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在“氧墙”边界捕获铁(III)-氧物种:对Fe(III)-O键本质的洞察

Trapping Iron(III)-Oxo Species at the Boundary of the "Oxo Wall": Insights into the Nature of the Fe(III)-O Bond.

作者信息

Andris Erik, Navrátil Rafael, Jašík Juraj, Puri Mayank, Costas Miquel, Que Lawrence, Roithová Jana

机构信息

Department of Organic Chemistry, Faculty of Science , Charles University , Hlavova 2030/8 , 128 43 Prague 2 , Czech Republic.

Department of Chemistry and Center for Metals in Biocatalysis , University of Minnesota , Minneapolis , Minnesota 55455 , United States.

出版信息

J Am Chem Soc. 2018 Oct 31;140(43):14391-14400. doi: 10.1021/jacs.8b08950. Epub 2018 Oct 18.

Abstract

Terminal non-heme iron(IV)-oxo compounds are among the most powerful and best studied oxidants of strong C-H bonds. In contrast to the increasing number of such complexes (>80 thus far), corresponding one-electron-reduced derivatives are much rarer and presumably less stable, and only two iron(III)-oxo complexes have been characterized to date, both of which are stabilized by hydrogen-bonding interactions. Herein we have employed gas-phase techniques to generate and identify a series of terminal iron(III)-oxo complexes, all without built-in hydrogen bonding. Some of these complexes exhibit ∼70 cm decrease in ν(Fe-O) frequencies expected for a half-order decrease in bond order upon one-electron reduction to an S = 5/2 center, while others have ν(Fe-O) frequencies essentially unchanged from those of their parent iron(IV)-oxo complexes. The latter result suggests that the added electron does not occupy a d orbital with Fe═O antibonding character, requiring an S = 3/2 spin assignment for the nascent Fe-O species. In the latter cases, water is found to hydrogen bond to the Fe-O unit, resulting in a change from quartet to sextet spin state. Reactivity studies also demonstrate the extraordinary basicity of these iron(III)-oxo complexes. Our observations show that metal-oxo species at the boundary of the "Oxo Wall" are accessible, and the data provide a lead to detect iron(III)-oxo intermediates in biological and biomimetic reactions.

摘要

末端非血红素铁(IV)-氧代化合物是最强且研究最多的强C-H键氧化剂之一。与这类配合物数量的不断增加(迄今为止已超过80种)形成对比的是,相应的单电子还原衍生物要罕见得多,且可能稳定性较差,到目前为止仅表征了两种铁(III)-氧代配合物,它们均通过氢键相互作用得以稳定。在此,我们采用气相技术生成并鉴定了一系列末端铁(III)-氧代配合物,所有这些配合物均无内在氢键。其中一些配合物在单电子还原为S = 5/2中心时,其ν(Fe-O)频率预计会因键级降低半级而降低约70 cm,而其他配合物的ν(Fe-O)频率与其母体铁(IV)-氧代配合物的频率基本不变。后一结果表明,添加的电子并未占据具有Fe═O反键特征的d轨道,这就要求新生的Fe-O物种的自旋量子数S = 3/2。在后一种情况下,发现水与Fe-O单元形成氢键,导致自旋态从四重态变为六重态。反应性研究还证明了这些铁(III)-氧代配合物具有非凡的碱性。我们的观察结果表明,“氧墙”边界处的金属-氧代物种是可以获得的,这些数据为检测生物和仿生反应中的铁(III)-氧代中间体提供了线索。

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