“…Recent studies showed that the cation distribution in a cubic CuFe 2 O 4 can be given as ðCu x Fe 1Àx Þ T d ½Cu 1Àx Fe 1þx O h O 4 ; in which the parentheses and square brackets denote tetrahedral and octahedral sites, respectively, whereas tetragonal CuFe 2 O 4 is completely inverse, i.e., x ¼ 0 [5,6]. The ground state of Cu 2þ ion in the octahedral crystal field is an orbital doublet 2 E g ðt 6 2g e 3 g Þ and so subject to a Jahn-Teller effect which removes the degeneracy of the ground state.…”