2018
DOI: 10.1002/anie.201812724
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Selective Formation of an FeIVO or an FeIIIOOH Intermediate From Iron(II) and H2O2: Controlled Heterolytic versus Homolytic Oxygen–Oxygen Bond Cleavage by the Second Coordination Sphere

Abstract: We demonstrate that the devised incorporation of an alkylamine group into the second coordination sphere of an FeII complex allows to switch its reactivity with H2O2 from the usual formation of FeIII species towards the selective generation of an FeIV‐oxo intermediate. The FeIV‐oxo species was characterized by UV/Vis absorption and Mössbauer spectroscopy. Variable‐temperature kinetic analyses point towards a mechanism in which the heterolytic cleavage of the O−O bond is triggered by a proton transfer from the … Show more

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Cited by 56 publications
(27 citation statements)
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“…mCPBA to the very same complex solution at −20 °C, a set of two new quadrupole doublets appears with a distribution of 37 % and 63 %, respectively. The minor quadrupole doublet with an isomer shift of 0.04 mm s −1 close to zero and a corresponding quadrupole splitting of 0.54 mm s −1 is well in line with the formation of a high‐spin Fe(IV)oxo compound and comparable values were previously reported for tetradentate tpa Ph Fe(IV)O (δ=0.09 mm s −1 ; ΔE Q =0.51 mm s −1 ; S=2; tpa Ph : tris(5‐phenylpyrrole‐2‐ylmethyl)amine) [24] and other ferryl species [25,26] . In addition, a ferric species (δ=0.48 mm s −1 ; ΔE Q =1.91 mm s −1 ) is observed and a similar Mößbauer spectrum upon Fe(IV)oxo formation was previously reported by Nordlander and colleagues and assigned to an oxo‐bridged iron dimer impurity [27] .…”
Section: Resultssupporting
confidence: 88%
“…mCPBA to the very same complex solution at −20 °C, a set of two new quadrupole doublets appears with a distribution of 37 % and 63 %, respectively. The minor quadrupole doublet with an isomer shift of 0.04 mm s −1 close to zero and a corresponding quadrupole splitting of 0.54 mm s −1 is well in line with the formation of a high‐spin Fe(IV)oxo compound and comparable values were previously reported for tetradentate tpa Ph Fe(IV)O (δ=0.09 mm s −1 ; ΔE Q =0.51 mm s −1 ; S=2; tpa Ph : tris(5‐phenylpyrrole‐2‐ylmethyl)amine) [24] and other ferryl species [25,26] . In addition, a ferric species (δ=0.48 mm s −1 ; ΔE Q =1.91 mm s −1 ) is observed and a similar Mößbauer spectrum upon Fe(IV)oxo formation was previously reported by Nordlander and colleagues and assigned to an oxo‐bridged iron dimer impurity [27] .…”
Section: Resultssupporting
confidence: 88%
“…One of them, which accounts for almost 50 % of the sample, exhibits an isomeric shift of δ = 0.42 mm/s and a quadrupole splitting of ΔE Q = 0.53 mm/s and we assign it to an iron(III) product. It has not escaped our attention that these parameters strongly resemble those that were assigned to the iron(IV) oxo species formed upon treatment of the α-Fe sites in Fe-BEA (iron modified beta-zeolite) after treatment with N 2 O (δ = 0.41 mm/s, ΔE Q = 0.55 mm/s), [18] however, it is unlikely that a corresponding complex would be stable at room temperature, as in our case, and in addition a band between λ = 550-750 nm in the UV-vis spectrum which is characteristic for iron(IV) oxo compounds [19] cannot be found in the spectra shown in Figure 4. The two other compounds have an isomeric shift of around δ = 0.4 mm/s, too.…”
Section: Resultsmentioning
confidence: 54%
“…In the Fe−O bond homolysis, a high‐spin Fe III −OOR would produce peroxyl radical, which often leads to uncontrolled oxidation of substrates in alkylperoxide‐dependent catalytic oxidations by iron complexes . Recent reports indicated that different strategies, such as use of protic/Lewis acid or use of secondary coordination interactions, could direct the heterolytic O−O cleavage of Fe−OOR (R=H, acyl) species . Direct formation of iron(IV)‐oxo species from iron(II) precursor complexes and hydrogen peroxide have been reported without generation of iron(III)‐hydroperoxo intermediates .…”
Section: Methodsmentioning
confidence: 99%
“…Recent reports indicated that different strategies, such as use of protic/Lewis acid or use of secondary coordination interactions, could direct the heterolytic O−O cleavage of Fe−OOR (R=H, acyl) species . Direct formation of iron(IV)‐oxo species from iron(II) precursor complexes and hydrogen peroxide have been reported without generation of iron(III)‐hydroperoxo intermediates . A putative Fe II −OOR(H), generated in situ upon one‐electron reduction of the iron(III) intermediate, has been proposed to undergo heterolytic O−O bond cleavage, resulting in the formation of the corresponding iron(IV)‐oxo species .…”
Section: Methodsmentioning
confidence: 99%