Abstract
Magnetic properties of a nickel‐zinc ferrite (15% NiO, 35% ZnO, 50% Fe2O3) were measured over a temperature range of 23°C to 110°C at hydrostatic pressures up to 40 000 psi. The relation between the shift in Curie temperature, ΔTc, and the change in pressure, Δp, was empirically found to be ΔTc=0.078(Δp)0.316 . It is shown that if magnetic anisotropy and internal strains limit the magnetizing processes, the relation between coercive force, Hc, maximum flux density, Bm, and initial permeability, μ0, is given by Hc=δBm0 , where δ is a proportionality constant. The experimental results obtained over the entire range of temperature and pressure verify the above relation. The value of δ is 2.56 for the ferrite investigated.

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