Abstract
A Richter-type peak of magnetic loss and the disaccommodation were observed for cobalt-substituted Ni-Zn ferrites containing Fe2O3 less than the stoichiometric composition. These phenomena can be interpreted in terms of the diffusion of electrons between Co2+ ions and Co3+ ions. The induced anisotropy caused by the preferential occupation of Co3+ ions in four kinds of 16d sites may explain these phenomena. Relaxation times are represented by the equation τ=τ∞exp (Q⁄kT), where τ∞ are approximately 10−17 to 10−15 sec for the Richter-type peak and 10−10 to 10−11 sec for the disaccommodation. Activation energies are about 0.8 to 1.0 eV for the former, and about 0.5 to 0.7 eV for the latter.