Cation distribution at 1600 K in the system Fe3O4‐FeA12O4 was derived from Seebeck coefficient measurements assuming that the aluminum distribution behaved according to the thermodynamic model proposed by O'Neill and Navrotsky. Approximately 10% of the aluminum resides tetrahedrally. This system provides a good test of thermodynamic models.
|Original language||English (US)|
|Journal||Journal of the American Ceramic Society|
|State||Published - Mar 1985|
ASJC Scopus subject areas
- Ceramics and Composites
- Materials Chemistry