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O 2 Activation by Non-Heme Thiolate-Based Dinuclear Fe Complexes
Iron centers featuring thiolates in their metal coordination sphere (as ligands or substrates) are well-known to activate dioxygen. Both heme and non-heme centers that contain iron-thiolate bonds are found in nature. Investigating the ability of iron-thiolate model complexes to activate O is expecte...
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Published in: | Inorganic chemistry 2020-03, Vol.59 (5), p.3249-3259 |
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Main Authors: | , , , , , , , , , , |
Format: | Article |
Language: | English |
Citations: | Items that this one cites Items that cite this one |
Online Access: | Get full text |
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Summary: | Iron centers featuring thiolates in their metal coordination sphere (as ligands or substrates) are well-known to activate dioxygen. Both heme and non-heme centers that contain iron-thiolate bonds are found in nature. Investigating the ability of iron-thiolate model complexes to activate O
is expected to improve the understanding of the key factors that direct reactivity to either iron or sulfur. We report here the structural and redox properties of a thiolate-based dinuclear Fe complex, [Fe
(LS)
] (LS
= 2,2'-(2,2'-bipyridine-6,6'-iyl)bis(1,1-diphenylethanethiolate)), and its reactivity with dioxygen, in comparison with its previously reported protonated counterpart, [Fe
(LS)(LSH)]
. When reaction with O
occurs in the absence of protons or in the presence of 1 equiv of proton (i.e., from [Fe
(LS)(LSH)]
), unsupported μ-oxo or μ-hydroxo Fe
dinuclear complexes ([Fe
(LS)
O] and [Fe
(LS)
(OH)]
, respectively) are generated. [Fe
(LS)
O], reported previously but isolated here for the first time from O
activation, is characterized by single crystal X-ray diffraction and Mössbauer, resonance Raman, and NMR spectroscopies. The addition of protons leads to the release of water and the generation of a mixture of two Fe-based "oxygen-free" species. Density functional theory calculations provide insight into the formation of the μ-oxo or μ-hydroxo Fe
dimers, suggesting that a dinuclear μ-peroxo Fe
intermediate is key to reactivity, and the structure of which changes as a function of protonation state. Compared to previously reported Mn-thiolate analogues, the evolution of the peroxo intermediates to the final products is different and involves a comproportionation vs a dismutation process for the Mn and Fe derivate, respectively. |
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ISSN: | 0020-1669 1520-510X |
DOI: | 10.1021/acs.inorgchem.9b03633 |