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Phase Relations in the System Fe 2 O 3 –Fe 3 O 4 –YFeO 3 in Air
Author(s) -
HOOK H. J.
Publication year - 1961
Publication title -
journal of the american ceramic society
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.9
H-Index - 196
eISSN - 1551-2916
pISSN - 0002-7820
DOI - 10.1111/j.1151-2916.1961.tb15362.x
Subject(s) - orthoferrite , yttrium , isobar , mole fraction , eutectic system , yttrium iron garnet , stoichiometry , analytical chemistry (journal) , ternary operation , oxide , materials science , phase (matter) , iron oxide , solubility , mineralogy , thermodynamics , chemistry , metallurgy , alloy , nucleon , physics , magnetization , organic chemistry , atomic physics , quantum mechanics , chromatography , magnetic field , computer science , programming language
Measurements were made of temperature and ternary composition for coexisting liquid and crystalline phases on the air isobar in the system Fe 2 O 3 ‐Fe 3 O 4 ‐YFeO 3 with particular regard to the stability range and compositional limits of yttrium iron garnet. Phase equilibrium relations were determined by conventional quenching techniques combined with measurements of loss in weight at the reaction temperature to locate true ternary compositions. The intersection of the air isobar with the ternary univariant boundary curve for coexisting magnetite, garnet, and liquid phases results in a eutectic‐type situation at the composition Y 0.27 Fe 1.73 O 2.87 and 1469°± 2°C. A similar intersection of the isobar with the boundary curve for coexisting garnet, orthoferrite, and liquid phases gives rise to a peritectic‐type reaction at 1555° 3°C. and Y 0.44 Fe 1.56 O 2.89 The yttrium iron garnet crystallizing from liquids within these temperature and composition limits contains up to 0.5 mole % iron oxide in excess of the stoichiometric formula in terms of the starting composition 37.5 mole % Y 2 O 3 , 62.5 mole % Fe 2 O 3 . At 1470° C. the garnet phase in equilibrium with oxide liquid contains 2 mole % FeO in solid solution. The small solubility of excess of iron oxide and partial reduction of the garnet phase in air are unavoidable during equilibrium growth from the melt.