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圆偏振X射线的共振和非共振磁散射:钆铁石榴石的磁散射因子和电子密度

Resonant and non-resonant magnetic scatterings with circularly polarized X-rays: magnetic scattering factor and electron density of gadolinium iron garnet.

作者信息

Sasaki Yo, Okube Maki, Sasaki Satoshi

机构信息

Materials and Structures Laboratory, Tokyo Institute of Technology, Nagatsuta 4259, Yokohama, 226-8503, Japan.

出版信息

Acta Crystallogr A Found Adv. 2017 May 1;73(Pt 3):257-270. doi: 10.1107/S2053273317003588. Epub 2017 Apr 27.

Abstract

Theoretical and experimental studies on resonant magnetic scattering have been carried out using circularly polarized X-rays. Polarization dependence of the asymmetric ratio between right- and left-handed polarized scattering amplitudes has revealed that resonant and non-resonant magnetic scatterings can be observed simultaneously. In this study, synchrotron X-ray intensity experiments were conducted on Gd iron garnet (GdIG) at the pre-edge of the Fe K absorption edge. The asymmetric ratio between circular polarizations exhibited three peaks due to the resonant magnetic responses of Fe in the Fe2 (24d) site. These magnetic responses are antiparallel and have apparently higher resolution than dispersive X-ray magnetic circular dichroism at the pre-edge region; this can be mainly attributed to electric dipole transitions from 1s to t energy levels of the 3d orbitals in the tetrahedral symmetry in an unstable state quenched at higher temperature. Resonant magnetic scattering factors f' were estimated from the asymmetric ratios. Fourier analysis was conducted using the intensity differences among circularly polarized X-rays at an energy of E = 7.1085 keV. At this energy level, the characteristic distribution of magnetic electron density was clearly observed. This distribution was interpreted as a spin arrangement of Gd and Fe ions in GdIG. Also observed was the presence of hybridization of the magnetic electron orbitals as well as of the resonant magnetic Fe. The proposed method has the potential to be widely used in crystal structure analysis.

摘要

利用圆偏振X射线对共振磁散射进行了理论和实验研究。右旋和左旋偏振散射振幅之间不对称比的偏振依赖性表明,可以同时观察到共振和非共振磁散射。在本研究中,在Fe K吸收边的前缘对钆铁石榴石(GdIG)进行了同步加速器X射线强度实验。由于Fe2(24d)位点中Fe的共振磁响应,圆偏振之间的不对称比呈现出三个峰值。这些磁响应是反平行的,并且在边缘前区域具有比色散X射线磁圆二色性明显更高的分辨率;这主要可归因于在较高温度下淬灭的不稳定状态下,从1s到四面体对称性中3d轨道的t能级的电偶极跃迁。从不对称比估计共振磁散射因子f'。使用能量为E = 7.1085 keV的圆偏振X射线之间的强度差异进行傅里叶分析。在这个能量水平上,清楚地观察到了磁电子密度的特征分布。这种分布被解释为GdIG中Gd和Fe离子的自旋排列。还观察到了磁电子轨道以及共振磁Fe的杂化现象。所提出的方法有潜力在晶体结构分析中得到广泛应用。

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