Abstract
Defect-free pyrite (100) surfaces were generated and a controlled manipulation of sulfur defect density at these surfaces was performed. Sulfur species of different coordination environments at the surface were probed by photoemission in combination with theoretical modeling of core-level shifts. A strict structural assignment of peaks at the surface in the low defect density regime was achieved. Based on our results, a defect that is related to a surface sulfur vacancy is confirmed to provide the active site for the rapid initial oxidation of pyrite.
- Received 10 June 2004
DOI:https://doi.org/10.1103/PhysRevB.70.195404
©2004 American Physical Society