School of Chemical Sciences, University of Illinois at Urbana-Champaign, 600 S. Mathews Avenue, Urbana, Illinois 61801, United States.
School of Chemistry, CRANN and AMBER Research Centres, Trinity College Dublin, College Green, Dublin 2, Ireland.
Inorg Chem. 2022 May 30;61(21):8182-8192. doi: 10.1021/acs.inorgchem.2c00462. Epub 2022 May 17.
The reduction of nitrite (NO) to generate nitric oxide (NO) is a significant area of research due to their roles in the global nitrogen cycle. Here, we describe various modifications of the tris(5-cyclohexyliminopyrrol-2-ylmethyl)amine H[N(pi)] ligand where the steric bulk and acidity of the secondary coordination sphere were explored in the non-heme iron system for nitrite reduction. The cyclohexyl and 2,4,6-trimethylphenyl variants of the ligand were used to probe the mechanism of nitrite reduction. While previously stoichiometric addition of nitrite to the iron(II)-species generated an iron(III)-oxo complex, changing the secondary coordination sphere to mesityl resulted in an iron(III)-hydroxo complex. Subsequent addition of an electron and two protons led to the release of water and regeneration of the starting iron(II) catalyst. This sequence mirrored the proposed mechanism of nitrite reduction in biological systems, where the distal histidine residue shuttles protons to the active site. Computational studies aimed at interrogating the dissimilar behavior of the cyclohexyl and mesityl ligand systems resulting in Fe(III)-oxo and Fe(III)-hydroxo complexes, respectively, shed light on the key role of H-bonds involving the secondary coordination sphere in the relative stability of these species.
由于其在全球氮循环中的作用,亚硝酸盐(NO)还原生成一氧化氮(NO)是一个重要的研究领域。在这里,我们描述了三(5-环己基异吲哚啉-2-基甲基)胺 H[N(pi)]配体的各种修饰,其中在非血红素铁体系中探索了第二配位球的空间位阻和酸度,以用于亚硝酸盐还原。环己基和 2,4,6-三甲基苯基配体变体被用于探测亚硝酸盐还原的机制。虽然之前亚硝酸盐与铁(II)物种的化学计量添加生成了铁(III)-氧配合物,但将第二配位球改变为间三甲苯基导致了铁(III)-羟配合物的形成。随后加入一个电子和两个质子导致水的释放和起始铁(II)催化剂的再生。这一序列反映了生物体系中亚硝酸盐还原的提议机制,其中远端组氨酸残基将质子穿梭到活性位点。旨在探讨环己基和间三甲苯基配体系统导致分别形成 Fe(III)-氧和 Fe(III)-羟配合物的不同行为的计算研究,阐明了涉及第二配位球的氢键在这些物种的相对稳定性中的关键作用。