3268
M. Verschoor-Kirss et al. / Journal of Organometallic Chemistry 694 (2009) 3262–3269
The susceptibility data (both leff versus T and M versus H) con-
5. Conclusions
firm that electron transfer has indeed occurred and that the prod-
uct of the reaction between 1 and DDQ is not a (diamagnetic)
neutral charge transfer complex similar to the mixed stack tetracy-
anoethylene complex of ferrocene [27], or the iodine adduct of
FcCH@NC6H4@NCHFc, [FcCH@NC6H4@NCHFc][I4.5][28]. The tem-
perature dependence of the Mössbauer spectra of [FcCH@NC6H4@
NCHFc][I4.5], a mixed iron(II) and iron(III) complex at ambient T)
reveals [28] an increase in the fraction of low-spin FeII relative to
FeIII at lower temperatures concurrent with a decrease in the effec-
tive moment. These results are consistent with a unique retro-elec-
tron transfer process from the poly-iodide anion to FeIII and that is
fully reversible. No such behavior is observed for either of
[1+Å][DDQÅꢀ] or [2+Å][DDQÅꢀ].
The electrochemistry of 2 alone provides few clues to the nature
of the oxidized product. Like the electrochemistry of 1, the anodic
electrochemistry of 2 suggests a single-electron, reversible process
in solution. The oxidation potential of 2 is only slightly more posi-
tive than that of ferrocene but 2 is, apparently, considerably more
difficult to oxidize than 1. Again, electron transfer from an electron
donor, 2, to the electron acceptor (DDQ) is confirmed by the mag-
netic susceptibility measurements. In the solid state, dramatically
different behavior is observed in the Mössbauer spectra of
[2Å+][DDQÅꢀ]. The chemical oxidation of 2 clearly favors a product
where iron has been oxidized from FeII to FeIII. Compound
[2Å+][DDQÅꢀ] contains essentially all low-spin FeIII at 293 and
77.5 K. This is the exact opposite of the observations for
[1Å+][DDQÅꢀ].
While the anodic electrochemistry of 1 and 2 appears to be con-
sistent with oxidation of ferrocene FeII to ferrocenium FeIII, the
products of chemical oxidation with the single-electron oxidant
DDQ lead to surprisingly different results. The product of chemical
oxidation of 1 suggests loss of an electron from the ligand, delocal-
ization of the odd electron into the p-system of the pyrrole ligand
or initial oxidation at iron followed by intramolecular electron
transfer from the ligand to iron. The structure of [1]Å+ is mostly
likely to be either a, b, c, or a hybrid thereof, in Eq. (3) rather than
d. The strongest evidence for this conclusion comes from the
Mössbauer spectra, a technique that has proven to be accurate in
distinguishing low-spin FeII from FeIII in the solid state. Low-spin
FeIII, however, is clearly seen in the Mössbauer spectrum of the
product of chemical oxidation of 2. The contrasting behavior of
two seemingly similar ferrocene-substituted nitrogen heterocycles
suggests that further studies of the chemical oxidation of a wider
range of compounds are warranted. Finally, the present results
may in part ultimately reflect the fundamental differences be-
tween solution species as obtained via classical electrochemical
oxidations versus direct chemical reactions accompanied in some
cases by rapid crystallization of the solid and for which imponder-
able lattice effects can be important in the context of the species
that is actually stabilized.
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