The micromagnetic theory is a simple and powerful method to calculate the spin-wave dispersion relation in the long-wavelength region. The calculation has been performed within the framework of the two-sublattice model which is the adequate micromagnetic description for rare-earth--transition-metal compounds. A magnetocrystalline anisotropy of the easy-axis type is assumed and the cases of ferromagnetic and ferrimagnetic coupling of the two sublattices are considered. The theoretical results are compared to neutron-scattering data obtained from RFe₂, R₂{Fe}₁₇$, ${R}₂Co₁₇, and R₂{Fe}₁₄$B, with R representing different rare-earth atoms.
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Ried et al. (1994) studied this question.
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