不顺序的Nd0.5Ba0.5Mn0.5Fe0.5O3-δ/2和112型有序的NdBaMnFeO6-δ矿的对比磁性特性
Aslam Hossain1, Artem R Gilev2, Premakumar Yanda3
1Smart Materials Research Institute, Southern Federal University, Sladkova 178/24, Rostov-on-Don 344090, Russia.
ACS omega
|September 2, 2024
概括
无序的岩石表现出玻璃状和反铁磁状态,而有序的岩石则保持偏磁性. 氧化状态的变化驱动了Nd-Ba-Mn-Fe-O材料中的这些磁性.
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:
- 矿氧化物由于其多样性的特性,在材料科学中至关重要.
- 了解复杂矿的磁性行为是开发新磁性材料的关键.
研究的目的:
- 研究和比较无序和有序的Nd-Ba-Mn-Fe-O矿的磁性特性.
- 阐明这些材料中的结构秩序和磁性秩序之间的关系.
主要方法:
- 在不同的温度和磁场下进行了直流磁化测量.
- 分析了磁性易感性数据,以确定磁性排序温度和状态.
主要成果:
- 无序的Nd0.5Ba0.5Mn0.5Fe0.5O3-δ/2呈现出低于185K的反铁磁顺序,并在室温下呈现玻璃状.
- 订购的NdBaMnFeO6-δ在研究的温度范围内表现出一种超磁性状态.
- 无序的样本在更高的磁场下过渡到反铁磁状态.
结论:
- 结构障碍显著影响了Nd-Ba-Mn-Fe-O矿的磁性.
- 观察到的磁性行为与氧化状态的变化有关.
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