A
perovskite is any material with the same type of
crystal structure as
calcium titanium oxide (CaTiO
3), known as the
perovskite structure, or
XIIA
2+VIB
4+X
2-3 with the oxygen in the
face centers. Perovskites take their name from the
mineral, which was first discovered in the
Ural mountains of
Russia by Gustav Rose in 1839 and is named after Russian mineralogist
L. A. Perovski (1792–1856). The general chemical formula for perovskite compounds is ABX
3, where 'A' and 'B' are two
cations of very different sizes, and X is an
anion that bonds to both. The 'A' atoms are larger than the 'B' atoms. The ideal cubic-symmetry structure has the B
cation in 6-fold coordination, surrounded by an
octahedron of
anions, and the A cation in 12-fold
cuboctahedral coordination. The relative ion size requirements for stability of the cubic structure are quite stringent, so slight buckling and distortion can produce several lower-symmetry distorted versions, in which the coordination numbers of A cations, B cations or both are reduced.