Department of Chemistry , The Johns Hopkins University , 3400 North Charles Street , Baltimore , Maryland 21218 , United States.
Department of Chemistry and Chemical Biology, Baker Laboratory , Cornell University , Ithaca , New York 14853 , United States.
J Am Chem Soc. 2019 Nov 6;141(44):17533-17547. doi: 10.1021/jacs.9b05274. Epub 2019 Oct 24.
The activation of dioxygen by Fe(MeTACN)(SSiMe) () is reported. Reaction of with O at -135 °C in 2-MeTHF generates a thiolate-ligated (peroxo)diiron complex Fe(O)(MeTACN)(SSiMe) () that was characterized by UV-vis (λ = 300, 390, 530, 723 nm), Mössbauer (δ = 0.53, |Δ| = 0.76 mm s), resonance Raman (RR) (ν(O-O) = 849 cm), and X-ray absorption (XAS) spectroscopies. Complex is distinct from the outer-sphere oxidation product (UV-vis (λ = 435, 520, 600 nm), Mössbauer (δ = 0.45, |Δ| = 3.6 mm s), and EPR ( = 5/2, = [6.38, 5.53, 1.99])), obtained by one-electron oxidation of . Cleavage of the peroxo O-O bond can be initiated either photochemically or thermally to produce a new species assigned as an Fe(O) complex, Fe(O)(MeTACN)(SSiMe) (), which was identified by UV-vis (λ = 385, 460, 890 nm), Mössbauer (δ = 0.21, |Δ| = 1.57 mm s), RR (ν(Fe═O) = 735 cm), and X-ray absorption spectroscopies, as well as reactivity patterns. Reaction of at low temperature with H atom donors gives a new species, Fe(OH)(MeTACN)(SSiMe) (). Complex was independently synthesized from by the stoichiometric addition of a one-electron oxidant and a hydroxide source. This work provides a rare example of dioxygen activation at a mononuclear nonheme iron(II) complex that produces both Fe-O-O-Fe and Fe(O) species in the same reaction with O. It also demonstrates the feasibility of forming Fe/O intermediates with strongly donating sulfur ligands while avoiding immediate sulfur oxidation.
报道了 Fe(MeTACN)(SSiMe)()对二氧化二氧的活化。在 -135°C 下,将 与 O 在 2-MeTHF 中反应,生成一个硫代配体(过氧)双核铁配合物 Fe(O)(MeTACN)(SSiMe)(),通过紫外可见光谱 (λ = 300, 390, 530, 723nm)、穆斯堡尔谱 (δ = 0.53, |Δ| = 0.76mm s)、共振拉曼光谱 (RR) (ν(O-O) = 849cm) 和 X 射线吸收光谱 (XAS) 进行了表征。配合物 与通过 单电子氧化得到的外球氧化产物 不同 (紫外可见光谱 (λ = 435, 520, 600nm)、穆斯堡尔谱 (δ = 0.45, |Δ| = 3.6mm s) 和 EPR ( = 5/2, = [6.38, 5.53, 1.99]))。过氧 O-O 键的断裂可以通过光化学或热化学引发,生成一种被指定为 Fe(O) 配合物的新物种 Fe(O)(MeTACN)(SSiMe)(),通过紫外可见光谱 (λ = 385, 460, 890nm)、穆斯堡尔谱 (δ = 0.21, |Δ| = 1.57mm s)、RR (ν(Fe═O) = 735cm) 和 X 射线吸收光谱以及反应模式来鉴定。在低温下, 与 H 原子供体反应生成一种新的物种 Fe(OH)(MeTACN)(SSiMe)()。配合物 可以通过计量加入单电子氧化剂和氢氧根源,从 独立合成。这项工作提供了一个单核非血红素铁(II)配合物活化二氧化二氧的罕见例子,该反应在同一反应中产生了 Fe-O-O-Fe 和 Fe(O) 物种。它还证明了在避免硫立即氧化的情况下,与强供电子硫配体形成 Fe/O 中间体是可行的。