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Interaction of Trace Rare-Earth Dopants and Nanoheterogeneities Induces Giant Magnetostriction in Fe-Ga Alloys

机译:微量稀土掺杂物和纳米异质性的相互作用在Fe-Ga合金中引起巨大的磁致伸缩

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摘要

The discovery of a tenfold increase in magnetostriction of Fe by alloying nonmagnetic Ga was a breakthrough in magnetostrictive materials. The large magnetostriction is attributed to tetragonal nanoheterogeneities dispersed in the bcc matrix. A further remarkable fivefold increase is achieved by trace rare earth doping (1 at%) up to a value of approximate to 1500 ppm, more than 50 times that of pure iron. However, it remains a mystery why trace rare earth dopants can induce such giant magnetostriction. Here, it is found that interaction of rare earth dopants with the nanoheterogeneities produces the giant magnetostriction, through a combination of experimental studies, first-principles calculation and phase field simulations. The dopants tend to enter the nanoheterogeneities, increasing their distortion thereby creating a larger tetragonal distortion of the matrix as well as increased magnetocrystalline anisotropy. A mesoscopic model is developed using phase field simulation showing that the bulk tetragonal distortion arises mainly from those nanoheterogeneities with fixed Ga-Ga pairs parallel to the applied magnetic field. Increased tetragonal distortion of the doped nanoheterogeneities leads to further distortion of the matrix. The results deepen the understanding of heterogeneous magnetostriction, and will guide the search for new magnetic materials with giant magnetostriction.
机译:通过合金化非磁性Ga将Fe的磁致伸缩增加十倍的发现是磁致伸缩材料的一项突破。大的磁致伸缩归因于分散在bcc基质中的四方纳米异质性。微量稀土掺杂(<1 at%)达到了约1500 ppm的值,是纯铁的50倍以上,实现了进一步的五倍增长。然而,为什么微量的稀土掺杂剂会引起这种巨大的磁致伸缩仍然是一个谜。在这里,通过结合实验研究,第一性原理计算和相场模拟,发现稀土掺杂剂与纳米异质性的相互作用产生了巨大的磁致伸缩。掺杂剂趋于进入纳米异质性,从而增加其畸变,从而使基体产生更大的四边形畸变,并增加磁晶各向异性。使用相场模拟建立了介观模型,表明相变模型主要由那些具有平行于外加磁场的固定Ga-Ga对的纳米异质性引起。掺杂的纳米异质性的四边形变形增加,导致基体进一步变形。研究结果加深了对异质磁致伸缩的理解,并将为寻找具有巨大磁致伸缩的新型磁性材料提供指导。

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