Abstract
The reduction of nitrite (NO(2)(-)) to nitric oxide (NO(•)) is a fundamental transformation within both the global nitrogen cycle and enzymatic signaling pathways. Although extensively investigated, the elusive {FeNO}(6) intermediate implicated in the 2H(+)/1e(-) reduction pathway has rarely been observed or isolated due to the inherent instability. Here, we present a comprehensive mechanistic investigation of nitrite reduction by a mononuclear iron(II)-nitrite complex, [Fe(II)(TBDAP)(NO(2))(CH(3)CN)](+) (1) (TBDAP = N,N'-di-tert-butyl-2,11-diaza[3.3](2,6)-pyridinophane). Treatment of 1 with 2.5 equiv of triflic acid (HOTf) affords the {FeNO}(6) (2) intermediate, which was characterized using a combination of various physicochemical techniques and DFT calculations. Isotopic labeling using Na(15)NO(2) confirmed the formation of 2 via heterolytic N-O bond cleavage. Kinetic studies revealed a HOTf-independent rate constant and a markedly negative value of activation entropy for the formation of 2, suggesting that the rate-determining step involves an associative reaction between Fe(II) and NO(+). Electrochemical analysis showed a reversible redox couple for 2, and subsequent one-electron reduction by ferrocene released NO(•). The generation of NO(•) was confirmed through trapping experiments using [Co(TPP)], resulting in the formation of [Co(TPP)(NO)]. The experimental findings establish {FeNO}(6) as an isolable and reactive intermediate, offering new insight into the mechanistic landscape of nitrite reduction.