Hu et al.
equilibrium (S ) 1/2 h S ) 5/2)9,10 system and a monoclinic,
intermediate-spin system, S ) 3/2.11 In these complexes, the
two pyridines maintain a relative parallel orientation but the
absolute orientation of the two axial ligands with respect to
the porphinato core changed. Although this system showed
large changes in the electronic structure of iron(III), control-
ling axial ligand orientation more likely will affect the
relative energies of the three lowest d-orbitals of iron, namely
the dxy, dxz, and dyz orbitals.
identical axial ligands that have different structure and/or
physical properties have been studied.18,24,25 Both [Fe(TPP)-
(HIm)2]+ and [Fe(TMP)(5-MeIm)2]+ have been shown to
form two different low-spin crystalline species. They are
structurally distinguished by the relative orientation of the
two axial ligands. We have synthesized and structurally
characterized a new bis-ligated complex, perp-[Fe(OEP)(2-
MeHIm)2]Cl. Interestingly, this new complex is a low-spin
species with two perpendicular ligands that is distinct from
the related complex paral-[Fe(OEP)(2-MeHIm)2]ClO4 26 with
parallel axial ligands and a high-spin state. As expected from
analogous iron(III) species, the porphyrin core in this new
species is necessarily ruffled to accommodate the two
sterically hindered ligands. The solid-state structure shows
that the coordinated imidazole ligands form hydrogen bonds
with the chloride anions and provides a probable explanation
for the apparent stronger ligand field observed in this
complex.
In those model compounds, most bis-ligated d5 iron(III)
complexes have a characteristic rhombic EPR spectrum,12
with three observed g values, while some iron(III) species
have an unusual EPR spectrum: a single-feature low-spin
EPR signal with g g 3.2. This EPR spectral type has been
called large gmax13 or highly anisotropic low-spin (HALS).14
The origin of the large gmax EPR spectrum was first studied
in the complex [Fe(TPP)(2-MeHIm)2]+.15,16 This study
showed that the spectrum resulted from mutually perpen-
dicular axial ligands that lead to nearly degenerate iron dπ
orbitals. Subsequently, a number of additional iron(III)
species were shown to have the two planar ligands oriented
perpendicular to each other.17-19,22 Most of these species
display a large gmax EPR spectrum17,18,20,23 and an unusually
small value of the Mo¨ssbauer quadrupole splitting con-
stant.16,17,19,21,22 A final case is found for strong π-accepting
ligands, such as 3- and 4-cyanopyridine, where the interaction
with axial ligands lowers the energy of iron dπ orbitals below
dxy so that the ground state changes to (dxz,dyz)4(dxy)1. This
leads to a final type of EPR spectrum observed in low-spin
iron(III): an axial EPR spectrum. All of the complexes with
relative perpendicular ligands are found to have strongly
ruffled porphyrinato cores. For these systems, this conforma-
tion allows for the possibility of a π interaction between iron
and the porphyrin.
Experimental Section
General Information. All solvents were used as received. The
free-base porphyrin octaethylporphyrin (H2OEP)8 was purchased
from Mid-century. The metalation of the free-base porphyrin to
give [Fe(OEP)Cl] was done as previously described.27 [Fe(OEP)]2O
was prepared according to a modified Fleischer preparation.28
Synthesis of perp-[Fe(OEP)(2-MeHIm)2]Cl. To a solution of
[Fe(OEP)Cl] (30 mg, 0.05 mmol) in 10 mL of chloroform,
2-methylimidazole (20 mg, 0.24 mmol) was added. The mixture
was stirred for 4 h, then transferred into several 8 mm × 250 mm
glass tubes, and layered by hexanes as nonsolvent for crystallization.
After 10 days, block crystals were formed along with variable
amount of microcrystalline materials. Samples for Mo¨ssbauer
spectroscopy were made from single crystals enriched to 95% in
57Fe. In addition, Mo¨ssbauer spectroscopy verified that the micro-
crystalline material was identical to the block crystals.
X-ray Structure Determination. A dark red crystal with the
dimensions 0.46 × 0.20 × 0.12 mm3 was used for the structure
determination. The single-crystal experiment was carried out on a
Bruker Apex system with graphite-monochromated Mo KR radiation
(λ ) 0.71073 Å). The crystalline sample was placed in inert oil,
mounted on a glass pin, and transferred to the cold gas stream of
the diffractometer. Crystal data were collected at 100 K, Table 1.
The structure was solved by direct methods using SHELXS-
9729 and refined against F 2 using SHELXL-97;30,31 subsequent
difference Fourier syntheses led to the location of most of the
remaining nonhydrogen atoms. For the structure refinement all data
were used including negative intensities. The structure was refined
in space group P21/c. The program SADABS32 was applied for
In addition to the above-mentioned [Fe(OEP)(3-ClPy)2]-
ClO4,8 several other examples of iron(III) porphyrins with
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9722 Inorganic Chemistry, Vol. 45, No. 24, 2006