Quantum Monte Carlo calculations of the structural properties and the B1-B2 phase transition of MgO

D. Alfè, M. Alfredsson, J. Brodholt, M. J. Gillan, M. D. Towler, and R. J. Needs
Phys. Rev. B 72, 014114 – Published 14 July 2005

Abstract

We report diffusion Monte Carlo (DMC) calculations on MgO in the rock-salt and CsCl structures. The calculations are based on Hartree-Fock pseudopotentials, with the single-particle orbitals entering the correlated wave function being represented by a systematically convergeable cubic-spline basis. Systematic tests are presented on system-size errors using periodically repeating cells of up to over 600 atoms. The equilibrium lattice parameter of the rocksalt structure obtained within DMC is almost identical to the Hartree-Fock result, which is close to the experimental value. The DMC result for the bulk modulus is also in good agreement with the experimental value. The B1-B2 transition pressure (between the rocksalt and CsCl structures) is predicted to be just below 600GPa, which is beyond the experimentally accessible range, in accord with other predictions based on Hartree-Fock and density functional theories.

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  • Received 21 February 2005

DOI:https://doi.org/10.1103/PhysRevB.72.014114

©2005 American Physical Society

Authors & Affiliations

D. Alfè1,2, M. Alfredsson1, J. Brodholt1, M. J. Gillan2, M. D. Towler3, and R. J. Needs3

  • 1Department of Earth Sciences, University College London, Gower Street, London WC1E 6BT, United Kingdom
  • 2Department of Physics and Astronomy, University College London, Gower Street, London WC1E 6BT, United Kingdom
  • 3Theory of Condensed Matter Group, Cavendish Laboratory, University of Cambridge, Cambridge CB3 0HE, United Kingdom

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Vol. 72, Iss. 1 — 1 July 2005

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