An approach to the magnetic relaxation processes in lithium ferrites

The relaxation of the initial magnetic permeability has been measured in polycrystalline Li x Fe 3− x O 4 samples, with x ranging from 0 to 0.5, by means of the magnetic disaccommodation (DA) technique. We have found that there is no abrupt transition for a given composition, but there is a progressive modification of the characteristic relaxation processes of magnetite. These results have been interpreted on the basis of the increasing amount of Li ions in the spinel lattice and hence, the resulting modifications on their proximities.