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低维氟化物β-FeF₃(H₂O)₂·H₂O的结构和磁性特性

Structural and magnetic properties of the low-dimensional fluoride β-FeF3(H2O)2·H2O.

作者信息

Nénert Gwilherm, Fabelo Oscar, Forsberg Kerstin, Colin Claire V, Rodríguez-Carvajal Juan

机构信息

PANalytical B. V., Lelyweg 1, 7602 EA Almelo, The Netherlands.

出版信息

Dalton Trans. 2015 Aug 21;44(31):14130-8. doi: 10.1039/c5dt02242h.

Abstract

We have reinvestigated the crystal structure of the low-dimensional fluoride β-FeF3(H2O)2·H2O using high resolution neutron and X-ray diffraction data. Moreover we have studied the magnetic behavior of this material combining medium resolution and high flux neutron powder diffraction together with magnetic susceptibility measurements. This fluoride compound exhibits vertex-shared 1D Fe(3+) octahedral chains, which are extended along the c-axis. The magnetic interactions between adjacent chains involve super-superexchange interactions via an extensive network of hydrogen bonds. This interchain hydrogen bonding scheme is sufficiently strong to induce a long range magnetic order appearing below T = 20(1) K. The magnetic order is characterized by the propagation vector k = (0, 0, 1/2), giving rise to a strictly antiferromagnetic structure where the Fe(3+) spins are lying within the ab-plane. Magnetic exchange couplings extracted from magnetization measurements are found to be J∥/kb = -18 K and J⊥/kb = -3 K. These values are in good agreement with the neutron diffraction data, which show that the system became antiferromagnetically ordered at ca. TN = 20(1) K.

摘要

我们利用高分辨率中子和X射线衍射数据,对低维氟化物β-FeF₃(H₂O)₂·H₂O的晶体结构进行了重新研究。此外,我们结合中分辨率和高通量中子粉末衍射以及磁化率测量,研究了该材料的磁行为。这种氟化物化合物呈现出沿c轴延伸的顶点共享一维Fe(3+)八面体链。相邻链之间的磁相互作用涉及通过广泛氢键网络的超超交换相互作用。这种链间氢键方案足够强,可诱导在T = 20(1) K以下出现长程磁有序。磁有序的特征是传播矢量k = (0, 0, 1/2),产生一种严格的反铁磁结构,其中Fe(3+)自旋位于ab平面内。从磁化测量中提取的磁交换耦合被发现为J∥/kb = -18 K和J⊥/kb = -3 K。这些值与中子衍射数据吻合良好,中子衍射数据表明该系统在约TN = 20(1) K时变为反铁磁有序。

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