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Synthesis and characterization of the reduced single-layer manganite Sr2MnO3.5+x

机译:还原型单层锰矿Sr2MnO3.5 + x的合成与表征

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The nuclear and magnetic structures of polycrystalline Sr2MnO3.5 have been determined by the Rietveld analysis of neutron powder diffraction data and electron diffraction techniques. The pure Mn3+ single-layered phase crystallizes in the primitive monoclinic space-group Y2(1)/c with lattice constants a = 6.8524(3) Angstrom; b = 10.8131(4) Angstrom; c = 10.8068(4) Angstrom; beta = 113.247(4)degrees. The oxygen defects form an ordered superstructure within the perovskite block layers consisting of interconnected MnO5 square pyramids, slightly different from those observed for the defect perovskites SrMDO2.5 and Ca2MHO3.5. Magnetic susceptibility studies show a broad transition at similar to280K, which is attributed to an overall antiferromagnetic ordering of spins, which leads to doubling of the unit cell along [100]. The magnetic unit cell comprises ferromagnetic clusters of four corner-sharing MnO5 pyramids, which are antiferromagnetically aligned to other similar clusters within the perovskite block layers. (C) 2002 Elsevier Science (USA). [References: 20]
机译:通过中子粉末衍射数据的Rietveld分析和电子衍射技术确定了多晶Sr2MnO3.5的核和磁结构。纯Mn3 +单层相在原始单斜空间群Y2(1)/ c中结晶,晶格常数为a = 6.8524(3)埃; b = 10.8131(4)埃; c = 10.8068(4)埃; beta = 113.247(4)度。氧缺陷在由相互连接的MnO5四棱锥组成的钙钛矿块层中形成有序的上部结构,与钙钛矿SrMDO2.5和Ca2MHO3.5缺陷所观察到的略有不同。磁化率研究表明,在类似于280K的范围内发生了宽泛的转变,这归因于自旋的整体反铁磁有序性,这导致单位晶胞沿[100]加倍。磁性单位单元包括四个角共享MnO5金字塔的铁磁簇,它们与钙钛矿块层中的其他类似簇反铁磁对齐。 (C)2002 Elsevier Science(美国)。 [参考:20]

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