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 |
|---|---|
| Pages (from-to) | 1113-1118 |
| Number of pages | 6 |
| Journal | Philosophical Magazine A |
| Volume | 64 |
| Issue number | 5 |
| Publication status | Published - Nov 1991 |