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一种新的八面体位置含钒的LaCo₀.₇₁(₁)V₀.₂₉(₁)O₂.₉₇(₃)钙钛矿:合成、结构与磁性表征

A new LaCo0.71(1)V0.29(1)O2.97(3) perovskite containing vanadium in octahedral sites: synthesis and structural and magnetic characterization.

作者信息

Fuertes V C, Blanco M C, Franco D G, Ceppi S, Sánchez R D, Fernández-Díaz M T, Tirao G, Carbonio R E

机构信息

INFIQC-CONICET, Dpto. de Fisicoquímica, Fac. de Ciencias Químicas, U.N.C., Córdoba 5000, Argentina.

出版信息

Dalton Trans. 2015 Jun 21;44(23):10721-7. doi: 10.1039/c4dt03858d. Epub 2015 Feb 13.

DOI:10.1039/c4dt03858d
PMID:25679183
Abstract

In the course of an investigation to prepare the hypothetic new double perovskite La(3)Co(2)VO(9) with Co(2+) and V(5+) in octahedral sites, we obtained the new simple perovskite LaCo(0.71(1))V(0.29(1))O(2.97(3)) as the main phase. The pure compound was then synthesized by the citrate decomposition method. The crystal structure was studied by X-ray (PXRD) and powder neutron diffraction (PND). Physical properties were characterized by X-ray absorption spectroscopy (XAS), X-ray emission spectroscopy (XES) and thermogravimetric analysis (TGA). Rietveld refinements were performed in the orthorhombic space group Pnma (#62). Refined cell parameters were a = 5.4762(2) Å, b = 7.7609(2) Å and c = 5.5122(1) Å. Magnetization measurements showed that this perovskite is an antiferromagnet with a Neel temperature of 15 K. At high T the magnetization follows the Curie-Weiss law corrected by temperature independent paramagnetism (TIP) showing an effective magnetic moment of 3.03μ(B) well described by the contribution of Co(2+) (HS), Co(3+) (IS), V(3+) and V(4+) ions. The crystallographic formula was refined by PND and oxidation state distribution was determined by the combination of PND, XAS, TGA and magnetic measurements.

摘要

在一项旨在制备假设的新型双钙钛矿La(3)Co(2)VO(9)(其中Co(2+)和V(5+)位于八面体位置)的研究过程中,我们得到了新型简单钙钛矿LaCo(0.71(1))V(0.29(1))O(2.97(3))作为主要相。然后通过柠檬酸盐分解法合成了纯化合物。通过X射线(PXRD)和粉末中子衍射(PND)研究了晶体结构。通过X射线吸收光谱(XAS)、X射线发射光谱(XES)和热重分析(TGA)对物理性质进行了表征。在正交空间群Pnma(#62)中进行了Rietveld精修。精修后的晶胞参数为a = 5.4762(2) Å,b = 7.7609(2) Å,c = 5.5122(1) Å。磁化测量表明,这种钙钛矿是一种反铁磁体,奈尔温度为15 K。在高温下,磁化遵循由与温度无关的顺磁性(TIP)校正的居里-外斯定律,显示出3.03μ(B)的有效磁矩,这可以很好地由Co(2+)(高自旋)、Co(3+)(低自旋)、V(3+)和V(4+)离子的贡献来描述。通过PND精修了晶体学公式,并通过PND、XAS、TGA和磁性测量的组合确定了氧化态分布。

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