematics, Columbia University, Columbia Univ, Applied Physics and Applied Mathematics, Columbia University, Columbia University, Department of Applied Physics and Applied Mathematics, Department of Earth and Environmental Sciences, Lamont Doherty Earth Observatory, Columbia University