在2D磁铁Fe3GeTe2中通过几何诱导的应变稳定局部自旋纹理
Yuhan Sun1, Max T Birch2, Simone Finizio3,4
1Max Planck Institute for Solid State Research, Heisenbergstrasse 1, 70569, Stuttgart, Germany.
Advanced materials (Deerfield Beach, Fla.)
|June 19, 2025
概括
像Fe3GeTe2 (FGT) 这样的二维铁磁体中的几何诱导应变可以局部控制磁自旋纹理. 这种应变工程稳定了异国情调的磁域,包括 skyrmions,为新型自旋电子设备铺平了道路.
科学领域:
- 凝聚物质物理学 凝聚物质物理学
- 材料科学 材料科学 材料科学
- 纳米技术纳米技术
背景情况:
- 应变工程是调整2D范德瓦尔斯 (vdW) 铁磁体用于自旋电子的关键.
- 之前的研究集中在全球应变效应上,忽视了当地的磁自旋纹理影响.
研究的目的:
- 为了研究几何学诱导的应变对2D铁磁磁体中局部磁自旋纹理的影响.
- 用空间变化的应变来证明Fe3GeTe2 (FGT) 中磁性的操纵.
主要方法:
- 利用扫描传输X射线显微镜 (STXM) 来可视化磁性秩序.
- 采用微柱阵列,在FGT板中创建受控的,由几何学诱导的拉伸配置文件.
主要成果:
- 空间变化的平面内应变 (<0.5%) 局部增加了FGT的基里温度10K.
- 稳定磁域,包括斯基尔米翁和更高阶的拓旋转纹理 (斯基尔米翁,斯基尔米翁袋),靠近柱子角.
结论:
- 在2D vdW铁磁体中,由几何引发的应变提供了一种用于局部控制2D vdW铁磁体磁转纹理的方法.
- 这种压力介导的拓旋转纹理控制为基于旋转的信息技术开辟了新的可能性.
关键词:
2D磁铁的使用方法Fe3GeTe2Fe2Fe2Fe2Fe2Fe2Fe3GeTe2Fe2Fe2Fe3Fe2Fe2Fe2Fe3Fe2Fe3Fe2Fe3Fe2Fe3Fe3Fe2Fe3Fe2Fe3Fe3Fe2Fe3Fe2Fe3Fe3Fe2Fe3Fe2Fe3Fe3Fe2Fe3Fe3Fe2Fe3Fe2Fe3Fe2Fe3Fe2Fe3Fe2Fe3Fe2Fe3Fe2Fe3Fe3Fe2Fe2Fe3Fe2Fe3Fe2Fe3Fe3Fe2Fe3Fe2Fe3Fe2Fe3Fe2Fe3Fe2Fe3Fe3Fe2Fe3Fe2Fe3Fe3Fe2Fe3Fe3Fe2Fe3Fe2Fe3Fe2Fe3更高阶的拓学旋转纹理.斯基尔米昂斯斯基尔米昂斯应变工程是一种应变工程.更多相关视频
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