2020 Volume 67 Issue 2 Pages 78-83
The uniaxial magnetic anisotropy of the magnetoplumbyte-type (M-type) hard ferrite magnet is improved by the substitution of small amount of Co for Fe. The Co atoms occupy at least 3 sites among 5 crystallographically inequivalent Fe sites. Different magnetic functions of Co are expected at the different sites because of different oxygen coordinations around the sites. We have revealed from 59Co nuclear magnetic resonance experiment that only Co located at the tetrahedrally coordinated 4f1 site is responsible for the enhancement in the uniaxial anisotropy, demonstrating that the control of the Co occupation site is essentially important in the Co-doped M-type ferrite. If only the tetrahedrally coordinated 4f1 site were occupied by Co atoms, the magnetic performance can be improved more efficiently.