A R T I C L E S
Laws et al.
below. The reasons for this underdevelopment would seem to
be the relatively positive potential of the couple (ca. 0.9 V vs
ferrocene) and the instability of the radical cation on the longer-
term (spectroscopic or electrosynthetic) time scale. This paper
addresses the second of these points, which we consider to be
the more serious impediment to development of cymantrenyl
redox tags.
The expectation that cymantrene would be significantly harder
to oxidize than ferrocene owing to the presence of its strongly
π-accepting carbonyl groups has been confirmed both by
photoelectron spectroscopy (PES)6,7 and by a number of
electrochemical studies.8–15 More poorly understood, however,
is the dramatically reduced lifetime of the cymantrene radical
cation, 1+, compared to the ferrocenium ion. The frontier orbitals
of cymantrene and ferrocene are similar in makeup, both
compounds being viewed as pseudo-octahedral systems in which
the three fac carbonyls are topologically equivalent to the Cp
anion,16,17 with the three highest-energy filled orbitals for the
d6 complexes being closely spaced in energy. In the case of
cymantrene, these orbitals are derived primarily from e- and
a-type contributions of the Mn(CO)3 moiety,18–20 and their close
spacing has been confirmed experimentally by the finding that
the lowest energy ionizations of cymantrene are unresolved by
PES.6,7 A number of groups have shown8–12 that the one-
electron anodic oxidation of 1 is at least partially chemically
reversible on the CV time scale21 in nonaqueous media, but
based on the published work, even in situ spectral characteriza-
tion of 1+ has apparently eluded investigators22 (carbonyl-
substituted derivatives have proven more stable, as will be
discussed below). Qualitatively, it might be expected that
removal of an electron from 1 would weaken the Mn-C(O)
bonds (owing to reduced metal-to-CO back-bonding) and
perhaps the Mn-Cp bond (depending on the nature of the
SOMO of 1+). However, neither of these possibilities seemed,
to us at least, sufficient to make the cymantrene radical cation
inherently unstable under the conditions employed for its
electrochemical generation. The treatment by Field et al.7 of
the highest filled orbitals of 1, concluding that the trio of e-
and a-type orbitals have significant metal-ligand mixing, further
begs the question of why 1+ does not exhibit greater stability.
We set out to see if its reported decomposition arose from
follow-up reactions with the electrochemical supporting elec-
trolyte anions, usually either [PF6]- or [BF4]-, which are known
to have modest nucleophilicity toward organometallic radical
cations.23–25 This is, indeed, the case. In this paper we show
that when the cymantrene radical cation is generated in a
medium consisting of CH2Cl2 and [NBu4][B(C6F5)4], it is
persistent on a synthetic (electrolysis) time scale, allowing its
broad spectral characterization (UV-vis, IR, near IR, ESR, and
1H NMR). Furthermore, two of its Cp-substituted analogues,
namely the amino-substituted complex Mn(C5H4NH2)(CO)3, 2,
(3) Leading references to the literature of ferrocenyl redox tags are: (a)
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is approximately 10 s.
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A
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Mn
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) 91.6 G) is also likely to have arisen from
Mn
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