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亚硒酸锰(Mn(SeO3).2H2O)和亚硒酸铁(Fe2(SeO3)3.3H2O)的合成、热学、光谱学及磁性研究

Synthesis, thermal, spectroscopic and magnetic studies of the Mn(SeO3).2H2O and Fe2(SeO3)3.3H2O selenites.

作者信息

Larrañaga Aitor, Mesa José L, Pizarro José L, Lezama Luis, Arriortua María I, Rojo Teófilo

机构信息

Departamento de Mineralogía y Petrología, Facultad de Ciencia y Tecnología, Apdo. 644, 48080 Bilbao, Spain.

出版信息

Spectrochim Acta A Mol Biomol Spectrosc. 2008 Mar;69(3):1020-6. doi: 10.1016/j.saa.2007.06.019. Epub 2007 Jun 23.

Abstract

Mn(SeO(3)).2H(2)O (1) and Fe(2)(SeO(3))(3).3H(2)O (2) have been synthesized by slow evaporation from an aqueous solution in the case of (1) and using mild hydrothermal conditions for (2). The crystal structures of both phases have been refined by the Rietveld method. The compounds crystallize in different spatial groups, the P2(1)/n monoclinic one with parameters a=6.649(1)A, b=6.542(1)A, c=10.890(1)A and beta=103.85(1) degrees being Z=4 for (1) and the R3c trigonal space group with parameters a=9.361(1)A, c=20.276(1)A and Z=6 for (2). The crystal structure of compound (1) consists of a three-dimensional framework formed by MnO(6) octahedra and (SeO(3))(2-) oxoanions with trigonal pyramidal geometry, which gives rise to Mn(2)O(10) dimers of edge-sharing octahedra. The crystal structure of phase (2) can be described as a three-dimensional framework formed by MnO(6) octahedra and (SeO(3))(2-) oxoanions with trigonal pyramidal geometry. In this phase the octahedral entities are linked along the three crystallographic axes through the selenite anions. Diffuse reflectance spectrum and luminescent measurements for (1) indicate the existence of Mn(2+) cations in a slightly distorted octahedral environment. Diffuse reflectance spectrum and Mössbauer spectroscopy, in the paramagnetic region, for (2) show the existence of Fe(3+) cations in slightly distorted octahedral symmetry. ESR spectra of both compounds are isotropic with a g-value of 1.99(1) and 2.00(1), respectively. Magnetic measurements of both phases indicate an antiferromagnetic behavior. For phase (2), both, the ESR and magnetic measurements suggest a spin change from Fe(3+) (S=5/2) to Fe(2+) (S=2) at low temperatures.

摘要

通过水溶液缓慢蒸发的方法合成了 Mn(SeO₃)·2H₂O (1),并采用温和水热条件合成了 Fe₂(SeO₃)₃·3H₂O (2)。两种相的晶体结构均采用 Rietveld 方法进行了精修。化合物结晶于不同的空间群,(1) 为 P2₁/n 单斜晶系,参数 a = 6.649(1)Å,b = 6.542(1)Å,c = 10.890(1)Å,β = 103.85(1)°,Z = 4;(2) 为 R3c 三方空间群,参数 a = 9.361(1)Å,c = 20.276(1)Å,Z = 6。化合物 (1) 的晶体结构由 MnO₆ 八面体和具有三角锥几何形状的 (SeO₃)²⁻ 含氧阴离子形成的三维骨架组成,由此产生了共边八面体的 Mn₂O₁₀ 二聚体。相 (2) 的晶体结构可描述为由 MnO₆ 八面体和具有三角锥几何形状的 (SeO₃)²⁻ 含氧阴离子形成的三维骨架。在该相中,八面体实体通过亚硒酸根阴离子沿三个晶轴相连。(化合物 1) 的漫反射光谱和发光测量表明,Mn²⁺ 阳离子存在于轻微畸变的八面体环境中。在顺磁区域,(化合物 2) 的漫反射光谱和穆斯堡尔谱表明,Fe³⁺ 阳离子存在于轻微畸变的八面体对称性中。两种化合物的电子顺磁共振谱均为各向同性,g 值分别为 1.99(1) 和 2.00(1)。两种相的磁性测量均表明存在反铁磁行为。对于相 (2),电子顺磁共振和磁性测量均表明,在低温下自旋从 Fe³⁺ (S = 5/2) 转变为 Fe²⁺ (S = 2)。

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