Km. Rosso et al., Atomically resolved electronic structure of pyrite {100} surfaces: An experimental and theoretical investigation with implications for reactivity, AM MINERAL, 84(10), 1999, pp. 1535-1548
Clean pyrite {100} surfaces, generated by cleaving in UHV, were investigate
d using scanning tunneling microscopy and spectroscopy for the purpose of u
nderstanding the electronic structure at the surface. Calculations of the s
urface atomic structure and LEED data support a (100) surface structure tha
t undergoes very little relaxation and can be approximated by a simple term
ination of the bulk structure along a plane of cleaved Fe-S bonds. UPS spec
tra show a well defined peak at similar to 1 eV forming the top of the vale
nce band for the near surface. Calculated densities of states for the bulk
crystal suggest that this band is comprised primarily of non-bonding Fe 3d
t(2g) character and lesser S 3p and Fe 3d e(g) character. Slab calculations
predict that the loss of coordination at the surface results primarily in
the displacement of Fe 3d(z2)-like surface states into the bulk band gap. E
vidence for this surface state is found in low bias STM imaging and normali
zed single-point tunneling spectra. Calculations of the LDOS at surface Fe
and S sites indicate that the highest occupied state is primarily of 3d(z2)
-like character and the lowest unoccupied state is of mixed Fe 3d(z2)-S 3p
character. The results predict that due to the dangling bond surface states
, Fe sites are energetically favored over S-2 sites for redox interaction w
ith electron donors or acceptor species on this surface. Surface redox reac
tions are expected to involve the quenching of these high energy dangling b
onds, leading to new bonds and surface species, changing the chemical makeu
p of the surface.