Band structure and Fermi surface of rhombohedral and simple graphites

被引:0
作者
Villaquirán, C [1 ]
Gómez, M
Luiggi, N
机构
[1] Univ Cauca, Dept Fis, Popayan, Colombia
[2] Univ Oriente, Nucleo Sucre, Dept Fis, Grp Fis Met, Cumana, Venezuela
来源
PHYSICA STATUS SOLIDI B-BASIC RESEARCH | 2000年 / 220卷 / 01期
关键词
D O I
10.1002/1521-3951(200007)220:1<691::AID-PSSB691>3.0.CO;2-D
中图分类号
O469 [凝聚态物理学];
学科分类号
070205 ;
摘要
Using ab-initio calculation, we have computed the band structure, Fermi surface and other electronic parameters associated with the transport coefficients of graphite for different stackings of carbon layers. Software CRYSTAL was used with a Pople standard STO-21G* basis set. Different Hamiltonians were tested, choosing a restricted Hartree-Fock one, because it generated the best qualitative results. All graphites studied present a Valence bandwidth, near 0.60 a.u., in agreement with the literature; Single layer graphites generate two II bands around of the Fermi level (E-F = -0.438 a.u.). Four IT bands, one being degenerate, appear in hexagonal 3D simple graphite, E-F being equal to -0.00954 a.u. In hexagonal Bernal graphite the splitting of the valence II band was accentuated, and E-F = -0.00140 a.u. Rhombohedral graphite shows a band structure slightly different, with E-F = 0.0381 a.u. Important differences between band structures are reported in the HKH edge according to stacking of graphite layers. The Fermi surface for each graphite type is located near the P point (single layer) or around the HKH edge of the first Brillouin zone (3D graphite). In general such surfaces present a central electron orbit of maximal size in the plane, which diminishes in size when the z component of the k vector moves in KH direction.
引用
收藏
页码:691 / 696
页数:6
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