“…Thus, ionic conductivity can be optimized by partial substitution of lattice elements in the crystal structure. [56][57][58] Generally, oxide electrolytes are divided into sodium super ionic conductor (NASICON, LiM 2 (PO 4 ) 3 , M = Ge, Ti, Zr), [59,60] lithium super ionic conductor (LISICON, Li 3+x X x Y 1-x O 4 , X = Si, Ge, Ti, Y = P, As, V, Cr), [61][62][63] Perovskite types, [64,65] Garnet types (A 3 B 2 (XO 4 ) 3 , A = Ca, Mg, Y, La; B = Al, Fe, Ga, Ge, Mn, Ni, V), [66,67] etc. Perovskite-type electrolytes were reported as early as 1953, and their general formula for the Perovskite structure is ABO 3 (the coordinated cations of A and B are 12 and 6, respectively).…”