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首页> 外文期刊>International Journal of Quantum Chemistry >STRUCTURAL CHEMISTRY AND ELECTRONIC PROPERTIES OF Sr2FeIrO6
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STRUCTURAL CHEMISTRY AND ELECTRONIC PROPERTIES OF Sr2FeIrO6

机译:Sr2FeIrO6的结构化学和电子性质

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摘要

A polycrystalline sample of Sr2FeIrO6 has been synthesized and shown by a combination of XRD, neutron diffraction, magnetometry, and Mossbauer spectroscopy to be a triclinic (space group I-1; a=5.54996(3) angstroms, b=5.57847(3) angstroms, c=7.84165(3) angstroms, alpha=89.990(1) degrees, beta=90.059(1) degrees, gamma=90.079(1) degrees) perovskite, with a partially ordered (0.928:0.072(4)) distribution of transition metal cations over the six-coordinate sites. The predominant oxidation states are Fe3+ and Ir5+, although the Mossbauer data suggest that approx 4% Fe4+ is present. The compound is a Type II antiferromagnet below 120 K, with an ordered magnetic moment on the Fe-dominated sites of 3.67(3) mu B per Fe3+ cation. The spins associated with the antisite defects are frustrated and do not take part in the long-range magnetic ordering, consequently giving rise to hysteresis in the magnetic susceptibility below 40 K. The possible location of the Fe4+ cations is discussed briefly. 19 refs.
机译:合成了Sr2FeIrO6的多晶样品,并通过XRD,中子衍射,磁力法和Mossbauer光谱法显示为三斜晶系(空间群I-1; a = 5.54996(3)埃,b = 5.57847(3)埃,c = 7.84165(3)埃,alpha = 89.990(1)度,beta = 90.059(1)度,gamma = 90.079(1)度钙钛矿,过渡部分分布(0.928:0.072(4))六个配位点上的金属阳离子。尽管Mossbauer数据表明存在大约4%的Fe4 +,但主要的氧化态是Fe3 +和Ir5 +。该化合物是低于120 K的II型反铁磁体,在每个Fe3 +阳离子的Fe占位的位置上有序磁矩为3.67(3)μB。与反位缺陷相关的自旋受挫并且不参与长距离磁排序,因此在低于40 K的磁化率中产生磁滞。简要讨论了Fe4 +阳离子的可能位置。 19个参考

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