Abstract
An in situ study of cubanite (CuFe2S3) was performed using energy dispersive X-ray diffraction and Mössbauer spectroscopy in a diamond anvil cell at room temperature and pressures up to 5 GPa. Mössbauer spectra of orthorhombic cubanite show a single iron site with a hyperfine magnetic field that is relatively insentive to pressure, and a centre shift which decreases with pressure at a rate consistent with no significant changes in bonding. Above 3 GPa, however, a nonmagnetic component appears that can be fitted to a single asymmetric quadrupole doublet with a centre shift corresponding to valence between Fe2+ and Fe3+. This is consistent with X-ray diffraction data that show an accompanying transition from the orthorhombic structure to the NiAs structure, where localised electron transfer could occur across pairs of face-shared octahedra or extended electron delocalisation could occur along sheets of face- and edge-shared octahedra.
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References
C.A. McCammon, J. Zhang, R.M. Hazen and L.W. Finger, Am. Mineral. 77(1992)937.
L. Merrill and W.A. Bassett, Rev. Sci. Instr. 45(1974)290.
L.J. Cabri, S.R. Hall, J.T. Syzmanski and J.M. Stewart, Can. Mineral. 12(1973)33.
C.A. McCammon, in:Recent Trends in High Pressure Research, ed. A.K. Singh (Oxford & IBH, New Delhi, 1992) p. 824.
C.A. McCammon, in:High Pressure Science and Technology, ed. S.C. Schmidt (American Institute of Physics, New York) in press.
P. Imbert and M. Wintenberger, Bull Soc. Fr. Minéral. Cristallogr. 90(1967)299.
S.V. Karyagin, Sov. Phys. Solid State 8(1966)391.
D.L. Williamson, in:Mössbauer Isomer Shifts, eds. G.K. Shenoy and F.E. Wagner (North-Holland, Amsterdam, 1978) p.317.
H.G. Drickamer, R.W. Vaughn and A.R. Champion, Accounts Chem. Res. 2(1969)40.
H.E. King, Jr. and C.T. Prewitt, Acta Cryst. B38(1982)1877.
H. King, D. Virgo and H.K. Mao, Ann. Rept. Geophys. Lab. 77(1978)830.
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McCammon, C.A. High-pressure in situ investigation of cubanite (CuFe2S3): Electronic structure. Hyperfine Interact 93, 1511–1514 (1994). https://doi.org/10.1007/BF02072901
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DOI: https://doi.org/10.1007/BF02072901