“…The brownmillerite oxides ( A 2 B 2 O 5 , A = alkali earth, B = transition or group 3 metal) have been widely studied over many decades for their diverse properties, which include fast ionic conductivity, − thermoelectricity, catalytic activity, , and complex magnetic ordering. , The structure is derived from the archetypical cubic perovskite by removal of parallel ⟨110⟩ rows of oxygen atoms to yield alternating layers of B O 6 and B O 4 units arranged in corner-linked sheets and chains, respectively (Figure a). Oxide-ionic conductivity has been observed and characterized in several brownmillerite phases, though many of these exhibit a sharp increase in conductivity upon conversion to a cubic perovskite phase with disordered oxygen vacancies at high temperatures, ,, suggesting that the best performance may be achieved by suppressing the low-temperature brownmillerite phase.…”