Experimental results are given on the velocity of propagation of a single domain boundary in a crystal of silicon iron with a simple domain structure. In weak applied magnetic fields ({~}0.003 oersted) the velocity is given by a relation of the form v=G(H-H₀), where G is a constant {~}4 cm/sec./oersted in this crystal, and H₀0.003 oersted is the starting field. Calculation of the eddy current losses accompanying the motion of a plane boundary gives a theoretical expression for G in good agreement with experimental values; the predicted linear dependence on the resistivity was approximately verified by measurements at 78^∘{}, 194^∘{}, and 293^∘{}K. In stronger fields (>5 oersteds) there is evidence that the wall closes on itself, and the experimental velocity of collapse of the wall as deduced from flux changes agrees with the theoretical result based on a model of eddy current losses accompanying a collapsing cylindrical boundary. The results have a bearing on the well-known eddy current anomaly, namely, the fact that the total loss in a ferromagnetic material undergoing a.c. magnetization is often two or three times larger than the eddy-current and hysteresis losses calculated in the usual way assuming a spatially uniform and isotropic classical permeability.
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Williams et al. (1950) studied this question.
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