Abstract
It is shown that our theory of the magnetic annealing effect in ferrites as given in Part I can explain almost all of the available experimental results on the induced uniaxial anisotropy as dependent on the concentration, on the orientation of the magnetic field during annealing, and on the temperature of magnetic annealing. Thus, we conclude that the uniaxial anisotropy induced by magnetic annealing in ferrite is caused by an anisotropic distribution among cations and cation vacancies, namely, by a similar mechanism as in ferromagnetic metallic solid solutions.
