Phase transformation in Si from semiconducting diamond to metallic β-Sn phase in QMC and DFT under hydrostatic and anisotropic stress

被引:64
|
作者
Hennig, R. G. [1 ,2 ]
Wadehra, A. [2 ]
Driver, K. P. [2 ]
Parker, W. D. [2 ]
Umrigar, C. J. [3 ]
Wilkins, J. W. [2 ]
机构
[1] Cornell Univ, Dept Mat Sci & Engn, Ithaca, NY 14853 USA
[2] Ohio State Univ, Dept Phys, Columbus, OH 43210 USA
[3] Cornell Univ, Atom & Solid State Phys Lab, Ithaca, NY 14853 USA
基金
美国国家科学基金会;
关键词
GENERALIZED GRADIENT APPROXIMATION; HIGH-PRESSURE PHASES; ELECTRON-GAS; SILICON; TRANSITION; ENERGY; SIMULATIONS; DEPENDENCE; ACCURATE;
D O I
10.1103/PhysRevB.82.014101
中图分类号
T [工业技术];
学科分类号
08 ;
摘要
Silicon undergoes a phase transition from the semiconducting diamond phase to the metallic beta-Sn phase under pressure. We use quantum Monte Carlo calculations to predict the transformation pressure and compare the results to density-functional calculations employing the local-density approximation, the generalized-gradient approximations PBE, PW91, WC, AM05, PBEsol, and the hybrid functional HSE06 for the exchange-correlation functional. Diffusion Monte Carlo predicts a transition pressure of 14.0 +/- 1.0 GPa slightly above the experimentally observed transition pressure range of 11.3-12.6 GPa. The HSE06 hybrid functional predicts a transition pressure of 12.4 GPa in excellent agreement with experiments. Exchange-correlation functionals using the local-density approximation and generalized-gradient approximations result in transition pressures ranging from 3.5 to 10.0 GPa, well below the experimental values. The transition pressure is sensitive to stress anisotropy. Anisotropy in the stress along any of the cubic axes of the diamond phase of silicon lowers the equilibrium transition pressure and may explain the discrepancy between the various experimental values as well as the small overestimate of the quantum Monte Carlo transition pressure.
引用
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页数:9
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