Sakai Takanori, Ohgo Yoshiki, Hoshino Akito, Ikeue Takahisa, Saitoh Takashi, Takahashi Masashi, Nakamura Mikio
Department of Chemistry, School of Medicine, Toho University, Tokyo 143-8540, Japan.
Inorg Chem. 2004 Aug 9;43(16):5034-43. doi: 10.1021/ic049825q.
The spin states of the iron(III) complexes with a highly ruffled porphyrin ring, [Fe(TEtPrP)X] where X = F-, Cl-, Br-, I-, and ClO4(-), have been examined by 1H NMR, 13C NMR, EPR, and Mössbauer spectroscopy. While the F-, Cl-, and Br- complexes adopt a high-spin (S = 5/2) state, the I- complex exhibits an admixed intermediate-spin (S = 5/2, 3/2) state in CD2Cl2 solution. The I- complex shows, however, a quite pure high-spin state in toluene solution as well as in the solid. The results contrast those of highly saddled [Fe(OETPP)X] where the I- complex exhibits an essentially pure intermediate-spin state both in solution and in the solid. In contrast to the halide-ligated complexes, the ClO4(-) complex shows a quite pure intermediate-spin state. The 13C NMR spectra of [Fe(TEtPrP)ClO4] are characterized by the downfield and upfield shifts of the meso and pyrrole-alpha carbon signals, respectively: delta(meso) = +342 and delta(alpha-py) = -287 ppm at 298 K. The data indicate that the meso carbon atoms of [Fe(TEtPrP)ClO4] have considerable amounts of positive spin, which in turn indicate that the iron has an unpaired electron in the d(xy) orbital; the unpaired electron in the d(xy) orbital is delocalized to the meso positions due to the iron(d(xy))-porphyrin(a(2u)) interaction. Similar results have been obtained in analogous [Fe(TiPrP)X] though the intermediate-spin character of [Fe(TiPrP)X] is much larger than that of the corresponding [Fe(TEtPrP)X]. On the basis of these results, we have concluded that the highly ruffled intermediate-spin complexes such as [Fe(TEtPrP)ClO4] and [Fe(TiPrP)ClO4] adopt a novel (d(xz), d(yz))3(d(xy))1(d(z)(2)1 electron configuration; the electron configuration of the intermediate-spin complexes reported previously is believed to be (d(xy))2(d(xz)), d(yz))2(d(z)(2))1.
通过1H NMR、13C NMR、EPR和穆斯堡尔光谱研究了具有高度褶皱卟啉环的铁(III)配合物[Fe(TEtPrP)X](其中X = F-、Cl-、Br-、I-和ClO4(-))的自旋态。虽然F-、Cl-和Br-配合物呈现高自旋(S = 5/2)态,但I-配合物在CD2Cl2溶液中表现出混合的中间自旋(S = 5/2,3/2)态。然而,I-配合物在甲苯溶液以及固体中显示出相当纯的高自旋态。这些结果与高度鞍形的[Fe(OETPP)X]相反,在[Fe(OETPP)X]中,I-配合物在溶液和固体中均呈现基本纯的中间自旋态。与卤化物配位的配合物不同,ClO4(-)配合物显示出相当纯的中间自旋态。[Fe(TEtPrP)ClO4]的13C NMR光谱的特征在于,在298 K时,中位碳信号和吡咯-α碳信号分别向低场和高场位移:δ(中位)= +342,δ(α-吡咯)= -287 ppm。数据表明,[Fe(TEtPrP)ClO4]的中位碳原子具有相当数量的正自旋,这反过来表明铁在d(xy)轨道上有一个未成对电子;由于铁(d(xy))-卟啉(a2u)相互作用,d(xy)轨道上的未成对电子离域到中位位置。在类似的[Fe(TiPrP)X]中也获得了类似的结果,尽管[Fe(TiPrP)X]的中间自旋特征比相应的[Fe(TEtPrP)X]大得多。基于这些结果,我们得出结论,高度褶皱的中间自旋配合物,如[Fe(TEtPrP)ClO4]和[Fe(TiPrP)ClO4],采用一种新颖的(d(xz), d(yz))3(d(xy))1(d(z)(2)1电子构型;先前报道的中间自旋配合物的电子构型被认为是(d(xy))2(d(xz)), d(yz))2(d(z)(2))1。