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
H. Seidel and H. Boyet, J. Appl. Phys., 28, no 4, 452, 1957.
S. V. Vonsovskii and Ya. S. Shur, Ferromagnetism [in Russian], OGIZ, GITTL, Moscow-Leningrad, 1948.
I. R. Macdonald, Proc. Phys. Soc., 64, 968, 1951.
I. N. Bronshtein and K. A. Semendyaev, Handbook of Mathematics [in Russian], GITTL, Moscow, p. 218, 1954.
D. Polder, Phil. Mag., 40, 99, 1949.
A. G. Gurevich, UHF Ferrites [in Russian], GIFML, 1960.
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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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DOI: https://doi.org/10.1007/BF00818277