Abstract
Thermoelectric coefficient measurements in the system Fe3O4‐Fe2TiO4 were used to determine the cation distributions from 600° to 1300°C. The cation distributions obeyed the relation ‐RT In K=‐9.61+2(‐0.0154T)b+0.0256T (kJ/mol) where KFecd is the iron distribution constant and b is the tetrahedral Fe3+ concentration. Low‐temperature extrapolations agreed with experimental magnetometry and lattice parameter results. With the incorporation of a subregular size‐mismatch term, agreement with high‐temperature thermodynamic data was achieved. A solvus at intermediate temperatures was correctly predicted by the model.
Original language | English (US) |
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Pages (from-to) | 829-834 |
Number of pages | 6 |
Journal | Journal of the American Ceramic Society |
Volume | 66 |
Issue number | 12 |
DOIs | |
State | Published - Jan 1 1983 |
ASJC Scopus subject areas
- Ceramics and Composites
- Materials Chemistry