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中国物理 B 2004
The anisotropy of Gd-Fe exchange interaction for Gd2Fe17 and Gd2Fe17H3Keywords: 磁化曲线,磁异性,土壤化合物,关联交换,结晶状态 Abstract: The magnetization curves along the crystal axes for Gd_2Fe_{17} and Gd_2Fe_{17}H_3 were analysed based on the single-ion model. If the Gd-Fe exchange interaction has been taken as isotropic as usual, the fitted values of magneto-crystalline anisotropy of the Fe sublattices in Gd_2Fe_{17} and Gd_2Fe_{17}H_3 would become unreasonably different from those of the corresponding Y or Lu compounds. It was shown that the large difference is caused by the neglect of the anisotropy of the Gd-Fe exchange interaction.
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