Abstract
Cation distribution at 1600 K in the system Fe//3O//4-FeAl//2O//4 was derived from Seebeck coefficient measurements assuming that the aluminum distribution behaved according to the thermodynamic model proposed by H. S. C. O'Neill and A. Navrotsky. Approximately 10% of the aluminum resides tetrahedrally. This system provides a good test of thermodynamic models.
| Original language | English |
|---|---|
| Journal | Journal of the American Ceramic Society |
| Volume | 68 |
| Issue number | 3 |
| Publication status | Published - Mar 1985 |
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ASJC Scopus subject areas
- Ceramics and Composites