铁谷物理学在堆叠的双层变磁系统中
Yun-Qin Li1,2, Yu-Ke Zhang1, Xin-Le Lu1
1Key Laboratory of Polar Materials and Devices (MOE), School of Physics and Electronic Science and Shanghai Center of Brain-inspired Intelligent Materials and Devices, East China Normal University, Shanghai 200241, China.
Nano letters
|April 7, 2025
概括
在变磁体中滑动的间层可以诱导和控制大谷极化. 这一发现为旋转电子学和山谷电子学开辟了新的途径,通过将旋转,山谷,层和光学属性关联起来.
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
背景情况:
- 变磁体是一种新兴的磁相,具有补偿的磁顺序和非相对论的自旋分裂.
- 众所周知,应变工程可以在变磁体中诱导谷极化,但可控制的切换仍然是一个挑战.
研究的目的:
- 提出和研究层间滑动作为一种诱导和操纵变磁体中山谷偏振的方法.
- 探索Fe2MX4 (M = Mo,W; X = S,Se,Te) 对国家铁路的潜力.
主要方法:
- 严格约束的模型计算.
- 第一原则计算.第一原则计算.
主要成果:
- 层间滑动成功诱导并有效地操纵了变磁体中的大谷极化.
- 滑动诱导的铁路山谷状态表现出独特的特性,如旋转轨道合独立的线性光学二极化和异常的山谷霍尔效应.
- 在Fe2MX4家族中展示了潜力.
结论:
- 层间滑动提供了一条可行的路线,用于在变磁体中可控制的山谷偏振.
- 这些发现强调了旋转,谷,层和光学自由度之间的相关性.
- 变磁体在旋转电子,山谷电子及其混合领域的应用方面表现有前途.
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