Abstract
X-ray photoelectron and absorption spectra have been obtained for natural specimens of cubanite and compared with the corresponding spectra for chalcopyrite. Synchrotron X-ray photoelectron spectra of surfaces prepared by fracture under ultra-high vacuum revealed some clear differences for the two minerals, most notably those reflecting their different structures. In particular, the concentration of the low binding energy S species formed at cubanite fracture surfaces was approximately double that produced at chalcopyrite surfaces. However, the core electron binding energies for the two S environments in cubanite were not significantly different, and were similar to the corresponding values for the single environment in chalcopyrite. High binding energy features in the S 2p and Cu 2p spectra were not related to surface species produced either by the fracture or by oxidation, and most probably arose from energy loss due to inter-band excitation. Differences relating to the Fe electronic environments were detectable, but were smaller than expected from some of the observed physical properties and Mössbauer spectroscopic parameters for the two minerals. X-ray absorption and photoelectron spectra together with the calculated densities of states for cubanite confirmed an oxidation state of CuI in the mineral. It was concluded that the best formal oxidation state representation for cubanite is CuI(Fe2)VS −II3 .
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Acknowledgments
This work was supported by the Australian Synchrotron Research Program, which was funded by the Commonwealth of Australia under the Major National Research Facilities Program. The research was partly undertaken on the soft X-ray beam-line (BL14ID) at the Australian Synchrotron, Victoria, Australia. The IWRI author acknowledges funding support for the Australian Mineral Science Research Institute by AMIRA International, the Australian Research Council, and the South Australian Government. The authors are grateful to Bruce Cowie for assistance in the use of BL14D at the AS, Yaw-wen Yang and Jyh-Fu Lee for access to BL24A and BL17C at the NSRRC, and to Allan Pring, Museum of South Australia for the massive cubanite and chalcopyrite specimens.
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Goh, S.W., Buckley, A.N., Skinner, W.M. et al. An X-ray photoelectron and absorption spectroscopic investigation of the electronic structure of cubanite, CuFe2S3 . Phys Chem Minerals 37, 389–405 (2010). https://doi.org/10.1007/s00269-009-0341-z
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DOI: https://doi.org/10.1007/s00269-009-0341-z