4362 J. Am. Chem. Soc., Vol. 122, No. 18, 2000
Hauser et al.
2
2
experimental observation. Even if covalency and lattice con-
tributions significantly influence the actual values of the efg
components, it is difficult to envisage a reversal of the sign of
Vz′z′, particulary in this case of a strong axially symmetric efg.
(ii) The symmetry of the magnetic hyperfine coupling tensor
Aeff as can be derived from the t2g-hole description of 1 is also
not consistent with the experiment: The orbital and spin-dipolar
contributions to A in this model33,36 yield the largest, negative
component of A in the direction of the efg main component,
whereas in the simulations of the spectra the Aeff component
along the efg z-direction was found to be the weakest (and
positive).
to the assumption that the antibonding dx -y orbital is too high
2
in energy above the dz and the dπ orbitals to be populated.
The resulting ground-state configuration is basically (dxy)2(dxz)1-
1
2
(dyz)1(dz ) .
High-field Mo¨ssbauer measurements (7 T, 4.2 K) of the {Fe-
NO}8 and the {Fe-NO}6 species derived from 1 by electro-
chemical reduction and oxidation, respectively, reveal an S )
0 ground state for both complexes, namely trans-[(cyclam)Fe-
(NO)(Cl)]0 and trans-[(cyclam)Fe(NO)(Cl)]2+. Also, for [L′Fe-
(NO)(ONO)(NO2)]+, an {Fe-NO}6 species, a diamagnetic
ground state has been established. We assume that the S ) 0
ground state of these complexes owes its origin to strong
intramolecular spin couplings (see below). The magnetic Mo¨ss-
bauer spectra (Figure S4) were simulated by using the isomer
shifts and the electric quadrupole splittings from the respective
zero-field spectra. All species, namely the {Fe-NO}6 and the
{Fe-NO}8 derivatives of 1 and [L′Fe(NO)(ONO)(NO2)]+,
possess a positive sign of the quadrupole splitting and high axial
symmetry of the efg with η ≈ 0. The low isomer shift and large,
positive quadrupole splitting with η ≈ 0 of the two present {Fe-
NO}6 species are consistent with those observed for Werner-
type octahedral low-spin FeIV complexes.15 The axial efg can
be rationalized in a ligand field model for the spin-orbit
interaction of distorted octahedral (t2g)4 complexes. In this model
the valence contribution to the efg originates from two electron
holes in the t2g subshell which is positive for a (dxy)2(dxz)1(dyz)1
ground-state configuration of FeIV.44-47 Thus the electronic
structures of trans-[(cyclam)Fe(NO)Cl]2+ and [L′Fe(NO)(ONO)-
(NO2)]+, both of which are of the {Fe-NO}6 (S ) 0) type, can
be described as low-spin FeIV (S ) 1) coupled antiferromag-
netically to an NO- (S ) 1) ligand.
These arguments led us to consider the alternative description
of 1, not as a low-spin FeIII complex but as an antiferromag-
netically coupled system of intermediate-spin ferric ion (S )
3/2) and an NO- (S ) 1). Since in this picture iron has the major
eff
local spin, the sign of the isotropic part Aiso with respect to
1
the system spin St ) /2 is the same as that of the (negative)
intrinsic value. The value of the isotropic part turns out to be
rather weak in this model (1/3tr(AFe(III),S)3/2) ) -5 T), when
the experimental value for the system spin is converted
according to the spin-projection formula AFe(III),S)3/2 ) +3/5 Aeff.
However, this does not contradict the basic assumption of
intermediate spin FeIII, because it is clear that spin-dipolar
contributions and covalent orbital delocalizations cannot be
neglected for a nitrosyl complex.
Iron(III) intermediate spin states were first reported for five-
coordinate iron porphyrinates with square-pyramidal geometry;37
but other examples with salen and dithiocarbamate and other
ligands are also described in detail.38-40 The large pos-
itive quadrupole splitting (≈+3 mm s-1, η ≈ 0) was recognized
as a characteristic feature of intermediate-spin ferric por-
phyrinates.41 Detailed analyses of EPR and Mo¨ssbauer spectra
showed the presence of a highly anisotropic hyperfine tensor
with large, negative components in x/y-directions and weak,
positive z-components. Both features, the positive, axial quad-
rupole interaction and the anisotropic magnetic hyperfine tensor,
are very similar to what we found for 1. In the theoretical model
developed by Maltempo42 the “spin-Hamiltonian” parameters43
are derived by mixing of close lying 4A2 and 6A1 orbital singlet
states. Square-planar geometry was taken as the starting point
for the description of the spin-quartet ground state, according
Discussion
Rodriguez et al.3 have recently reported a detailed Mo¨ssbauer
study and density functional theory calculation on the nitrosyl
derivatives of deoxyhemerythrin which contains a high-spin
ferrous site with isomer shift and quadrupole splitting at 1.21
and +2.66 mm s-1, respectively, and a nitrosyl iron site {Fe-
NO}7 (S ) 3/2) with 0.68 and +0.61 mm s-1, respectively. While
the isomer shift for the former was considered to be normal
(typical) for an octahedral ferrous ion in an oxygen/nitrogen
donor environment, the latter value has been considered
“unusual” or not typical (in fact enhanced) with respect to a
normal high-spin ferric ion or, conversely, reduced with respect
to a high-spin ferrous ion. They concluded that an isomer shift
of 0.68 mm s-1 is intermediate between high-spin ferrous and
ferric and does not allow an oxidation state assignment.
In contrast to this interpretation we would like to point out
that the isomer shift is only considered to be unusual because
there are but few high-spin ferric complexes reported to date
with such large isomer shift. For example, Lippard et al.48 have
structurally characterized a (µ-1,2-peroxo)diiron(III) complex
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