Relation between disaccomodation and magnetic properties of manganese-ferrous ferrite
β Scribed by U. Enz
- Publisher
- Elsevier Science
- Year
- 1958
- Weight
- 790 KB
- Volume
- 24
- Category
- Article
- ISSN
- 0031-8914
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β¦ Synopsis
Initial permeability, crystalline anisotropy and magnetostriction have been measured on a single crystal of manganese-ferrous ferrite. The initial permeability shows a high disaccomodation, i.e. a decrease with time. This decrease can be as high as 95~o of the value immediately after demagnetisation. Disaccomodation is a timedependent blocking of domain walls, the cause of which is supposed to be a transition of electrons between different ions. The blocked walls cause constricted minor hyseresis loops which indeed have been found. Manganese-ferrous ferrites have in general an extra peak of the permeability as a function of temperature not understood up till now. I t is shown that this is an effect of disaccomodation.
π SIMILAR VOLUMES
The oxyfluoride phases \(x \mathrm{NbFeO}_{4}-(1-x) \mathrm{FeF}_{2}\) have been synthesized. They exist in a limited range \(0.8<x<1\). They are isomorphous with \(\mathrm{NbFeO}_{4}\), having the wolframite structure. The refinement of the crystallographic structure of the oxyfluoride phase \(\mat