The proposed model is capable of reproducing, with no adjustable parameters, the substitution dependence of the magnetic moment at 0^∘{}K of various substituted rare-earth iron garnets. Maxima in the temperature dependence of the moments are predicted and agree with experimental observations. The model also predicts that the hyperfine field in these systems has a different temperature and substitution dependence from that of the corresponding sublattice magnetization.
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I. Nowik (1968) studied this question.
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