Phase Equilibria in the System Fe‐Al‐O

C. E. MEYERS; T. O. MASON; W. T. PETUSKEY; J. W. HALLORAN; H. K. BOWEN

doi:10.1111/j.1151-2916.1980.tb09856.x

Phase Equilibria in the System Fe‐Al‐O

C. E. MEYERS^*, T. O. MASON, W. T. PETUSKEY, J. W. HALLORAN, H. K. BOWEN

^*Corresponding author for this work

Materials Science and Engineering

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

56 Scopus citations

Abstract

The composition limits for the spinel solid solution Fe(Fe_1‐x Al_x)₂O₄ were determined experimentally as a function of oxygen pressure at 1280°, 1380°, and 1500°C, using precise lattice parameter measurements. The results were combined with information from the literature to develop self‐consistent stability diagrams of P₀₂ vs cation fraction at constant temperatures for the iron‐aluminum oxide system.

Original language	English (US)
Pages (from-to)	659-663
Number of pages	5
Journal	Journal of the American Ceramic Society
Volume	63
Issue number	11-12
DOIs	https://doi.org/10.1111/j.1151-2916.1980.tb09856.x
State	Published - Jan 1 1980

ASJC Scopus subject areas

Ceramics and Composites
Geology
Geochemistry and Petrology
Materials Chemistry

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10.1111/j.1151-2916.1980.tb09856.x

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AU - MASON, T. O.

AU - PETUSKEY, W. T.

AU - HALLORAN, J. W.

AU - BOWEN, H. K.

PY - 1980/1/1

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N2 - The composition limits for the spinel solid solution Fe(Fe1‐x Alx)2O4 were determined experimentally as a function of oxygen pressure at 1280°, 1380°, and 1500°C, using precise lattice parameter measurements. The results were combined with information from the literature to develop self‐consistent stability diagrams of P02 vs cation fraction at constant temperatures for the iron‐aluminum oxide system.

AB - The composition limits for the spinel solid solution Fe(Fe1‐x Alx)2O4 were determined experimentally as a function of oxygen pressure at 1280°, 1380°, and 1500°C, using precise lattice parameter measurements. The results were combined with information from the literature to develop self‐consistent stability diagrams of P02 vs cation fraction at constant temperatures for the iron‐aluminum oxide system.

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Phase Equilibria in the System Fe‐Al‐O

Abstract

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