在Sm-doped NdFeO3中调整旋转重定向和旋转切换
Sk Samim Ahammad1, C M N Kumar2, Michał Rams3
1Department of Physics, Indian Institute of Science, Bangalore, Karnataka, 560012, India. sksamima@iisc.ac.in.
稀土石的合精确控制了磁性转换. 一种新的负场冷却方法调整了自旋切换温度,超过了先进材料的158K记录范围.
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:
- 稀土形铁素对于功能磁性材料至关重要.
- 调整磁过渡,如旋转重定向 (SRT) 和旋转切换 (SSW) 是高级应用的关键.
- Nd1-xSmxFeO3系统为研究这些现象提供了一个平台.
研究的目的:
- 在Nd1-xSmxFeO3单晶中研究SRT和SSW的演变.
- 了解Sm3+兴奋剂对磁过渡温度的影响.
- 展示一种用于控制旋转切换温度 (TSSW) 的新方法.
主要方法:
- Nd1-xSmxFeO3 (x = 0.1,0.3,0.5) 的单晶使用光学浮带炉生长.
- 进行结构分析以确认格子参数.
- 通过使用可变温度测量来研究磁性过渡温度.
主要成果:
- Sm3+兴奋剂诱导了系统的晶格收缩和受控的SRT温度.
- 24的共存区域随着Sm3+度的增加而缩小.
- 一个负场冷却协议使TSSW能够在前所未有的158K范围内调整TSSW, -20 Oe.
结论:
- 通过Sm3+的兴奋剂进行组合工程,可以精确地控制稀土形铁的磁转换.
- 演示的场冷却协议为调整磁性功能提供了一个强大的策略.
- 这些发现为开发用于先进应用的新型磁性材料铺平了道路.
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