在B20非中心对称的CoSi中,Gd替代引发了不相称的反铁磁性
Ravi Kumar Kalabarigi1,2, S Shanmukharao Samatham3,4, S Shravan Kumar Reddy3
1AU Trans-Disciplinary Research Hub, Andhra University, Visakhapatnam 530 003, Andhra Pradesh, India.
概括
加多化的化 (Co1-xGdxSi) 呈现复杂的磁性过渡,包括两个不同的反铁磁相. 这项研究探讨了用于新型磁性材料的过渡金属单化物中的稀土兴奋剂.
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:
- 过渡金属单化物是一种具有有趣磁性质的材料.
- 稀土元素兴奋剂提供了一条调整和设计这些化合物的磁性行为的途径.
研究的目的:
- 为了研究加多 (Gd) 合的化 (Co1-xGdxSi,x=0.01) 的结构和磁性特性.
- 探索稀土替代在过渡金属单化物中的潜力,以开发新型磁性材料.
主要方法:
- 采用X射线衍射来确定晶体结构和晶格参数.
- 磁化测量是根据温度和磁场 (T-H相图) 进行的.
主要成果:
- Co1-xGdxSi合金在B20立方结构中结晶,其晶格参数为a=4.4429 Å.
- 在38.44K (AFM-I) 和21.87K (AFM-II) 观察到两个反铁磁 (AFM) 过渡.
- 观察到磁化在9.79K以下的上升和场诱导的过渡,表明复杂的磁性排序.
结论:
- 该研究揭示了Gd-doped CoSi中复杂的磁相过渡,包括不相称和弱相关的AFM状态.
- 在高磁场下,AFM-I状态转变为铁磁状态,突出显示可调节的磁性特性.
- 在过渡金属单化物中用稀土进行兴奋剂是一种有前途的战略,用于发现异国情调的磁性材料.
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