论文标题
对有序双钙岩Sr2ybruo6的磁接地状态的调查:两个过渡的故事
Investigation of the magnetic ground state of the ordered double perovskite Sr2YbRuO6: a tale of two transitions
论文作者
论文摘要
通过批量测量支持的全面的MUON自旋旋转/松弛(MUSR)和中子粉末衍射(NPD)研究已在有序的双钙钛矿SR2YBRUO6上进行了研究,以研究磁场状态的性质。在TN1〜42 K和TN2〜36 K处的两个急剧过渡已在静态和动态磁化测量中观察到,与热容量数据一致。为了确认观察到的相变和磁接地态的起源,这里介绍了微观证据。远距离磁性排序的初始指示来自MUON初始不对称性的急剧下降,而TN1附近的松弛率峰值。 NPD证实SR2YBRUO6的磁接地态由抗铁磁(AFM)结构组成,其结构具有平行Yb3+和Ru5+矩的互穿晶格,位于AB-Plane中并采用A-Type AFM结构。有趣的是,在TN2的远程排序参数中观察到了一个很小但显着的变化,证实了RU和YB矩的存在弱自旋重新定位(即自旋构型的变化),以及TN2 YB3+旋转的磁矩演变的变化。 YB3+和RU5+矩的温度依赖性行为表明RU5+的4D电子在稳定双钙钛矿SR2YBRUO中的远距离有序磁场状态方面起着主导作用,而仅YB3+矩显示在TN2处仅显示YB3+矩。通过使用Goodenough-kanamori-Anderson(GKA)规则来解释观察到的磁结构和RU-和YB离子之间的铁磁相互作用。在磁化数据中存在第二磁相变和补偿点的可能原因与磁各向异性的竞争机制有关。
Comprehensive muon spin rotation/relaxation (muSR) and neutron powder diffraction (NPD) studies supported via bulk measurements have been performed on the ordered double perovskite Sr2YbRuO6 to investigate the nature of the magnetic ground state. Two sharp transitions at TN1 ~ 42 K and TN2 ~ 36 K have been observed in the static and dynamic magnetization measurements, coinciding with the heat capacity data. In order to confirm the origin of the observed phase transitions and the magnetic ground state, microscopic evidences are presented here. An initial indication of long-range magnetic ordering comes from a sharp drop in the muon initial asymmetry and a peak in the relaxation rate near TN1. NPD confirms that the magnetic ground state of Sr2YbRuO6 consists of an antiferromagnetic (AFM) structure with interpenetrating lattices of parallel Yb3+ and Ru5+ moments lying in the ab-plane and adopting a A-type AFM structure. Intriguingly, a small but remarkable change is observed in the long-range ordering parameters at TN2 confirming the presence of a weak spin reorientation (i.e. change in spin configuration) transition of Ru and Yb moments, as well as a change in the magnetic moment evolution of the Yb3+ spins at TN2. The temperature dependent behaviour of the Yb3+ and Ru5+ moments suggests that the 4d-electrons of Ru5+ play a dominating role in stabilizing the long range ordered magnetic ground state in the double perovskite Sr2YbRuO6 whereas only the Yb3+ moments show an arrest at TN2. The observed magnetic structure and the presence of a ferromagnetic interaction between Ru- and Yb- ions are explained with use of the Goodenough-Kanamori-Anderson (GKA) rules. Possible reasons for the presence of the second magnetic phase transition and of a compensation point in the magnetization data are linked to competing mechanisms of magnetic anisotropy.