The oxidation state of copper and cobalt in carrollite, CuCo2S4

Richard A D Pattrick, Victoria S. Coker, Carolyn I. Pearce, Neil D. Telling, Gerrit van der Laan

Research output: Contribution to journalArticlepeer-review

Abstract

Using X-ray absorption spectroscopy (XAS) at the Cu L2,3 and Co L2,3 edges, we demonstrate that the valence state of copper in the thiospinel carrollite (CUCo2S4) is Cu+ with a d count of Cu d9.8. The Co has a d count of d6.4, so that the highly covalent mineral has an electronic formula of Cu1.2+ (Co2.4+)2 (S1.5-)4. There is half a hole per atom in the S 3p band (per unit formula); the Co L2,3 XAS indicates a covalent low-spin electronic structure. These data dispel the notion of the presence of Cu2+ in carrollite.
Original languageEnglish
Pages (from-to)1317-1322
Number of pages5
JournalCanadian Mineralogist
Volume46
Issue number5
DOIs
Publication statusPublished - Oct 2008

Keywords

  • Carrollite
  • L-edge
  • Low-spin electronic structure
  • Oxidation state
  • Thiospinel
  • X-ray absorption spectroscopy

Research Beacons, Institutes and Platforms

  • Dalton Nuclear Institute

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