Rath Sankar Prasad, Olmstead Marilyn M, Balch Alan L
Department of Chemistry, University of California-Davis, Davis, CA 95616, USA.
Inorg Chem. 2006 Jul 24;45(15):6083-93. doi: 10.1021/ic0607033.
The apportionment of electrons between iron and the porphyrinic macrocycle in complexes of octaethyloxophlorin (H3OEPO) has been a vexing problem. In particular, for (Py)2Fe(OEPO), which is an important intermediate in heme degradation, three resonance structures involving Fe(III), Fe(II), or Fe(I), respectively, have been considered. To clarify this matter, the electronic and geometric structures of (Py)2Fe(III)(OEPO), (Im)2Fe(III)(OEPO).2THF, and (Im)2Fe(III)(OEPO).1.6CHCl3 have been examined by single-crystal X-ray diffraction, measurement of magnetic moments as a function of temperature, and EPR and NMR spectral studies. The results clearly show that both complexes exist in the Fe(III)/oxophlorin trianion form rather than the Fe(II)/oxophlorin radical form previously established for (2,6-xylylNC)(2)Fe(II)(OEPO.). In the solid state from 10 to 300 K, (Py)2Fe(III)(OEPO) exists in the high-spin (S = 5/2) state with the axial ligands in parallel planes, a planar porphyrin, and long axial Fe-N distances. However, in solution it exists predominantly in a low-spin (S = 1/2) form. In contrast, the structures of (Im)2Fe(III)(OEPO).2THF and (Im)2Fe(III)(OEPO).1.6CHCl3 consist of porphyrins with a severe ruffled distortion, axial ligands in nearly perpendicular planes, and relatively short axial Fe-N distances. The crystallographic, magnetic, EPR, and NMR results all indicate that (Im)2Fe(III)(OEPO) exists in the low-spin Fe(III) form in both the solid state and in solution.
在八乙基氧代卟啉(H3OEPO)配合物中,铁与卟啉大环之间电子的分配一直是个棘手的问题。特别是对于(Py)2Fe(OEPO),它是血红素降解中的一个重要中间体,人们已经考虑了分别涉及Fe(III)、Fe(II)或Fe(I)的三种共振结构。为了阐明这个问题,通过单晶X射线衍射、测量磁矩随温度的变化以及EPR和NMR光谱研究,对(Py)2Fe(III)(OEPO)、(Im)2Fe(III)(OEPO)·2THF和(Im)2Fe(III)(OEPO)·1.6CHCl3的电子和几何结构进行了研究。结果清楚地表明,这两种配合物均以Fe(III)/氧代卟啉三阴离子形式存在,而不是先前为(2,6 - 二甲苯基异腈)(2)Fe(II)(OEPO·)所确定的Fe(II)/氧代卟啉自由基形式。在10至300 K的固态下,(Py)2Fe(III)(OEPO)以高自旋(S = 5/2)状态存在,轴向配体在平行平面内,卟啉平面,且轴向Fe - N距离较长。然而,在溶液中它主要以低自旋(S = 1/2)形式存在。相比之下,(Im)2Fe(III)(OEPO)·2THF和(Im)2Fe(III)(OEPO)·1.6CHCl3的结构由具有严重褶皱变形的卟啉、轴向配体在近乎垂直的平面内以及相对较短的轴向Fe - N距离组成。晶体学、磁性、EPR和NMR结果均表明,(Im)2Fe(III)(OEPO)在固态和溶液中均以低自旋Fe(III)形式存在。