低温拉曼光谱研究无声和自旋声合的近二维稀土基法兰西石矿
1Department of Physics, University of Calcutta, 92 A.P.C. Road, Kolkata 700009, India.
Journal of physics. Condensed matter : an Institute of Physics journal
|February 19, 2024
概括
弗朗西斯矿物中的稀土元素会影响磁性. DyCufr显示了与元磁转换相关的自旋声子合,而NdCufr则没有.
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
- 磁力学 磁力学 是一种
背景情况:
- 弗朗西斯石 (Cu3Bi(SeO3) 2O2Cl) 具有准二维结构和显著的磁性特征.
- 用稀土 (RE) 金属取代非磁性 (Bi) 引入了额外的磁中心,使磁性性能能够微调.
研究的目的:
- 调查稀土元素替代对法兰西石化合物的磁性和声子特性的影响.
- 探索旋声子合 (SPC) 和磁性转换之间的关系,特别是 induced-field-induced metamagnetic transitions (MMT) 的关系.
主要方法:
- 采用温度依赖的拉曼光谱法,研究基于RE的法兰西体 (RECufr) 中的音声振动,从11K到295K.
- 分析的重点是声软化和与磁性订序温度和MMT相关的无和性.
主要成果:
- 在研究的RECufr化合物中,自旋声子合 (SPC) 不同:在DyCufr中适度,在LaCufr中弱,在NdCufr中不存在.
- DyCufr 在其反铁磁排序温度 (T≈39 K) 下显示了两个拉曼活性声子的软化,表明中度SPC.
- 观察到MMT的强度和SPC的发展之间存在相关性,DyCufr中的强度MMT促进SPC,而NdCufr中的弱度MMT则没有.
结论:
- 弗朗西斯石的磁性特性可以通过稀土元素替代来调节,从而影响自旋声联.
- 旋声子合的存在和强度与磁性行为直接相关,特别是场诱导的超磁性转换.
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