The results of linear augmented-plane-wave band calculations for cubic
FeSi, carried out in the local-density approximation, predict a small
(approximately 0.11 eV) indirect semiconductor gap which agrees well
with empirical estimates (approximately 0.13 eV). The origin of this g
ap, which occurs within the Fe (3d) manifold, can be traced to a pseud
ogap that is present in the reference rocksalt phase that underlies th
e lower-symmetry FeSi structure. The relationship between the FeSi ban
d structure and several types of many-body correlation mechanisms that
have been advanced to explain its anomalous temperature-dependent mag
netic properties is discussed.