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Direct observation of Σ7 domain boundary core structure in magnetic skyrmion lattice

机译:磁天文子晶格中Σ7畴边界核结构的直接观察

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摘要

Skyrmions are topologically protected nanoscale magnetic spin entities in helical magnets. They behave like particles and tend to form hexagonal close-packed lattices, like atoms, as their stable structure. Domain boundaries in skyrmion lattices are considered to be important as they affect the dynamic properties of magnetic skyrmions. However, little is known about the fine structure of such skyrmion domain boundaries. We use differential phase contrast scanning transmission electron microscopy to directly visualize skyrmion domain boundaries in FeGe1−xSix induced by the influence of an “edge” of a crystal grain. Similar to hexagonal close-packed atomic lattices, we find the formation of skyrmion “Σ7” domain boundary, whose orientation relationship is predicted by the coincidence site lattice theory to be geometrically stable. On the contrary, the skyrmion domain boundary core structure shows a very different structure relaxation mode. Individual skyrmions can flexibly change their size and shape to accommodate local coordination changes and free volumes formed at the domain boundary cores. Although atomic rearrangement is a common structural relaxation mode in crystalline grain boundaries, skyrmions show very unique and thus different responses to such local lattice disorders.
机译:Skyrmion是螺旋磁体中受拓扑保护的纳米级磁性自旋实体。它们的行为像粒子,并倾向于形成像原子一样的六方密堆积晶格,作为它们的稳定结构。在天体离子晶格中的畴边界被认为是重要的,因为它们会影响磁性天体离子的动力学特性。然而,人们对这种天rm离子域边界的精细结构知之甚少。我们使用差分相衬扫描透射电子显微镜直接可视化FeGe1-xSix中由于晶粒“边缘”的影响而引起的天空离子域边界。与六方密堆积原子格子相似,我们发现了天合子“Σ7”畴边界的形成,其重合关系由重合点阵理论预测为几何稳定。相反,天蝎子域边界核结构显示出非常不同的结构弛豫模式。各个天体可以灵活地更改其大小和形状,以适应局部协调变化和在域边界核心处形成的自由体积。尽管原子重排是晶粒边界中常见的结构弛豫模式,但天rm子显示出非常独特的特征,因此对这种局部晶格紊乱的反应也不同。

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