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基于二茂铁/二茂铁阳离子对和 Keggin 型多金属氧酸盐的电荷转移盐。

A Charge-Transfer Salt Based on Ferrocene/Ferrocenium Pairs and Keggin-Type Polyoxometalates.

机构信息

Departamento de Química Inorgánica, Facultad de Ciencia y Tecnología, Universidad del País Vasco UPV/EHU, P.O. Box 644, 48080 Bilbao, Spain.

Centro de Física de Materiales CFM (CSIC⁻UPV/EHU), Paseo Manuel Lardizabal 5, 20018 Donostia-San Sebastián, Spain.

出版信息

Molecules. 2018 Nov 30;23(12):3150. doi: 10.3390/molecules23123150.

Abstract

A new hybrid inorganic-organometallic salt has been obtained from the reaction of the Keggin-type silicotungstate anion with ferrocene in a water/methanol mixture as a result of the partial oxidation of ferrocene molecules to ferrocenium cations. Single-crystal X-ray diffraction analysis reveals the presence of four ferrocenium (Fe) cations and one ferrocene (Fe) molecule per plenary Keggin anion in the crystal structure of [Fe (Cp)₂]₄[SiWO]·[Fe(Cp)₂]·2CH₃OH (). Compound thus constitutes the first example in the literature in which ferrocenium and ferrocene species coexist in the structure of a polyoxometalate-based salt. The two crystallographically independent ferrocenium species in the asymmetric unit of exhibit different configurations: One displays an eclipsed conformation with ideal symmetry, whereas the conformation in the other one is staggered . The crystal packing of can be best described as an organometallic sub-lattice of ferrocenium and ferrocene species linked by a network of π-π interactions that generates rectangular cavities of about 14 × 10 Å in which strings of Keggin anions and methanol molecules are hosted, further connected to each other via weak O···C-O···O type hydrogen bonds. The charge-transfer nature of the salt has been studied by solid-state diffuse reflectance UV-Vis spectroscopy and the presence of magnetically isolated Fe/Fe centres has been confirmed by Mössbauer spectroscopy. A topological study carried out on all of the pristine ferrocenyl species deposited in the Cambridge Structural Database (CSD) has allowed two main conclusions to be drawn: (1) these species tend to adopt extreme conformations (either eclipsed or staggered) with less than a 15% of examples showing intermediate states and (2) the oxidation state of the iron centres can be unequivocally assigned on the basis of a close inspection of the Fe···Cp distances, which allows ferrocene neutral molecules and ferrocenium cations to be easily distinguished.

摘要

一种新的杂化无机-有机金属盐已经通过 Keggin 型硅钨酸盐阴离子与二茂铁在水/甲醇混合物中的反应得到,这是由于二茂铁分子的部分氧化为二茂铁阳离子。单晶 X 射线衍射分析表明,在[Fe(Cp)_2]4[SiWO]·[Fe(Cp)_2]·2CH_3OH()的晶体结构中,每个完整的 Keggin 阴离子中存在四个二茂铁(Fe)阳离子和一个二茂铁(Fe)分子。因此,化合物构成了文献中第一个同时存在二茂铁阳离子和二茂铁分子的多金属氧酸盐基盐的结构的例子。在[Fe(Cp)_2]4[SiWO]·[Fe(Cp)_2]·2CH_3OH()的不对称单元中,两个结晶学上独立的二茂铁阳离子表现出不同的构型:一个呈现出理想的 C_2 对称的重叠构象,而另一个则是交错构象。[Fe(Cp)_2]4[SiWO]·[Fe(Cp)_2]·2CH_3OH()的晶体堆积可以最好地描述为通过π-π相互作用形成的二茂铁和二茂铁分子的有机金属亚晶格,这些相互作用生成约 14×10 Å的矩形空腔,其中容纳了 Keggin 阴离子和甲醇分子的链,通过弱 O···C-O···O 型氢键进一步相互连接。通过固态漫反射紫外可见光谱研究了盐的电荷转移性质,并通过 Mössbauer 光谱证实了存在磁性隔离的 Fe/Fe 中心。对剑桥结构数据库(CSD)中所有原始二茂铁基物种的拓扑研究得出了两个主要结论:(1)这些物种倾向于采取极端构象(要么重叠,要么交错),不到 15%的例子显示中间状态;(2)铁中心的氧化态可以根据 Fe···Cp 距离的仔细检查来明确确定,这允许容易地区分二茂铁中性分子和二茂铁阳离子。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8d24/6321299/9faf9b499b27/molecules-23-03150-g001.jpg

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