The Electronic Structure and Reactivity of Sulfide Surfaces: Combining Atomic-Scale Observations with Theoretical Calculations
The Electronic Structure and Reactivity of Sulfide Surfaces: Combining Atomic-Scale Observations with Theoretical Calculations
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发表时间:
1998-06
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通讯作者:
K. Rosso
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作者:
K. Rosso
The electronic structure of clean pyrite {100} and covellite {001} surfaces have been investigated in ultra-high vacuum (UHV) for the purpose of understanding the nature of sulfide surface reactivity. Using primarily scanning tunneling microscopy and spectroscopy (STM/STS), the electronic structure at atomic sites on these surfaces was directly probed, and chemical insight into the results was provided by ab-initio calculations. Pyrite is the most abundant sulfide at the earth’s near surface. Its oxidation influences a wide variety of natural and industrial chemical process, but very little is known about the stepwise oxidation reactions involved. For this reason, the first two chapters are directed at understanding the surface electronic structure and fundamental reactivity of pyrite surfaces at the atomic scale. UPS spectra show a characteristic peak at ~ 1 eV forming the top of the valence band for the near surface. Ab-initio calculated densities of states for the bulk crystal suggest that this band is comprised primarily of non-bonding Fe 3d t2g and lesser S 3p and Fe 3d eg states. Ab-initio slab calculations predict that the broken bonding symmetry at the surface displaces a Fe 3dz2 dangling bond state into the bulk band gap. Evidence confirming the presence of this surface state is found in low bias STM imaging and normalized single-point tunneling spectra, which are in remarkable agreement with calculations of the LDOS at surface Fe and S sites. The results predict that due to the dangling bond surface states, Fe sites are energetically favored for redox interaction with electron donors or acceptor species. STM/STS observations of