间层离子控制在12R-Ba4MMn3O12 (M = Ce, Pr) 层叠的矿中低维的旋转曲线
Corlyn E Regier1, Shaun O'Donnell2, Anuj Goyal2,3
1Department of Chemistry, Colorado State University, Fort Collins, Colorado 80523, United States.
Inorganic chemistry
|December 7, 2024
概括
研究人员研究了磁性六角矿,12R-Ba4MMn3O12. 他们发现,磁性介层离子改变了自旋方向,影响了磁性,并为设计新的磁性材料提供了洞察力.
科学领域:
- 材料科学 材料科学 材料科学
- 固态物理 固态物理
- 磁力学 磁力学 是一种
背景情况:
- 了解结构属性关系对于设计具有特定磁性质的材料至关重要.
- 层叠的六角矿石的磁性,特别是12R-Ba4MMn3O12家族的磁性,尚未得到充分理解.
- 本研究的重点是12R-Ba4MMn3O12家族,其中M=Ce4+ (二磁性) 和M=Pr4+ (重磁性).
研究的目的:
- 为了对12R-Ba4MMn3O12材料进行详细的磁结构研究.
- 阐明晶体结构,电子结构和磁性质之间的关系.
- 为了确定这些化合物的磁性结构.
主要方法:
- 可变温度粉末中子衍射以确定磁性结构.
- 粉末X射线衍射用于晶体结构分析.
- 射线吸收光谱学和电子结构特征的第一原则计算.
主要成果:
- 基于Ce的材料在7.75K以下具有抗铁磁性.
- 基于 Pr 的材料表现出复杂的磁性行为,净矩低于 200 K,反铁磁过渡在 12.15 K.
- 磁性中间层的离子会诱导Mn3O12三元体内旋转的外平面倾斜.
结论:
- 该研究提供了12R-Ba4MMn3O12.12的磁性,晶体和电子结构的详细图像.
- 这些发现提供了对六角矿层叠层叠的磁性的洞察.
- 这项工作作为理解和设计相关磁性材料的基础.
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