论文标题
稀土铁石榴石中伞状状态的起源和动力学
Origin and dynamics of umbrella states in rare-earth iron garnets
论文作者
论文摘要
稀有地球的铁石榴石$ r_ {3} $ fe $ _ {5} $ o $ _ {12} $是具有非常多样化的磁性阶段的迷人绝缘子。它们在自旋设备中的强大潜力鼓励了对其低温自旋结构和自旋波动力学的研究更新的兴趣。具有$ r $ $ $的稀土石榴石的引人注目的特征,表现出强烈的晶体场作用,例如TB-,Dy-,Ho-和Er-ions,是对具有稀有磁性力矩的“伞状”布置的低温非同性恋磁性结构的观察。在这项研究中,我们证明了这种伞状磁态自然是从稀土离子的晶体场各向异性中出现的。通过仅赋予晶体结构中必要元素的一般模型,我们展示了如何进行类似伞状的自旋结构,并通过稀有地球与铁离子与铁离子以及晶体场各向异性之间的竞争而进行倾斜角度。将我们的结果与实验数据进行了比较,并提出了对偏振旋转波动力学的研究。我们的研究提高了对伞状的旋转结构的理解,并为具有非固定磁相的稀土铁石榴石中的更复杂的自旋波计算铺平了道路。
Rare-earth iron garnets $R_{3}$Fe$_{5}$O$_{12}$ are fascinating insulators with very diverse magnetic phases. Their strong potential in spintronic devices has encouraged a renewal of interest in the study of their low temperature spin structures and spin wave dynamics. A striking feature of rare-earth garnets with $R$-ions exhibiting strong crystal-field effects like Tb-, Dy-, Ho-, and Er-ions is the observation of low-temperature non-collinear magnetic structures featuring "umbrella-like" arrangements of the rare-earth magnetic moments. In this study, we demonstrate that such umbrella magnetic states are naturally emerging from the crystal-field anisotropies of the rare-earth ions. By means of a general model endowed with only the necessary elements from the crystal structure, we show how umbrella-like spin structures can take place and calculate the canting-angle as a result of the competition between the exchange-interaction of the rare-earth and the iron ions as well as the crystal-field anisotropy. Our results are compared to experimental data, and a study of the polarised spin wave dynamics is presented. Our study improves the understanding of umbrella-like spin structures and paves the way for more complex spin wave calculations in rare-earth iron garnets with non-collinear magnetic phases.