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首页> 外文期刊>International Journal of Quantum Chemistry >Neutron powder diffraction study of the layer organic–inorganic hybrid iron(II) methylphosphonate-hydrate, Fe[(CD3PO3)(D2O)]
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Neutron powder diffraction study of the layer organic–inorganic hybrid iron(II) methylphosphonate-hydrate, Fe[(CD3PO3)(D2O)]

机译:有机-无机杂化膦酸铁-水合物Fe [(CD3PO3)(D2O)]层的中子粉末衍射研究

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摘要

The crystal and magnetic structures of the hybrid organic–inorganic layer compound Fe[(CD3PO3)(D2O)] have been studied by neutron powder diffraction as a function of temperature down to 1.5 K. The neutron diffraction pattern recorded at 200 K shows that the fully deuterated compound crystallizes in one of the two known forms of the undeuterated Fe[(CH3PO3)(H2O)]. The crystal structure is orthorhombic, space group Pmn21, with the following unit-cell parameters: a=5.7095(1) ?, b=8.8053(3) ? and c=4.7987(1) ?; Z=2. The crystal structure remains unchanged on cooling from 200 to 1.5 K. Moreover, at low temperature, Fe[(CD3PO3)(D2O)] shows a commensurate magnetic structure (k=(0,0,0)). As revealed by bulk susceptibility measurements on Fe[(CH3PO3)(H2O)], the magnetic structure corresponds to a canted antiferromagnet with a critical temperature TN=25 K. Neutron powder diffraction reveals that below TN=23.5 K the iron magnetic moments in Fe[(CD3PO3)(D2O)] are antiferromagnetically coupled and oriented along the b-axis, perpendicular to the inorganic layers. No ferromagnetic component is observable in the neutron powder diffraction experiment, due to its too small value (<0.1μB).
机译:通过中子粉末衍射研究了低至1.5 K的温度,研究了有机-无机杂化层化合物Fe [(CD3PO3)(D2O)]的晶体和磁性结构。200K记录的中子衍射图表明完全氘代的化合物以未氘化的Fe [(CH3PO3)(H2O)]的两种已知形式之一结晶。晶体结构为正交晶系,空间群Pmn21,具有以下晶胞参数:a = 5.7095(1),b = 8.8053(3)。和c = 4.7987(1)?; Z = 2。在从200 K冷却到1.5 K时,晶体结构保持不变。此外,在低温下,Fe [(CD3PO3)(D2O)]显示出相当的磁性结构(k =(0,0,0))。如对Fe [(CH3PO3)(H2O)]的磁化率测量所揭示的,磁性结构对应于临界温度TN = 25 K的倾斜反铁磁体。中子粉末衍射表明,在TN = 23.5 K以下,Fe中的铁磁矩[(CD3PO3)(D2O)]反铁磁耦合并沿b轴定向,垂直于无机层。由于中子粉末衍射值太小(<0.1μB),因此在中子粉末衍射实验中没有观察到铁磁成分。

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