arXiv · cond-mat/0502510
Quantum Monte Carlo calculations of the structural properties and the B1-B2 phase transition of MgO
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 rock-salt 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 rock-salt and CsCl structures) is predicted to be just below 600 GPa, which is beyond the experimentally accessible range, in accord with other predictions based on Hartree-Fock and density functional theories.
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D. Alfè, M. Alfredsson, J. Brodholt, M. J. Gillan M. D. Towler, R. J. Needs. 2005-02-21. Quantum Monte Carlo calculations of the structural properties and the B1-B2 phase transition of MgO. https://doi.org/10.1103/physrevb.72.014114
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