Hexagonal ferrites that have a previously unexplored class of substitutions
have been made and evaluated by observing their microwave absorption spect
ra as a function of temperature. The temperature dependences of the uniaxia
l anisotropy and the magnetic moment were determined. Substitutions were in
vestigated in hexagonal ferrites normally having a small divalent ion in th
eir composition, e.g., Zn-Z(Zn2Ba3Fe24O41), Ni-W, etc. Substitution of a fu
rther Zn and Ti for Fe reduced the uniaxial anisotropy field, H-a, of Zn-Z
rapidly from similar to 5 kOe to a few kilo-oersteds, while replacing only
about one of the 24 Fe atoms in the formula unit. This rapid reduction in a
nisotropy along with moderate reductions in T-C and moment at 300 K, imply
that these substitutions preferentially fill the high anisotropy, up-spin,
trigonal bipyramidal sites. The anisotropy field is only weakly temperature
dependent near 300 K. This contrasts strongly with the case of Co substitu
tions often used to obtain H-a in this range. Complications caused by rapid
magnetic relaxation and magnetostriction associated with divalent Co are a
lso avoided. [S0021-8979(00)26008-8].