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Ba3Fe2WO9-delta: Effect of oxygen non-stoichiometry on structural and magnetic properties

机译:Ba3Fe2WO9-δ:氧非化学计量对结构和磁性的影响

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The magnetic and structural properties of oxygen-deficient perovskites with composition Ba3Fe2WO9-6 (BFWO) have been systematically studied for two different oxygen contents corresponding to delta = 0.00 and 0.55 in the chemical formula in order, to determine and correlate their chemical composition, structural and magnetic properties. The evolution of nuclear and magnetic structures with temperature has been investigated by neutron powder diffraction. It was shown that at room temperature the stoichiometric compound (delta = 0.00) adopts a hexagonal 6H-perovskite structure (space group P6(3)/mmc). This phase, when heated at high temperature under a stream of Ar gas, transforms to an oxygen-deficient phase delta = 0.55), which is an ordered cubic perovskite structure (space group Fm-3m). The crystallographic and magnetic properties of the obtained phases are compared, and it is clear that the magnetic properties are significantly affected by oxygen non-stoichiometry. These changes of magnetic properties for such a slight decrease in oxygen content are interpreted as a result of structural transformations. Together with the experimental results based on neutron powder diffraction data a discussion of some aspects of the structural transformation (P6(3)/mmc -> Fm-3m) is presented. (c) 2006 Published by Elsevier Inc.
机译:已经系统地研究了化学组成为Ba3Fe2WO9-6(BFWO)的缺氧钙钛矿的磁性和结构性质,该化学性质对应于化学式中的delta = 0.00和0.55的两种不同的氧含量,以确定并关联它们的化学组成,结构和磁性。通过中子粉末衍射研究了核和磁结构随温度的演变。结果表明,在室温下,化学计量化合物(δ= 0.00)采用六方六方钙钛矿结构(空间群P6(3)/ mmc)。当在Ar气流下在高温下加热时,该相转变为缺氧相delta = 0.55),这是有序立方钙钛矿结构(空间群Fm-3m)。比较了所得相的晶体学和磁性,并且很明显,氧的非化学计量显着影响了磁性。氧含量如此轻微降低的磁性变化是结构转变的结果。结合基于中子粉末衍射数据的实验结果,对结构转变的某些方面进行了讨论(P6(3)/ mmc-> Fm-3m)。 (c)2006年由Elsevier Inc.发布。

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