Quasiparticle self-consistent GW calculations for PbS, PbSe, and PbTe: Band structure and pressure coefficients

被引:130
作者
Svane, A. [1 ]
Christensen, N. E. [1 ]
Cardona, M. [2 ]
Chantis, A. N. [3 ]
van Schilfgaarde, M. [4 ]
Kotani, T. [5 ]
机构
[1] Aarhus Univ, Dept Phys & Astron, DK-8000 Aarhus C, Denmark
[2] Max Planck Inst Festkorperforsch, D-70569 Stuttgart, Germany
[3] Los Alamos Natl Lab, Div Theoret, Los Alamos, NM 87545 USA
[4] Arizona State Univ, Sch Mat, Tempe, AZ 85287 USA
[5] Tottori Univ, Dept Appl Phys & Math, Tottori 6808552, Japan
基金
美国国家科学基金会;
关键词
2ND VALENCE-BAND; PHASE-TRANSITIONS; LEAD; CHALCOGENIDES; DIFFRACTION; DENSITIES; TRANSPORT; STATES;
D O I
10.1103/PhysRevB.81.245120
中图分类号
T [工业技术];
学科分类号
08 ;
摘要
The electronic band structures of PbS, PbSe, and PbTe in the rocksalt structure are calculated with the quasiparticle self-consistent GW (QSGW) approach with spin-orbit coupling included. The semiconducting gaps and their deformation potentials as well as the effective masses are obtained. The GW approximation provides a correct description of the electronic structure around the gap, in contrast to the local-density approximation, which leads to inverted gaps in the lead chalcogenides. The QSGW calculations are in good quantitative agreement with experimental values of the gaps and masses. At moderate hole doping a complex filamental Fermi-surface structure develops with ensuing large density of states. The pressure-induced gap closure leads to linear (Dirac-type) band dispersions around the L point.
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页数:10
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