The effects of hydrostatic pressure on the electronic band structure of the semiconductor mineral iron
pyrite FeS2
have been investigated theoretically by an ab initio full-potential linearized-augmented plane
wave (FPLAPW) method within a local approximation (LDA/GGA) to the density functional
theory. The calculations predict that at a pressure of 94.1 GPa the indirect band gap of pyrite
FeS2
vanishes and the material becomes a metal. This is due to the presence of the S–S and Fe–S
bonds, which provide novel energy band distortions in the process of attaining the metallic
state. Analysis indicates that, under increasing high pressure, the conduction bands
(3pz of
sulfur and 3dx2−y2+3dxy
of iron) intrude downwards into the valence bands, which are predominantly 3d in nature.
At normal pressure, the lattice constant, the bulk modulus, sulfur position parameter
u, S–S bond length, and the indirect band gap of pyrite
FeS2
are calculated using a fully relaxed unit cell and found to be equal to 541.8 pm, 159.7 GPa,
u = 0.383, 219.5 pm and 0.45 eV, respectively. Apart from the gap, which is too small (the usual 'LDA
error'), these results agree well with recent experiments. The effective masses of an electron
at selected points in the conduction band are reported.