Ferromagnetic grain boundary signature in die-upset Re-Fe-B magnets

L.Henderson Lewis, Yimei Zhu, D.O. Welch
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引用次数: 35

Abstract

Previous nanostructural and nanocompositional studies performed on the boundaries of deformed grains in two die-upset rare earth magnets with bulk compositions Nd13.75Fe80.25B6 and Pr13.75Fe80.25B6 indicate that the intergranular phase in many grain boundaries is enriched in iron relative to the bulk. We present here preliminary magnetic data that provide further evidence that this grain boundary phase is indeed iron-rich, and in fact appears to be ferromagnetic. Hysteresis loops were performed at 800 K on die-upset magnets with the above compositions. Each sample showed a clear hysteresis with coercivities between 34 and 40 Oe and an average remanence 4πBR of 6.8 G for the Nd-based sample and 10.3 G for the Pr-based sample. The ferromagnetic signals measured at high temperature in these magnets are attributed to the iron-rich grain boundary phase. The implications of this conclusion with respect to coercivity are discussed.

模镦Re-Fe-B磁体的铁磁晶界特征
对两种块体成分分别为Nd13.75Fe80.25B6和Pr13.75Fe80.25B6的压型稀土磁体变形晶界的纳米结构和纳米成分研究表明,相对于块体,许多晶界的晶间相富含铁。我们在这里提出了初步的磁性数据,提供了进一步的证据,证明这种晶界相确实是富铁的,实际上似乎是铁磁性的。在800 K的温度下,用上述成分对翻模磁体进行了磁滞回线实验。每个样品都表现出明显的磁滞,矫顽力在34 ~ 40 Oe之间,nd基样品的平均残余4πBR为6.8 G, pr基样品的平均残余4πBR为10.3 G。这些磁体在高温下测量的铁磁信号归因于富铁的晶界相。讨论了这一结论对矫顽力的影响。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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