Acta Crystallographica Section B

Structural Science

Volume 56, Part 3 (June 2000)



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Acta Cryst. (2000). B56, 402-408    [doi:10.1107/S0108768199016614]

Structures and phase transitions of the A7PSe6 (A = Ag, Cu) argyrodite-type ionic conductors. II. [beta]- and [bold gamma]-Cu7PSe6

E. Gaudin, F. Boucher, V. Petricek, F. Taulelle and M. Evain

Abstract: The crystal structures of two of the three polymorphic forms of the Cu7PSe6 argyrodite compound are determined by means of single-crystal X-ray diffraction. In the high-temperature form, at 353  K, i.e. 33  K above the first phase transition, [bold gamma]-Cu7PSe6 crystallizes in cubic symmetry, space group F43m. The full-matrix least-squares refinement of the structure leads to the residual factors R  = 0.0201 and wR = 0.0245 for 31 parameters and 300 observed independent reflections. In the intermediate form, at room temperature, [beta]-Cu7PSe6 crystallizes again in cubic symmetry, but with space group P213. Taking into account a merohedric twinning, the refinement of the [beta]-Cu7PSe6 structure leads to the residual factors R  = 0.0297 and wR  = 0.0317 for 70 parameters and 874 observed, independent reflections. The combination of a Gram-Charlier development of the Debye-Waller factor and a split model for copper cations reveals the possible diffusion paths of the d10 species in the [bold gamma]-Cu7PSe6 ionic conducting phase. The partial ordering of the Cu+ d10element at the phase transition is found in concordance with the highest probability density sites of the high-temperature phase diffusion paths. A comparison between the two Cu7PSe6 and Ag7PSe6 analogues is carried out, stressing the different mobility of Cu+ and Ag+ and their relative stability in low-coordination chalcogenide environments.

Online 1 June 2000


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