用偏振中子衍射-斜向顺磁体研究了[Fe(OD2)6]2+在塔顿亚铁铵中的磁化

B. Figgis, J. Forsyth, E. Kucharski, P. A. Reynolds, F. Tasset
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引用次数: 9

摘要

在1.5 K, 4.6 T的条件下,用磁场沿晶体b和c*轴取向的偏振中子衍射实验对氘化塔顿亚铁铵盐进行了研究。分别使用303和280个反射的翻转比,在消光校正后,得到磁性结构因子FM, Z(hkl) (eff)的唯一值为121和118。这些值被用于模型的细化,以描述晶体中的磁化密度。所有模型都导致顺磁体的磁化方向偏离磁场(37°和45°),相对于O6配体框架几乎恒定,表明铁原子位置的磁性各向异性很大。铁原子的磁化密度离域进入Fe-O重叠区(- 4.5%)和OD - 2配体(6.5%),其值与研究的其他Tutton盐中金属原子的自旋离域相当。早期基于光谱和磁数据的离子电子结构的配体场模型被证明是不充分的,因为它与铁原子周围磁化的各向异性不相容。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
The magnetization of [Fe(OD2)6]2+ in ammonium ferrous Tutton salt studied by polarized neutron diffraction - a canted paramagnet
A polarized neutron diffraction experiment has been done on deuterated ammonium ferrous Tutton salt at 1.5 K, 4.6 T with orientations of the magnetic field along the crystal b and c* axes. The flipping ratios of 303 and 280 reflections respectively were used, after correction for extinction, to give 121 and 118 unique values of the magnetic structure factor FM, Z(hkl) (eff). Those values were used in refinements of models for a description of the magnetization density in the crystal. All models resulted in substantial (37° and 45°) canting of the magnetization direction in the paramagnet away from the magnetic field, to an almost constant direction with respect to the O6 ligand framework, indicating large magnetic anisotropy at the iron atom sites. There is delocalization of magnetization density away from the iron atom into the Fe-O overlap region ( — 4.5%) and onto the OD 2 ligands (6.5%), values comparable with the delocalization of spin from the metal atom in other Tutton salts studied. An earlier ligand field model for the electronic structure of the ion based upon spectroscopic and magnetic data is shown to be inadequate, because it is incompatible with the observed anisotropy in the magnetization around the iron atoms.
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