“…For example, the MIT behaviors were observed in both the high-valence Fe-associated oxides, such as AFeO 3 (A represents alkane earth, e.g., Ca or Ca 1– x Sr x ), Re Cu 3 Fe 4 O 12 ( Re represents rare earth), , and ( Re ,A)FeO 3 , and the low-valence Fe-containing oxides, such as Fe 3 O 4 , Re BaFe 2 O 5 , and Re Fe 2 O 4 . , Taken ( Re ,A)FeO 3 as a representative example, the valence state of Fe can be well controlled by either adjusting the Re /A ratio or the oxygen composition, and this further results in dramatic changes in their crystal and electronic structures as well as electric/magnetic properties. Since the oxygen composition plays a significant role in the phase transition in many material systems, some attempts were executed based on the ab initio calculations to research the formation of oxygen vacancies in the perovskite structure. , It is worth noting that pronounced MIT and magnetic transitions were usually achieved at x values of ∼2/3 in Re 1– x Sr x FeO 3 with light rare-earth compositions (e.g., La, Pr, and Nd). This was attributed to the charge ordering (CO) in the Fe site following a Fe 3+ -Fe 3+ -Fe 5+ sequence along the <111> axis direction when descending the temperature across a critical point ( T CO ) that opens the energy band gap abruptly .…”