在NiI中,令人惊的压力诱导的磁变化从磁体秩序转变为反铁磁状态
Qiye Liu1,2, Wenjie Su2, Yue Gu3
1College of Integrated Circuits and Optoelectronic Chips, Shenzhen Technology University, Shenzhen, 518118, China.
Nature communications
|May 6, 2025
概括
水静压调整了NiI2片中的磁相互作用,增加了过渡温度. 在7GPa时,可逆的磁到反铁磁 (AFM) 阶段过渡突出了层间磁合的关键作用.
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
- 磁力学 磁力学 是一种
背景情况:
- 范德瓦尔斯 (vdW) 磁铁表现出独特的磁性特性,受层间相互作用的影响.
- 施加压力是调整这些层间磁相互作用和磁顺序的强大工具.
- 了解压力诱导的磁相过渡对于新型设备应用至关重要.
研究的目的:
- 为了研究水静压对NiI2 vdW磁铁磁性特性的影响.
- 探索压力诱导的磁和反铁磁 (AFM) 状态之间的相位过渡.
- 阐明层间磁相互作用在确定NiI2.2的磁性基本状态中的作用.
主要方法:
- 在高达11 GPa的水静压下对NiI2片进行实验性研究.
- 对黑磁和反铁磁状态的磁过渡温度的分析.
- 蒙特卡洛模拟以模拟层间相互作用对磁性排序的影响.
主要成果:
- 观察到磁性过渡温度的显著增加,无论是磁极和AFM状态,压力都在增加.
- 发现了可逆的黑磁到AFM相位过渡在7GPa左右,挑战了现有的理论.
- 蒙特卡洛模拟证实了第二近邻邻层间相互作用在有利于AFM状态而不是层内挫折的关键作用.
结论:
- 层间的磁相互作用对于决定像NiI2.2这样的vdW磁铁的磁性基态至关重要.
- 观察到的压力诱导相位过渡为磁性排序机制提供了新的见解.
- 这些发现为通过控制层间合来设计先进的纳米磁器件提供了机会.
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