一个非中心对称的FeCl多态的磁性特性3
Joshua J B Levinsky1,2, Ankit Labh3,4,5, Vladimir Pomjakushin6
1Zernike Institute for Advanced Materials, University of Groningen Nijenborgh 3 9747AG Groningen The Netherlands g.r.blake@rug.nl.
概括
研究人员生长了FeCl3单晶,并发现了一种新的性多态. 中子散射揭示了磁过渡和场诱导的自旋重定位,与已知的结构不同.
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
- 晶体学 晶体学是指结晶学.
背景情况:
- 铁 (III) 化物 (FeCl3) 是一种经过充分研究的材料,具有已知的磁性.
- 了解FeCl3中的磁结构关系对于开发新的磁性材料至关重要.
研究的目的:
- 为了合成FeCl3.3的单晶.
- 为了研究FeCl3多态体的磁结构性质.
- 为了确定FeCl3.3的新晶体和磁性相.
主要方法:
- 单晶通过升华和融方法生长.
- 测量直流磁化和交流磁性易感度.
- 单晶X射线衍射 (SCXRD) 方法.
- 中子粉衍射 (NPD) 和小角度中子散射 (SANS).
主要成果:
- 确定了一种新的性FeCl3多态,在P31空间组中结晶.
- 在TN = 8.6K时观察到一个弱的第一阶段磁相过渡到反铁磁状态,具有独特的磁传播向量k = (1/2,0,1/3).
- 观察到场诱导的旋转重定位,不同的临界场取决于相对于c轴的磁场方向.
结论:
- 这项研究揭示了FeCl3具有明显的磁性排序的新奇性多态形态.
- 无序的晶体模型是准确的NPD数据解释所必需的.
- FeCl3表现出复杂的磁性行为,包括场诱导的旋转重定位,突出其用于先进磁性应用的潜力.
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