在铁磁单层Fe3GeTe2中,压力诱导的极性金属相
Xiaoyan Miao1, Si Li1,2, Zhenyi Jiang1
1School of Physics, Northwest University, Xi'an 710127, China. chunmeizhang@nwu.edu.cn.
Physical chemistry chemical physics : PCCP
|July 5, 2023
概括
铁磁铁 Telluride (Fe3GeTe2) 单层上的压缩应变会产生磁极金属. 这个阶段结合了极化,金属性和铁磁性,用于自旋电子应用.
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
- 固态化学 固态化学
背景情况:
- 铁磁Fe3GeTe2单层正在积极研究其电子和磁性特性.
- 在基板上的实验生长过程中,外部压力是不可避免的因素.
- 应变对Fe3GeTe2特性的影响尚不清楚.
研究的目的:
- 研究外部应变对Fe3GeTe2单层结构,电子和磁性特性的影响.
- 探索创造具有独特性质的新型材料相的潜力.
主要方法:
- 使用密度函数理论 (DFT) 的计算.
- 在应变下对晶体配置和电子结构的系统研究.
主要成果:
- 适度的压力应变打破了垂直对称性,诱导了平面外的二极极矩.
- 铁磁性在应力下保持不变.
- 在Fe和Ge原子中,应变诱导的极化对费米水平状态的影响最小.
- 实现了磁极金属的独特阶段,解导电性和极化.
结论:
- 张力Fe3GeTe2单层表现出极化,金属性和铁磁性的罕见组合.
- 这种材料阶段对磁电和自旋电子的应用具有前景.
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