The Fe2 (NO)2 Diamond Core: A Unique Structural Motif In Non-Heme Iron-NO Chemistry.
The Fe2 (NO)2 Diamond Core: A Unique Structural Motif In Non-Heme Iron-NO Chemistry.
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Fe2 (NO)2 金刚石核心:非血红素铁-NO 化学中的独特结构基序。
DOI:
10.1002/anie.201911968
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发表时间:
2019
期刊:
影响因子:
--
通讯作者:
Lehnert,Nicolai
中科院分区:
文献类型:
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作者:
Dong,HaiT;Speelman,AmyL;Kozemchak,ClaireE;Sil,Debangsu;Krebs,Carsten;Lehnert,Nicolai
Non‐heme high‐spin (hs) {FeNO}8complexes have been proposed as important intermediates towards N2O formation in flavodiiron NO reductases (FNORs). Many hs‐{FeNO}8complexes disproportionate by forming dinitrosyl iron complexes (DNICs), but the mechanism of this reaction is not understood. While investigating this process, we isolated a new type of non‐heme iron nitrosyl complex that is stabilized by an unexpected spin‐state change. Upon reduction of the hs‐{FeNO}7complex, [Fe(TPA)(NO)(OTf)](OTf) (1), the N‐O stretching band vanishes, but no sign of DNIC or N2O formation is observed. Instead, the dimer, [Fe2(TPA)2(NO)2](OTf)2(2) could be isolated and structurally characterized. We propose that2is formed from dimerization of the hs‐{FeNO}8intermediate, followed by a spin state change of the iron centers to low‐spin (ls), and speculate that2models intermediates in hs‐{FeNO}8complexes that precede the disproportionation reaction.