An abiotic analogue of the diiron(IV)oxo "diamond core" of soluble methane monooxygenase generated by direct activation of O2 in aqueous Fe(II)/EDTA solutions: thermodynamics and electronic structure

被引:14
作者
Bernasconi, Leonardo [1 ,2 ]
Belanzoni, Paola [2 ,3 ]
Baerends, Evert Jan [2 ,4 ]
机构
[1] STFC Rutherford Appleton Lab, Didcot OX11 0QX, Oxon, England
[2] Pohang Univ Sci & Technol, Dept Chem, WCU Program, Pohang 790784, South Korea
[3] Univ Perugia, Dept Chem, I-06123 Perugia, Italy
[4] Vrije Univ Amsterdam, Theoret Chem Sect, NL-1081 HV Amsterdam, Netherlands
关键词
HIGH-VALENT IRON; DENSITY-FUNCTIONAL THEORY; HORSERADISH-PEROXIDASE COMPOUND; SPIN OXOIRON(IV) COMPLEX; C-H ACTIVATION; FE-IV=O; ALKANE HYDROXYLATION; DIOXYGEN ACTIVATION; SPECTROSCOPIC CHARACTERIZATION; ALIPHATIC HYDROXYLATION;
D O I
10.1039/c1cp21244c
中图分类号
O64 [物理化学(理论化学)、化学物理学];
学科分类号
070304 ; 081704 ;
摘要
We study the generation of a dinuclear Fe(IV)oxo species, [EDTAH center dot FeO center dot OFe center dot EDTAH](2-), in aqueous solution at room temperature using Density Functional Theory (DFT) and Ab Initio Molecular Dynamics (AIMD). This species has been postulated as an intermediate in the multi-step mechanism of autoxidation of Fe(II) to Fe(III) in the presence of atmospheric O-2 and EDTA ligand in water. We examine the formation of [EDTAH center dot FeO center dot OFe center dot EDTAH](2-) by direct cleavage of O-2, and the effects of solvation on the spin state and O-O cleavage barrier. We also study the reactivity of the resulting dinuclear Fe(IV) oxo system in CH4 hydroxylation, and its tendency to decompose to mononuclear Fe(IV) oxo species. The presence of the solvent is shown to play a crucial role, determining important changes in all these processes compared to the gas phase. We show that, in water solution, [EDTAH center dot FeO center dot OFe center dot EDTAH](2-) (as well as its precursor [EDTAH center dot Fe center dot O-2 center dot Fe center dot EDTAH](2-)) exists as stable species in a S = 4 ground spin state when hydrogen-bonded to a single water molecule. Its structure comprises two facing Fe(IV) oxo groups, in an arrangement similar to the one evinced for the active centre of intermediate Q of soluble Methane Monooxygenase (sMMO). The inclusion of the water molecule in the complex decreases the overall symmetry of the system, and brings about important changes in the energy and spatial distribution of orbitals of the Fe(IV) oxo groups relative to the gas phase. In particular, the virtual 3 sigma* orbital of one of the Fe(IV) oxo groups experiences much reduced repulsive orbital interactions from ligand orbitals, and its consequent stabilisation dramatically enhances the electrophilic character of the complex, compared to the symmetrical non-hydrated species, and its ability to act as an acceptor of a H atom from the CH4 substrate. The computed free energy barrier for H abstraction is 28.2 kJ mol(-1) (at the BLYP level of DFT), considerably below the gas phase value for monomeric [FeO center dot EDTAH](-), and much below the solution value for the prototype hydrated ferryl ion [FeO(H2O)(5)](2+).
引用
收藏
页码:15272 / 15282
页数:11
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