Angewandte
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complex in the reductive C N bond cleavage described
above. The neutral and diamagnetic dialkylaminocarbyne
complex [SiPiPr3]Fe(CNMe2) (5), can be prepared in a one pot
reaction via the sequential addition of Na(Hg) and MeOTf to
solutions of 1 (82% yield) (Figure 1). Fe(CNMe2) 5 is
isoelectronic to the previously reported iron siloxycarbyne
complex[9b] and accordingly displays a short Fe-C distance
(1.710(1) ꢀ), a long C-N distance (1.328(1) ꢀ), and a down-
field resonance (d = 279.6 ppm) in the 13C{1H} NMR spectrum
assigned to the carbyne carbon. Complex 5 is readily oxidized
by {Cp2Fe}{BArF24} to afford {[SiPiPr3]Fe(CNMe2)}{BArF
(6). The salient spectroscopic features of Fe(CNMe2)+
closely match those of the isoelectronic Fe(CNH2)+
}
6
4
24
(Figure 2). Compounds 5 and 6 are very stable in solution
and in the solid state when stored at room temperature under
an inert atmosphere.
Fe(CNMe2) 5 was found to react with proton and electron
equivalents to afford a mixture of CH4, Me2NH and small
amounts of Me3N. Whereas Fe(CN) 1 is reduced to CH4 and
NH3 with Cp*2Co and [2,5-Cl2-PhNH3][OTf] (vide supra),
exposure of Et2O solutions of 5 to these reagents only
furnishes small quantities of CH4 (ca. 0.01 equiv/Fe). Appa-
rently, more reactive proton and electron sources are required
Figure 3. A) Representative GC-FID chromatograms of sampled head-
spaces in the reaction of (dashed gray) 1 or (dashed black) [TBA][CN]
with 24 equiv Cp*2Co and 24 equiv [2,5-Cl2-PhNH3][OTf] in Et2O, and
(black) 5 with 10 equiv KC8 and 10 equiv HOTf. B) Mass spectrum of
CH4 produced from 1. C) Mass spectrum of CH4 produced from
compound 13C-1. D) Mass spectrum of CHxD4ꢀx produced from 1,
24 equiv Cp*2Co and 24 equiv partially-enriched DOTf.
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for C N bond scission in the case of 5, and 0.47 equiv of CH4
are detected when 5 is exposed to 10 equiv of KC8 and HOTf
(Figure 3) and found to contain 0.41(8) equiv/Fe of CH4.
Exposure of 13C-1 to these reaction conditions furnishes 13CH4
as the dominant isotopomer detected by GC-MS (Figure 3C).
Finally, replacing [2,5-Cl2-PhNH3][OTf] with partially-
enriched DOTf as the proton source furnishes a mixture of
deuterated methane products with masses up to and including
20 (Figure 2D) as is expected for CD4. Very little CH4 is
detected (0.007 equiv) when [TBA][CN] is used in place of
1 in these reactions (Figure 2A). Taken together, these
analyses indicate that the [SiP3iPr]Fe fragment facilitates the
proton-coupled six-electron reduction of coordinated cyanide
to CH4 and NH3 in moderate overall yields.
(Scheme 3). Reactions that employ 13C-5 generate 13CH4 as
Scheme 3. Reductive protonolysis of Fe(CNMe2) 5. Refer to the Sup-
porting Information for experimental details.
We also studied the stoichiometric reactivity of the
Fe(CNH) and Fe(CNH2) complexes to assess the intermedi-
acy of these species in a cyanide cleavage process. In the
absence of additional proton or electron equivalents, Fe-
(CNH2) 4 is unstable in solution (t1/2 (293 K) = 24 min), decaying
the predominant isotopomer, confirming the carbyne carbon
as the source of this hydrocarbon. Analysis of the reaction
volatiles obtained when 15N-5 is exposed to these conditions
reveals two detectable 15N-containing products (see the
Supporting Information). Resonances assigned to the N-H
protons of [H15NMe3][Cl] and [H215NMe2][Cl] are present at
to
a mixture of Fe-containing products that include
{[SiPiPr3]Fe(CNH)}{OTf} (3’) and [SiPiPr3]Fe(OTf)[6c] as read-
ily-identified species. Independent reactions reveal that both
NH3 (0.09(2) equiv/Fe) and H2 (0.24 equiv/Fe) are released on
leaving solutions of 4 to stand overnight. Furthermore,
Fe(CNH) 3’ slowly converts to [SiPiPr3]Fe(OTf) in THF
solutions (t1/2(298 K) = 4 h), presumably with the loss of the
CNH ligand. A similar ligand displacement reaction was
observed for the hydrazine adduct, {[SiPiPr3]Fe(N2H4}{OTf}.[9a]
This ligand exchange is likely irreversible under the relevant
reaction conditions as free hydrogen isocyanide readily
converts to hydrogen cyanide.[7a] Non-productive decomposi-
tion of an Fe(CNHx) complex may therefore partially account
for the moderate yields (< 41%) of CH4 and NH3 formed
upon exposure of 1 to excess proton and electron equivalents.
Given the challenges arising from the thermal instability
of 4 and 3’ in solution, we pursued more robust Fe(CNR2)
species to model the intermediacy of a terminal Fe carbyne
1
d = 10.84 and 9.05 ppm, respectively, in the H NMR spec-
trum and display well-resolved coupling to adjacent 15 N- and
1
1H nuclei. Comparison of the features present in the H, 13C,
and 15 N NMR spectra to authentic samples of these ammo-
nium salts solidifies their assignments. [SiPiPr3]Fe(OTf) was
identified as the major Fe-containing product of these
reactions (see the Supporting Information).
The organic products of these reactions lend some insight
into possible pathways for Fe-mediated cyanide reduction.
Upon exposure of Fe(CNMe2) 5 to proton and electron
equivalents, dimethylamine is found to be the dominant
(90%) N-containing product. Its formation is consistent with
a mechanism whereby an early cleavage of the cyanide-
ꢂ
derived C N bond occurs and is followed by the formation of
CH4. Scheme 4 outlines scenarios by which such a process
might in principle proceed, invoking unusual terminal carbide
Angew. Chem. Int. Ed. 2016, 55, 1 – 5
ꢀ 2016 Wiley-VCH Verlag GmbH & Co. KGaA, Weinheim
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