Oxides containing multivalent cations, such as transition elements, are much more prone to be non-stoichiometric. Examples are TiO2+x, BaTiO3-x and SrTiO3-x where Ti4+ ions can be easily reduced to Ti3+ creating oxygen deficiency of order 1% within the limits of the stability of oxide i.e. before decomposition and phase change.
Transition metal mono-oxide series Ni1-xO, Co1-xO, Mn1-xO and Fe1-xO are the oxides in which a fraction of the divalent cations is easily oxidized to the divalent state resulting in cation deficiency, x . The deficiency is ~5x10-4 % for Ni1-xO, ~1% for Co1-xO, ~0.1% for Mn1-xO and ~0.15% for Fe1-xO. FeO is seldom stoichiometric and it has a minimum non-stoichiometry of 0.05%.