Abstract
A careful electron diffraction investigation of pearceite-Tac and polybasite-Tac samples in the Ag+ fast ion conducting state reveals that the average hexagonal [AgI 9]9+ sub-structure in these mineral solid electrolyte systems is mutually incommensurable with respect to the remaining [(AgI,CuI)6(AsIII,SbIII)2S7]2-[CuIS4]7- framework sub-structure. It is shown how the mutual incommensurability of the two component sub-structures can be compatible with crystal chemical commonsense, with previously reported average structure refinements of these phases as well as providing an insight into their Ag+ fast ion conductivity at such low temperatures. In addition, Ag+/Cu+ ion ordering (and associated displacive shifts of the centreing S2- ions) in the S2-(Ag,Cu)6 octahedral sites is shown to provide a mechanism for low temperature superstructure ordering.
Original language | English |
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Pages (from-to) | 2080-2089 |
Number of pages | 10 |
Journal | Solid State Ionics |
Volume | 179 |
Issue number | 37 |
DOIs | |
Publication status | Published - 15 Nov 2008 |