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- W2046397923 abstract "Nd2Fe14B has a large uniaxial anisotropy at room temperature. It exhibits a spin reorientation phenomenon below ∼ 140 K. We have investigated the basic origin of the above properties employing a model in which the combined effects of crystal and exchange fields are taken into account. We show for the first time that the magnetocrystalline anisotropy arises due to a strong crystal field interaction in sublattice I while the spin reorientation phenomenon occurs due to a relatively weak crystal field interaction in sublattice II. Preliminary calculations for Tm2Fe14B also suggest a spin reorientation, thus lending further support to this model." @default.
- W2046397923 created "2016-06-24" @default.
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- W2046397923 date "1986-02-01" @default.
- W2046397923 modified "2023-09-26" @default.
- W2046397923 title "Origin of spin reorientation in rare earth-iron-boron permanent magnets" @default.
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- W2046397923 doi "https://doi.org/10.1016/0304-8853(86)90695-5" @default.
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