范德瓦尔斯的铁磁主导的铁-间隙 Fe Fe Fe Fe 的铁磁
Yueshen Wu1, Yuxiong Hu1, Cong Wang2,3
1School of Physical Science and Technology, ShanghaiTech University, Shanghai, 201210, China.
Advanced materials (Deerfield Beach, Fla.)
|June 7, 2023
概括
具有较高基里温度的铁 telluride (Fe3GeTe2) 晶体表现出 Fe-intercalation,导致交换偏差效应. 这种间歇机制解释了Fe3GeTe2.2中增强的磁性排序和变化的基里温度.
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:
- Fe3GeTe2 呈现出有趣的磁性,但其变量库里温度 (Tc) 背后的机制尚未完全理解.
- 了解影响Tc的因素对于旋转电子设备的潜在应用至关重要.
研究的目的:
- 研究不同基里温度的Fe3GeTe2晶体的原子结构和磁性.
- 阐明导致Tc值变化的潜在机制.
主要方法:
- 用Tc值为160K,210K和230K的Fe3GeTe2晶体进行元素映射.
- 电力运输测量以检测交换偏差效应.
- 第一个原则计算模型磁性合和层间相互作用.
主要成果:
- 在高Tc (210和230K) Fe3GeTe2样本的范德瓦尔斯间隙中观察到Fe-间隙.
- 高Tc样本表现出交换偏差效应,低Tc (160K) 样本没有这种效应.
- 第一个原则的计算表明,Fe-intercalation诱导局部反铁磁合,并通过层间交换路径增强Tc.
结论:
- 在Fe3GeTe2中的Fe间歇被确定为观察到的交换偏差效应的关键机制.
- 这种间隔层和相关的反铁磁排序解释了Fe3GeTe2.2中增强的基里温度.
- 这项研究澄清了隐藏的反铁磁排序,有助于提高Fe3GeTe2.2中的Tc.
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