Phase stabilities in copper ferrite are studied with substitution of T
i and Ge tetravalent ions. In Ti-substituted samples (Cu1+xTixFe2-2xO4
) the parent tetragonal structure is retained up to x=0.15, and for hi
gher content of Ti it changes to cubic. In the case of Ge-substituted
samples (Cu1+xGexFe2-2xO4), the cubic structure is observed for 0.0<x
less than or equal to 0.2, and the tetragonal structure reverts for hi
gher contents of Ge. The origin of the distortion lies in square coval
ent bond formation of copper ions at the octahedral site. The observed
results are explained on the basis of cation distribution and covalen
t bond formation of copper and germanium ions.