Abstract
A detailed study of the magnetic anisotropy of a Co1.1Fe1.9O4 single crystal at 77°K revealed that, after cooling in a magnetic field, a relatively small uniaxial anisotropy is superposed on the large cubic anisotropy (K1 and K2). Rotational hysteresis is present at 77°K which is explained in terms of the irreversible wall displacement and the relaxing anisotropy energy. The presence of large rotational hysteresis in polycrystalline specimens CoFe2O4∼Co3O4 is also shown and is explained on this basis. Preliminary data on the relaxation time of the phenomenon are presented. All the data are consistent with the mechanism presented by Mizushima, which assumes the electron diffusion between Co2+ and Co3+ions. Data in the series Fe1−2xNi2xCo2O4 are also presented. Suggestions are made that the rotational hystereses observed in Co2Ba2Fe12O22 and BaCoδTiδFe12−2δO18 at low temperatures are caused by the same mechanism.