(Alkenyl)zirconocene chlorides
Cp2Zr(Cl)(CHCHR) (4, R = H,
phenyl, n-butyl, or cyclohexyl)
react with “Cp2Zr” generated from various
precursors to yield the neutral dinuclear alkenyl-bridged
bis(metallocene) complexes 6
[Cp2Zr(μ-Cl)(μ-η1:η2-CHCHR)ZrCp2].
The complexes 6 are regioselectively
protonated by treatment with
(HNMe2Ph+)(BPh4
-)
(8a) to yield the unusually structured products 9
[Cp2Zr(μ-Cl)(μ-η1:η2-C1H2C2HR)ZrCp2
+],
which exhibit an unsymmetrically bridged hydrocarbyl ligand
containing
a novel type of a hypercoordinated carbon center (C1)
inside the rigid organometallic framework. From the
NMR analysis and an X-ray crystal structure determination of the
example 10c
[(MeCp)2Zr(μ-Cl)(μ-C1H2C2H-n-butyl)Zr(MeCp)2
+], it
is evident that the hypercarbon atom C1 is coordinated to
four close neighboring
atoms (Zr1, Zr2, C2, and
H1a) in a distorted square-planar arrangement with the
remaining C1−H1b bond being
oriented perpendicular to it. H1b thus marks the apex
of a distorted square pyramid; the hypercarbon atom
C1
is located in the center of the basal plane. This unusual
structural coordination geometry around C1 is
determined
by the stereoelectronic features of the two adjacent group 4 bent
metallocene units. From the dynamic features
of complex 9a (R = H), a stabilization energy of ca. 10
kcal mol-1 is estimated for the uncommon
coordination
mode of C1, which is favored here, relative to a “normal”
sp3-hybridized structure in a
C
2
v
-symmetric
metallacyclic framework. Part of the pronounced thermodynamic
stabilization of this unusual pentacoordinate
carbon geometry originates from the strong α-agostic
Zr···H1a−C1 interaction in the basal
plane. From the
monodeuterated derivative 9a-C1HD, an
energy difference of 220 cal mol-1 between D
and H favoring the
bridging position was determined.