Abstract
Lithium ion transport in crystalline solid electrolytes is discussed with reference to a model system LISICON, Li2+2xZn1-xGeO4. In LISICON, ionic conductivity is due to the presence of the interstitial Li+ ions which are not randomly distributed over sets of crystallographically identical sites but are incorporated within defect clusters. The structure of the solid consists of a mosaic of substructures, namely the lithium-rich defects and regions with the structure of stoichiometric Li2ZnGeO4. It is proposed that the interstitial Li+ ions are transported as an interstitial triple and that effectively the entire defect moves through the crystal. An explanation is also proposed for the curvature in the log s against 1/T plots for this electrolyte.
Original language | English |
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Pages (from-to) | 1113-1118 |
Number of pages | 6 |
Journal | Philosophical Magazine A |
Volume | 64 |
Issue number | 5 |
Publication status | Published - Nov 1991 |