High‐Temperature Cation Distributions in Fe3‐FeAl2O4

T. O. Mason*

*Corresponding author for this work

Research output: Contribution to journalArticlepeer-review

2 Scopus citations


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 languageEnglish (US)
Pages (from-to)C‐74-C‐75
JournalJournal of the American Ceramic Society
Issue number3
StatePublished - Mar 1985

ASJC Scopus subject areas

  • Ceramics and Composites
  • Materials Chemistry


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