Thermodynamics of defects in the (La x Ca 1-x )FeO 3-δ perovskite is modeled by means of the CALPHAD approach. In this phase, the A-sites are occupied by La +3 and Ca +2 , and Fe in the B-site is known to exist in +2, +3, and +4 oxidation states depending on the oxygen vacancy concentration. Therefore, the ionic sublattice model: (La +3 , Ca +2 )(Fe +2 , Fe +3 , Fe +4 )(O −2 , Va) 3 is used to describe the phase, and the model parameters are evaluated from experimental oxygen nonstoichiometry and phase equilibria data. With the Fe +2 and Fe +4 treated as the major species in the B-site, the calculated phase diagrams are in good agreement with the experimentally reported phase equilibria data. The concentration of various defects in (La x Ca 1-x )FeO 3-δ as a function of oxygen partial pressure and temperature are calculated at different concentrations of Ca. At high oxygen partial pressures, Fe +4 is predicted to be dominant while Fe +2 is dominant at low oxygen partial pressures.