High‐Temperature Cation Distributions in Fe3‐FeAl2O4

T. O. Mason

doi:10.1111/j.1151-2916.1985.tb09635.x

High‐Temperature Cation Distributions in Fe₃‐FeAl₂O₄

T. O. Mason^*

^*Corresponding author for this work

Materials Science and Engineering

Research output: Contribution to journal › Article › peer-review

8 Scopus citations

Abstract

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)
Pages (from-to)	C‐74-C‐75
Journal	Journal of the American Ceramic Society
Volume	68
Issue number	3
DOIs	https://doi.org/10.1111/j.1151-2916.1985.tb09635.x
State	Published - Mar 1985

ASJC Scopus subject areas

Ceramics and Composites
Materials Chemistry

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10.1111/j.1151-2916.1985.tb09635.x

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title = "High‐Temperature Cation Distributions in Fe3‐FeAl2O4",

abstract = "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.",

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year = "1985",

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N2 - 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.

AB - 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.

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ER -

High‐Temperature Cation Distributions in Fe₃‐FeAl₂O₄

Abstract

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