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首页> 外文期刊>Angewandte Chemie >Low-Spin Pseudotetrahedral Iron(I) Sites in Fe2(μ-S) Complexes
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Low-Spin Pseudotetrahedral Iron(I) Sites in Fe2(μ-S) Complexes

机译:Fe2(μ-S)配合物中的低自旋伪四面体铁(I)位点

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摘要

Fe~I centers in iron-sulfide complexes have little precedent in synthetic chemistry despite a growing interest in the possible role of unusually low valent iron in metallo-enzymes that feature iron-sulfur clusters. A series of three diiron [(L3Fe)2(μ-S)] complexes that were isolated and characterized in the low-valent oxidation states Fe~(II)—S—Fe~(II), Fe~(II)S— Fe~I, and Fe~IS—Fe~I is described. This family of iron sulfides constitutes a unique redox series comprising three nearly isostructural but electronically distinct Fe2(μ-S) species. Combined structural, magnetic, and spectroscopic studies provided strong evidence that the pseudotetrahedral iron centers undergo a transition to low-spin S = 1/2 states upon reduction from Fe~(II) to Fe~I. The possibility of accessing low-spin, pseudotetrahedral Fe~I sites compatible with S~(2-) as a ligand was previously unknown.
机译:尽管人们越来越关注异常低价铁在以铁硫簇为特征的金属酶中的可能作用,但在硫化铁络合物中的Fe〜I中心在合成化学中几乎没有先例。分离并表征了低价氧化态Fe〜(II)-S-Fe〜(II),Fe〜(II)S-的一系列三个二铁[(L3Fe)2(μ-S)]配合物描述了Fe〜I和Fe〜IS-Fe〜I。硫化铁族构成一个独特的氧化还原系列,包括三个几乎同构但电子上不同的Fe2(μ-S)物种。组合的结构,磁性和光谱学研究提供了有力的证据,表明伪四面体铁心在从Fe〜(II)还原为Fe〜I时会经历低自旋S = 1/2态的转变。以前尚不了解与S〜(2-)相容的低旋转伪四面体Fe〜I位点的可能性。

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