Experimental and theoretical characterization of the structure of defects at the pyrite FeS2(100) surface

K. Andersson, M. Nyberg, H. Ogasawara, D. Nordlund, T. Kendelewicz, C. S. Doyle, G. E. Brown, Jr., L. G. M. Pettersson, and A. Nilsson
Phys. Rev. B 70, 195404 – Published 5 November 2004

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 S 2p photoemission in combination with theoretical modeling of S 2p core-level shifts. A strict structural assignment of S 2p peaks at the FeS2(100) 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.

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  • Received 10 June 2004

DOI:https://doi.org/10.1103/PhysRevB.70.195404

©2004 American Physical Society

Authors & Affiliations

K. Andersson1,2,3, M. Nyberg1, H. Ogasawara2, D. Nordlund1, T. Kendelewicz3, C. S. Doyle3, G. E. Brown, Jr.2,3, L. G. M. Pettersson1, and A. Nilsson1,2

  • 1FYSIKUM, Stockholm University, SCFAB, S-10691 Stockholm, Sweden
  • 2Stanford Synchrotron Radiation Laboratory, 2575 Sand Hill Road, Menlo Park, California 94025, USA
  • 3Department of Geological and Environmental Sciences, Stanford University, Stanford, California 94305-2115, USA

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Issue

Vol. 70, Iss. 19 — 15 November 2004

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