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Nanometre imaging of Fe3GeTe2 ferromagnetic domain walls

机译:Fe3Gete2铁磁畴壁的纳米成像

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摘要

Fe3GeTe2 is a layered crystal which has recently been shown to maintain its itinerant ferromagnetic properties even when atomically thin. Here, differential phase contrast scanning transmission electron microscopy is used to investigate the domain structure in a Fe3GeTe2 cross-sectional lamella at temperatures ranging from 95 to 250 K and at nanometre spatial resolution. Below the experimentally determined Curie temperature (T-C) of 191 K, stripe domains magnetised along < 0001 >, bounded with 180(degrees) Bloch type domain walls, are observed, transitioning to mixed Bloch-Neel type where the cross-sectional thickness is reduced below 50 nm. When warming towards T-C, these domains undergo slight restructuring towards uniform size, before abruptly fading at T-C. Localised loss of ferromagnetic order is seen over time, hypothesised to be a frustration of ferromagnetic order from ambient oxidation and basal cracking, which could enable selective modification of the magnetic properties for device applications.
机译:Fe3GeTe2是一种层状晶体,最近被证明即使在原子薄的情况下也能保持其流动铁磁性。在这里,差分相衬扫描透射电子显微镜被用来研究在95到250 K的温度和纳米空间分辨率下Fe3GeTe2横截面薄片中的畴结构。在实验确定的191 K居里温度(T-C)以下,观察到沿<0001>磁化的条纹畴,以180(度)布洛赫型畴壁为界,过渡到混合布洛赫-尼尔型,其中横截面厚度降低到50 nm以下。当温度升高到T-C时,这些磁畴在T-C处突然消失之前,会朝着均匀的尺寸进行轻微的重组。随着时间的推移,铁磁有序的局部损失会被观察到,假设是由于环境氧化和基底开裂导致铁磁有序的挫败,这可能使器件应用的磁性能发生选择性改变。

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