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Direct imaging of dopant sites in rare-earth element-doped permanent magnet and correlated magnetism origin

机译:在稀土元素掺杂的永久磁铁和相关磁性起源中的掺杂位点的直接成像

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Identifying the dopants and their occupation sites in rare-earth-doped permanent magnets is critical not only to understand the mechanism of tuning their magnetic properties, but also to develop guiding principles to further improve their performance. In this study, we present a direct observation of the preferred atomic sites of La atoms in La-doped M-type SrFe12O19 hexaferrite. Our data solidly clarified that only the Sr2+ cations were replaced by La3+ cations, and the La-doping caused the changes in the valence states of iron cations located at the 4f(1) and 2a crystallographic sites. First principles calculations further revealed that after La-doping, the changes in the spin states of the Fe3+ cations located at the 4f(1) tetrahedral sites resulted in magnetization enhancement and those of the 2a octahedral sites contributed to electrical neutrality, well matching the experimental atomic-column resolution EELS and magnetic measurement results.
机译:在稀有地掺杂的永久磁铁中识别掺杂剂及其职业位点,不仅要了解调整其磁性的机制,而且要制定指导原则以进一步提高其性能。 在这项研究中,我们介绍了对LA掺杂的M型SRFE12O19 Hexaferrite中LA原子首选原子位点的直接观察。 我们的数据牢固地澄清了SR2+阳离子被LA3+阳离子取代,LA掺杂导致位于4F(1)和2A晶体学位点的铁阳离子的价值变化。 第一原理的计算进一步表明,在掺杂后,位于4f(1)四面体位点的Fe3+阳离子的自旋状态的变化导致磁化增强,而2A八面体位点的变化则有助于电气中性,与实验相匹配,很好地匹配了实验 原子柱分辨率鳗鱼和磁性测量结果。

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