晶体和磁性结构和BiMnO ((3+delta) 的特性
Alexei A Belik1, Katsuaki Kodama, Naoki Igawa
1International Center for Materials Nanoarchitectonics (MANA), National Institute for Materials Science (NIMS), 1-1 Namiki, Tsukuba, Ibaraki 305-0044, Japan. Alexei.BELIK@nims.go.jp
晶体和磁性结构的比斯木 manganite (BiMnO(3+delta)) 使用中子衍射确定. 氧含量 (三角形) 影响晶体对称性,磁性排序和磁矩大小,其中BiMnO{3.14) 呈现出旋转玻璃状态.
科学领域:
- 固态化学 固态化学
- 材料科学 材料科学 材料科学
- 晶体学 晶体学是指结晶学.
- 磁力学 磁力学 是一种
背景情况:
- 石棉矿 (BiMnO(3+delta)) 是一种具有复杂晶体和磁性结构的材料.
- 众所周知,矿矿的性质对氧气固体测量和缺陷敏感.
研究的目的:
- 为了确定BiMnO的晶体和磁性结构(3+delta) 对于不同的氧含量 (delta = 0.03,0.08,0.14).
- 研究氧气固体测量对结构对称性,磁性排序和磁矩的影响.
- 为了比较BiMnO(3+delta) 的性能与相关的色矿 (LaMnO(3+delta)) 的性能.
主要方法:
- 在低温 (8-10 K) 和室温 (290 K) 收集的中子衍射数据的瑞特维尔德精细化.
- 分析晶体结构,包括空间组的确定和晶格参数.
- 确定磁性结构,磁性排序温度 (T) 和精细的磁矩.
主要成果:
- BiMnO ((3.03) 和BiMnO ((3.08) 在单临床系统中结晶 (C2 / c和P2 ((1) / c),分别表现出低于82 K和68 K的铁磁性,其磁矩在10 K时为2.88 ((2) μB和2.33 ((2) μB.
- Mn空缺位于特定的位置,可能导致观察到的晶体对称性变化.
- BiMnO(3.14) 结晶在一个正方体系统 (Pnma) 中,并表现出一个自旋玻璃的磁性状态,没有磁性排序到8K.
结论:
- 晶体结构的系统变化,磁性排序和BiMnO的磁性属性 ((3+delta) 强烈依赖氧含量 (delta).
- 建议空缺订单和收费订单作为观察到的结构转型的机制.
- 该研究提供了BiMnO(3+delta的详细结构和磁性表征,突出了其与氧气固体测量的可调性.
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