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 language | English |
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Pages (from-to) | 1317-1322 |
Number of pages | 5 |
Journal | Canadian Mineralogist |
Volume | 46 |
Issue number | 5 |
DOIs | |
Publication status | Published - 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