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Crystallographic magnetic anisotropy and the permeability tensor of a ferrite

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Abstract

Seidel and Boyet [1] first derive the magnetic-permeability tensor for a single crystal of a cubic ferrite of low energy; they gave explicit expressions for the components for a crystal magnetized in the (110) plane. Here I consider the more general case of magnetization in any direction; the components are averaged to deduce the permeability of a polycrystalline aggregate.

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References

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Khlystov, A.S. Crystallographic magnetic anisotropy and the permeability tensor of a ferrite. Soviet Physics Journal 8, 31–34 (1965). https://doi.org/10.1007/BF00818277

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