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含二甲胂酸配体的铁(III)-氧簇化学:结构、磁性及计算研究

Iron(III)-Oxo Cluster Chemistry with Dimethylarsinate Ligands: Structures, Magnetic Properties, and Computational Studies.

作者信息

Lee Kenneth Hong Kit, Peralta Juan E, Abboud Khalil A, Christou George

机构信息

Department of Chemistry, University of Florida, Gainesville, Florida 32611-7200, United States.

Department of Physics and Science of Advanced Materials, Central Michigan University, Mount Pleasant, Michigan 48859, United States.

出版信息

Inorg Chem. 2020 Dec 21;59(24):18090-18101. doi: 10.1021/acs.inorgchem.0c02554. Epub 2020 Dec 8.

Abstract

A program has been initiated to develop Fe/oxo cluster chemistry with the "pseudocarboxylate" ligand dimethylarsinate (MeAsO) for comparison with the well investigated Fe/oxo/carboxylate cluster area. The synthesis and characterization of three polynuclear Fe complexes are reported, [FeO(OCBu)(OAsMe)(HO)]Cl (), NaFeNaO(OAsMe)(NO)(MeAsOH)(HO) (), and Fe(OAsMe)(MeAsOH)(hqn) (), where hqnH is 8-hydroxyquinoline. The Fe core of is a type never previously encountered in Fe carboxylate chemistry, consisting of two Fe units each of which comprises two {Fe(μ-O)} units bridged by three MeAsO groups and linked into an Fe loop structure by two η:η:μ MeAsO groups, a bridging mode extremely rare with carboxylates. also consists of two Fe units, differing in their ligation from those in , and this time linked together into a linear structure by a central {Na(NO)} bridging unit. is a linear Fe complex with no monatomic bridges between Fe ions, a very rare situation in Fe chemistry with any ligands and unprecedented in Fe carboxylate chemistry. The distinct differences observed in arsinate vs carboxylate ligation modes are rationalized largely based on the greater basicity of the former vs the latter. Variable-temperature dc and ac magnetic susceptibility data reveal all Fe pairwise interactions to be antiferromagnetic. For and , the different couplings were estimated by use of a magnetostructural correlation for high nuclearity Fe-oxo clusters and by density functional theory calculations using broken symmetry methods, allowing identification of their relative spin vector alignments and thus rationalization of their = 0 ground states. The values were then used as input values to give excellent fits of the experimental χ vs data. For , the fits of the experimental χ vs data to the Van Vleck equation or with PHI gave a very weak = -0.8(1) cm ( = -2· convention) between adjacent Fe ions and an = / ground state. These initial Fe arsinate complexes also provide structural parameters that help validate literature assignments of arsinate binding modes to iron oxide/hydroxide minerals as part of environmental concerns of using arsenic-containing herbicides in agriculture.

摘要

已启动一个项目来开发铁/氧簇化学,使用“假羧酸盐”配体二甲基胂酸酯(MeAsO),以便与研究充分的铁/氧/羧酸盐簇领域进行比较。报道了三种多核铁配合物的合成与表征,即[FeO(OCBu)(OAsMe)(HO)]Cl()、NaFeNaO(OAsMe)(NO)(MeAsOH)(HO)()和Fe(OAsMe)(MeAsOH)(hqn)(),其中hqnH为8 - 羟基喹啉。的铁核是铁羧酸盐化学中从未见过的类型,由两个铁单元组成,每个单元包含两个由三个MeAsO基团桥连的{Fe(μ - O)}单元,并通过两个η:η:μ MeAsO基团连接成一个铁环结构,这种桥连模式在羧酸盐中极为罕见。也由两个铁单元组成,其配位与中的不同,这次通过一个中心{Na(NO)}桥连单元连接成线性结构。是一种线性铁配合物,铁离子之间没有单原子桥,这在任何配体的铁化学中都是非常罕见的情况,在铁羧酸盐化学中更是前所未有的。在胂酸酯与羧酸盐配位模式中观察到的明显差异,很大程度上基于前者相对于后者更强的碱性得到合理解释。变温直流和交流磁化率数据表明所有铁对相互作用都是反铁磁性的。对于和,通过使用高核铁 - 氧簇的磁结构相关性以及使用破缺对称性方法的密度泛函理论计算,估计了不同的耦合,从而确定了它们的相对自旋矢量排列,进而解释了它们的基态为 = 0。然后将值用作输入值,对实验χ与数据进行了很好的拟合。对于,将实验χ与数据拟合到范弗莱克方程或使用PHI时,相邻铁离子之间给出了非常弱的 = -0.8(1) cm( = -2·惯例)以及 = /基态。这些最初的铁胂酸酯配合物还提供了结构参数,有助于验证将胂酸酯结合模式分配给铁氧化物/氢氧化物矿物的文献,这是农业中使用含砷除草剂环境问题的一部分。

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