压力调节的结构和磁相转换在二维的FeTe:四边形和六边形多态形态
Wuxiao Han1,2, Jiajia Feng3, Hongliang Dong3
1Advanced Research Institute of Multidisciplinary Sciences, Beijing Institute of Technology (ARIMS), Beijing 100081, China.
Nano letters
|January 11, 2024
概括
在压力下对二维 (2D) 铁化物 (FeTe) 的研究揭示了明显的磁过渡. 四边形FeTe在3GPa时从反铁磁转变为铁磁,而六边形FeTe保持铁磁性高达15GPa.
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) 铁素是理解复杂的过渡机制的关键.
- 这些材料有可能用于自旋电子和纳米电子应用.
- 水静压是诱导和研究材料相变的一个关键工具.
研究的目的:
- 系统地研究2D FeTe在极端条件下的结构演变和运输特性.
- 为了比较四边形 (t) 和六边形 (h) FeTe对称在压力下的行为.
- 为了映射t-FeTe和h-FeTe的温度-压力 (T-P) 阶段图.
主要方法:
- 在高水立压下对2D FeTe进行实验研究.
- 四角形和六角形FeTe之间的结构和运输特征的比较.
- 使用电传输测量和拉曼光谱来确认磁性状态.
主要成果:
- 四边形FeTe表现出由压力诱导的从反铁磁到铁磁状态的转变,约为3GPa,与结构崩有关.
- 六角FeTe保持其铁磁顺序高达15 GPa,通过运输和拉曼数据得到证实.
- 对t-FeTe和h-FeTe的详细TP相图成功地绘制出来.
结论:
- 该研究阐明了不同2D FeTe阶段的不同依赖压力的磁性行为.
- 这些发现为了解Fe chalcogenides的非凡特性提供了基础.
- 结果为开发自旋电子和纳米电子的先进应用铺平了道路.
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