Co-Cr ferrite has been studied with Mossbauer spectroscopy, X-ray diffracti
on, and vibrating sample magnetometery (VSM). The crystal structure for thi
s system is a spinel structure, and the lattice constants are in accordance
with Vegard's law. The Mossbauer spectra consist of two six-line patterns
corresponding to Fe3+ at the tetrahedral (A) and the octahedral (B) sites.
The Neel temperature decreases linearly with Cr concentration, suggesting t
he superexchange interaction Co-O-Fe link is stronger than that for the Cr-
O-Fe link. The Debye temperatures for the A and the B sites of CoFe1.9Cr0.1
O4 are found to be theta(A)=827+/-5 K and theta(B)=218+/-5 K. Atomic migrat
ion of CoFe1.9Cr0.1O4 starts near 295 K and increases rapidly with increasi
ng temperature to such a degree that 64 % of the ferric ions at the A sites
have moved over to the B sites at 600 K. The VSM data showed that the satu
ration magnetization decreased with increasing quantity of Cr ions.