The present study concerns the investigation of the oxygen content in the perovskite-type manganite Ca0.6−уSr0.4HoуMnO3−δ (0 ≤ y ≤ 0.15) as a function of temperature (T) and oxygen partial pressure (pO2) in the gas phase since the oxygen nonstoichiometry (δ) has a significant impact on the physicochemical properties of materials applied in a variety of high-temperature devices. The δ value has been determined using thermogravimetry and coulometric titration methods. The resulting pO2 – T – δ diagrams have been accurately described by the defect chemical equilibrium model, that accounts for the oxidation reaction of Mn3+ to Mn4+ in all of the studied samples. Additionally, for the samples containing holmium, the disproportionation reaction of Mn3+ to Mn2+ and Mn4+ has been considered. This is the first study to demonstrate the distinction in Mn3+ disproportionation reactions in stoichiometric and nonstoichiometric Ca0.6−уSr0.4HoуMnO3−δ manganites, resulting from the discrepancy in oxygen coordination of Mn3+ ions at low and high temperatures. The experimental dependencies δ(T, pO2) have been employed in order to calculate the chemical potential of oxygen (ΔμO) in relation to the standard state. Statistical thermodynamic analysis has yielded equations that describe the relationships between the partial molar enthalpy (ΔhO) and entropy (ΔsO) of oxygen with standard enthalpies and entropies of defect formation reactions, Mn3+ ion concentration, and nonstoichiometry δ. The calculated functions ΔhO(y, δ, T) and ΔsO(y, δ, T) have been shown to exhibit a high degree of correlation with the values of ΔhO and ΔsO obtained from the linear dependencies of ΔμO on T.
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