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Iron L-edge X-ray Absorption Spectroscopy of Oxy-Picket Fence Porphyrin: Experimental Insight into Fe-O2 Bonding

机译:氧凝固围栏卟啉的铁L边缘X射线吸收光谱:对Fe-O2键合的实验洞察

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摘要

The electronic structure of the Fe–O2 center in oxy-hemoglobin and oxy-myoglobin is a long-standing issue in the field of bioinorganic chemistry. Spectroscopic studies have been complicated by the highly delocalized nature of the porphyrin and calculations require interpretation of multi-determinant wavefunctions for a highly covalent metal site. Here, iron L-edge X-ray absorption spectroscopy (XAS), interpreted using a valence bond configuration interaction (VBCI) multiplet model, is applied to directly probe the electronic structure of the iron in the biomimetic Fe–O2 heme complex [Fe(pfp)(1-MeIm)O2] (pfp = meso-tetra(α,α,α,α-o-pivalamidophenyl) porphyrin or TpivPP). This method allows separate estimates of σ-donor, π-donor, and π-acceptor interactions through ligand to metal charge transfer (LMCT) and metal to ligand charge transfer (MLCT) mixing pathways. The L-edge spectrum of [Fe(pfp)(1-MeIm)O2] is further compared to those of [FeII(pfp)(1-MeIm)2], [FeII(pfp)], and [FeIII(tpp)(ImH)2]Cl (tpp = meso-tetraphenylporphyrin) which have FeII S = 0, FeII S = 1 and FeIII S = 1/2 ground states, respectively. These serve as references for the three possible contributions to the ground state of oxy-pfp. The Fe–O2 pfp site is experimentally determined to have both significant σ-donation and a strong π-interaction of the O2 with the iron, with the latter having implications with respect to the spin polarization of the ground state.
机译:氧合血红蛋白和氧合肌红蛋白中Fe–O2中心的电子结构是生物无机化学领域的一个长期存在的问题。卟啉的高度离域性质使光谱学研究变得复杂,计算需要解释高度共价金属位点的多决定波函数。在这里,铁L边缘X射线吸收光谱(XAS),使用价键构型相互作用(VBCI)多重峰模型解释,被用于直接探测仿生Fe–O2血红素络合物[Fe( pfp)(1-MeIm)O2](pfp =中四(α,α,α,α-o-新戊酰胺基苯基)卟啉或TpivPP)。该方法允许通过配体到金属的电荷转移(LMCT)和金属到配体的电荷转移(MLCT)混合途径分别估计σ供体,π供体和π受体的相互作用。进一步比较了[Fe(pfp)(1-MeIm)O2]的L-edge光谱与[Fe II (pfp)(1-MeIm)2],[Fe II (pfp)]和具有Fe II S =的[Fe III (tpp)(ImH)2] Cl(tpp =中四苯基卟啉) 0,Fe II S = 1,Fe III S = 1/2基态。这些作为对oxy-pfp基态的三种可能贡献的参考。通过实验确定,Fe–O2 pfp位置具有显着的σ贡献和O2与铁的强π相互作用,而后者与基态的自旋极化有关。

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