“…Recently, we have found that, upon the transition from a layered tetragonal phase with the ordered distribution of Gd/Sr ions in cobaltite Gd 0.2 Sr 0.8 CoO 3-δ to a cubic phase with the random arrangement of Sr 2+ and Gd 3+ cations in the A sites of the crystal lattice, many physicochemical properties, including the value of oxygen nonstoichiometry and type of the ordering of oxygen vacancies [12,13], change. This affects the mobility of lattice oxygen/oxygen vacancies and, consequently, the oxygen-ion conductivity.…”