在高度失序的脊柱铁矿中保护高度的磁性转换
Lujin Min1,2, John P Barber3,4, Yu Wang1,5
1Department of Physics, Pennsylvania State University, University Park, Pennsylvania 16802, United States.
Journal of the American Chemical Society
|August 20, 2024
概括
具有高度和高无序的氧化物表现出明显的磁性转变. 合成单晶揭示了随机元素分布,增强了同质性,并保持了磁性排序,开辟了新的研究途径.
科学领域:
- 材料科学
- 凝聚物质物理学
- 固态化学
背景情况:
- 研究对材料磁性排序的影响至关重要.
- 高氧化物 (HEO) 呈现极端混乱的密度,使磁性行为复杂化.
- 由于缺乏高质量的单晶,对HEO组成障碍的影响进行了深入的研究.
研究的目的:
- 合成高质量的单晶高旋铁.
- 调查构成障碍对高温体磁转换的影响.
- 了解 HEO 中元素分布和磁性排序之间的关系.
主要方法:
- 单晶高旋铁素 (Mg0.2Mn0.2Fe0.2Co0.2Ni0.2) Fe3-xO4 的合成
- 高温磁化测量
- 进行中子衍射实验.
- 扩展X射线吸收细结构 (EXAFS) 的测量.
主要成果:
- 在748K (x=1),694K (x=1.5) 和674K (x=1.8) 观察到的铁磁过渡.
- 与Fe3O4不同的是,磁性转换显示了x=1和x=1.5的最小扩展.
- EXAFS显示了随机元素分布,减少了局部集群和短距离订单.
- 提高了样本的均性,并保持了强烈的磁性转换,尽管结合长度有所变化.
结论:
- 首个具有远程磁性秩序的HEO散装单晶的成功合成.
- 在HEOs中随机元素分布增强了同质性,并加剧了磁性转换.
- 在HEO中显示高配置和磁性排序之间的相互作用.
- 开辟了磁性高氧化物研究和应用的新途径.
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