磁铁矿各介晶的磁各向异性

B. Gross, S. Philipp, E. Josten, J. Leliaert, E. Wetterskog, L. Bergström, M. Poggio
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引用次数: 3

摘要

对创造磁性超材料的兴趣导致了磁性纳米颗粒超结构的生长方法。磁赤铁矿($\gamma\text{-Fe}_2\text{O}_3$)纳米颗粒的介观晶体可以排列成高度有序的体心四边形晶格,晶格长度可达几微米。虽然已经对无序系综进行了测量,但由于单个介观晶体的总磁矩较小,因此确定其磁性是具有挑战性的。在这里,我们克服了这些挑战,利用灵敏的动态悬臂磁强计来研究单个微米尺寸的$\gamma\text{-Fe}_2\text{O}_3$介晶。这些测量结果揭示了一种明确的立方各向异性,这是由组成磁赤铁矿纳米颗粒的晶体各向异性和它们在介观晶格内的排列引起的。各向异性的特征及其起源得以揭示,是因为我们将高度有序的介晶的自组装与解析其个体磁性的能力结合起来。这种组合对于其他纳米粒子的磁各向异性的未来研究是有希望的,因为它们太小而无法单独研究。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Magnetic anisotropy of individual maghemite mesocrystals
Interest in creating magnetic metamaterials has led to methods for growing superstructures of magnetic nanoparticles. Mesoscopic crystals of maghemite ($\gamma\text{-Fe}_2\text{O}_3$) nanoparticles can be arranged into highly ordered body-centered tetragonal lattices of up to a few micrometers. Although measurements on disordered ensembles have been carried out, determining the magnetic properties of individual mesoscopic crystals is challenging due to their small total magnetic moment. Here, we overcome these challenges by utilizing sensitive dynamic cantilever magnetometry to study individual micrometer-sized $\gamma\text{-Fe}_2\text{O}_3$ mesocrystals. These measurements reveal an unambiguous cubic anisotropy, resulting from the crystalline anisotropy of the constituent maghemite nanoparticles and their alignment within the mesoscopic lattice. The signatures of anisotropy and its orgins come to light because we combine the self-assembly of highly ordered mesocrystals with the ability to resolve their individual magnetism. This combination is promising for future studies of the magnetic anisotropy of other nanoparticles, which are too small to investigate individually.
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