Effect of Oxygen Partial Pressure on Phase Relations
The system Fe-Mg-O is a good example showing that the oxygen partial pressure can have a profound influence on the phase diagram. At low oxygen partial pressures, iron is predominantly Fe2+ and the halite phase forms a complete solid solution from MgO to FeO, as shown in the left plot in Figure 3. Alternatively, in air, iron is mixed Fe2+/Fe3+ and, in addition to the halite phase (Fe,Mg)O, the spinel (Fe,Mg)3O4 and corundum (Fe,Mg)2O3 phases are also observed, as shown in the right plot in Figure 3. The new videos on the Learning Hub discuss how these types of calculations are done in Thermo-Calc and further discuss the results.