从斯通纳到局部电流磁力在原子薄的Cr2中
Yong Zhong1,2,3, Cheng Peng4, Haili Huang5
1Advanced Light Source, Lawrence Berkeley National Laboratory, Berkeley, CA, 94720, USA. ylzhong@stanford.edu.
Nature communications
|September 2, 2023
概括
原子薄的 Telluride (Cr2Te3) 薄膜表现出厚度依赖的铁磁性,从石头转变为海森堡型. 单层Cr2Te3显示强大的铁磁性与较低的基里温度,为2D磁性研究提供了一个平台.
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
- 这就是Spintronics.
背景情况:
- 二维 (2D) 铁磁是一种快速发展的领域,对自旋电子技术有着重大影响.
- 对二维铁磁体的高分辨率光谱研究受到纳米尺寸和空气灵敏度的限制.
研究的目的:
- 为了研究厚度依赖的铁磁性和电子结构进化在生长的Cr2Te3薄膜.
- 在二维极限中探索斯通纳和海森伯格类型磁力之间的过渡.
- 建立Cr2Te3作为一种模型系统,用于研究2D材料中的局部和流动铁磁.
主要方法:
- 协同使用角度分辨率光辐射光谱学 (ARPES) 和扫描道显微镜 (STM).
- 用于电子结构分析的X射线吸收光谱 (XAS).
- 为了补充实验发现的第一原则计算.
主要成果:
- 在原子薄的Cr2Te3.3中直接观察从斯通纳到海森伯格型的铁磁过渡.
- 单层Cr2Te3具有强大的铁磁性,但其基里温度较低.
- 接近费米水平的状态密度的显著下降与单层膜中抑制的基里温度相关.
结论:
- 维度是调整二维磁性的关键因素.
- 原子薄的Cr2Te3是探索局部和流动铁磁的相互作用的优秀平台.
- 这些发现为使用二维磁性材料的新型自旋电子应用铺平了道路.
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