Abstract
The solid solution sanmartinite (ZnWO4)-cuproscheelite (CuWO4) has been studied using Cu 2p X-ray absorption spectroscopy. While a single L3 absorption peak is observed for CuWO4, two distinct L3 absorption peaks with a separation of ∼0.8 eV are observed for the intermediate samples in the solid solution. The two peaks represent distinct Cu sites: one with all CuO6 next nearest neighbours in the (Cu,Zn)O6 chains, another having at least one ZnO6 next nearest neighbour. Both sites show a linear increase in covalency as a function of increasing Cu-content. The relative intensities of the two absorption peaks is dependent upon the Cu-content and has been used to model the site occupancies. The results reveal that the local structural effects can be associated with a composition-dependent structural phase transition from P2/c (ZnWO4) to P {Mathematical expression} (CuWO4). Deviations from a single-site model are explained in terms of the local environments, and evidence for site preferences and local clustering are explored.
Original language | English |
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Pages (from-to) | 375-381 |
Number of pages | 7 |
Journal | Physics and Chemistry of Minerals |
Volume | 20 |
Issue number | 6 |
DOIs | |
Publication status | Published - Dec 1993 |
Externally published | Yes |
ASJC Scopus Subject Areas
- General Materials Science
- Geochemistry and Petrology