Subsolidus phase relationships in the system Fe2O3-Al2O3-TiO2 between 1000° and 1300°C

被引:18
作者
Pownceby, MI [1 ]
Constanti-Carey, KK [1 ]
Fisher-White, MJ [1 ]
机构
[1] CSIRO Minerals, Clayton, Vic 3169, Australia
关键词
D O I
10.1111/j.1151-2916.2003.tb03405.x
中图分类号
TQ174 [陶瓷工业]; TB3 [工程材料学];
学科分类号
0805 ; 080502 ;
摘要
Subsolidus phase equilibria in the system Fe2O3-Al2O3-TiO2 were investigated between 1000degrees and 1300degreesC. Quenched samples were examined using powder X-ray diffraction and electron probe microanalytical methods. The main features of the phase relations were: (a) the presence of an M3O5 solid solution series between end members Fe2TiO5 and Al2TiO5, (b) a miscibility gap along the Fe2O3-Al2O3 binary, (c) an alpha-M2O3(ss) ternary solid-solution region based on mutual solubility between Fe2O3, Al2O3, and TiO2, and (d) an extensive three-phase region characterized by the assemblage M3O5 + alpha-M2O3(ss) + Cor(ss). A comparison of results with previously established phase relations for the Fe2O3-Al2O3-TiO2 system shows considerable discrepancy.
引用
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页码:975 / 980
页数:6
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