在堆叠依赖的二维材料中共存磁力,铁电和铁谷多铁力
Wei Xun1,2, Chao Wu1, Hanbo Sun1
1State Key Laboratory for Mechanical Behavior of Materials, Center for Spintronics and Quantum System, School of Materials Science and Engineering, Xi'an Jiaotong University, Xi'an, Shaanxi 710049, People's Republic of China.
Nano letters
|March 7, 2024
概括
研究人员建议在二维双层材料中进行层间滑动,以合磁性,铁电和谷极化. 这一发现为电子和自旋电子学中的新型多铁子装置铺平了道路.
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:
- 二维 (2D) 多铁材料对于先进的纳米设备至关重要.
- 在单一的二维材料中将磁性,铁电性和铁路性质结合在一起仍然是一个挑战.
研究的目的:
- 提出和研究一种机制来操纵2D材料中的合多铁性质.
- 探索层间滑动的潜力,以调节和可逆控制磁性,铁电和山谷极化.
主要方法:
- 在二维双层材料中滑动介层的理论建议.
- 使用理论计算,研究单层和双层GdI2的特性.
- 通过自旋哈密尔顿和层间电子跳跃来分析磁性相位过渡.
主要成果:
- 单层GdI2表现出铁磁半导体行为,具有显著的谷极化 (高达155.5 meV).
- 比拉耶GdI2展示了磁力和山谷极化之间强烈的合,可通过铁电滑动调节和可逆.
- 阐明了磁相转换的微观机制.
结论:
- 层间滑动提供了一种新的途径,可以在2D材料中实现合的多铁性质.
- 这些发现为开发下一代电子,谷电和旋电设备提供了新的方向.
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