巨大的自旋效应在Kagome螺旋磁铁中
Xitong Xu1,2, Yonglai Liu3,4, Kesen Zhao3,4
1Anhui Key Laboratory of Low-Energy Quantum Materials and Devices, High Magnetic Field Laboratory, HFIPS, Chinese Academy of Sciences, Hefei, Anhui, 230031, China. xuxitong@hmfl.ac.cn.
Nature communications
|March 18, 2025
概括
研究人员在kagome磁铁中发现了自旋效应,特别是TmMn6Sn6. 这种内在效应导致巨型电磁阻 (GMR) 比率超过160%,为新型自旋电子应用铺平了道路.
科学领域:
- 凝聚物质物理学 凝聚物质物理学
- 量子材料科学 量子材料科学
背景情况:
- 卡戈梅磁体为探索量子现象提供了一个独特的平台,因为它们结合了非微不足道的波段拓和电子相关性.
- 在kagome磁体中挫败的层间相互作用被研究了它们的潜力,以容纳新的量子效应.
研究的目的:
- 提出和实验验证kagome磁铁内在自旋效应的存在.
- 研究在应用磁场下的TmMn6Sn6的行为及其对自旋电子应用的潜力.
主要方法:
- 在挫败的Kagome磁铁中,自旋效应的理论建议.
- 实验证实使用Kagome头磁铁TmMn6Sn6.
- 磁力显微镜用于在垂直磁场下观察域结构.
主要成果:
- 在磁场下的TmMn6Sn6中,沿螺旋轴堆叠的条形域的观察.
- 这些域的归因是卡戈梅磁体状态中稳定性丧失.
- 由于内在的旋转效应和高旋转极化,实现了超过160%的巨型磁阻 (GMR) 比率.
结论:
- 卡戈梅磁铁与挫败的层间相互作用可以本质上表现出自旋效应.
- TmMn6Sn6作为这种现象的实验演示,模仿人工旋转.
- 这一发现为开发量子磁铁内在的自旋为未来的自旋电子学开辟了新的可能性.
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