Phase equilibrium in the system Y-Fe-O at 1100°C

Phase equilibrium was established in the Y-Fe-O system at 1100°C by varying the oxygen partial pressure from −log(P_O2/atm)=15.00 to 0, allowing construction of a phase diagram at 1100°C for the system Y₂O₃-Fe-Fe₂O₃. In the system, two ternary compounds, YFeO₃ and Y₃Fe₅O₁₂, were stable and had nonstoichiometric composition, whereas YFe₂O₄ was not found to be stable. The present result was different from that of previous studies at 1200°C, in which YFe₂O₄ was stable, along with the above two ternary compounds. Lattice constants of YFeO₃ and Y₃Fe₅O₁₂, prepared in air by a quenching method, were determined and compared with previous values, and showed close agreement. The standard Gibbs energy changes of the reactions in the Fe-O system, Fe+1/2O₂=FeO, 3FeO+1/2O₂=Fe₃O₄, and 2/3Fe₃O₄+1/6O₂=Fe₂O₃, were determined, and the obtained values were compared with the previous values. The standard Gibbs energy changes of the reactions, Fe+1/2Y₂O₃+3/4O₂=YFeO₃, and 3YFeO₃+2/3Fe₃O₄+1/6O₂=Y₃Fe₅O₁₂, were calculated from the oxygen partial pressures in equilibrium.