Alkylaluminum-Complexed Zirconocene Hydrides
A R T I C L E S
22,57 23,58 24,6g,h 31,59 33,28a,60 and 3530,61). Trimethylaluminum,
triisobutylaluminum, diisobutylaluminum hydride, and diisobuty-
laluminum chloride were used as obtained from Aldrich Chemical
Co., Milwaukee. CAUTION: alkylaluminum compounds are py-
rophoric and must be handled with special precautions (see, e.g.,
Shriver, D.F. The Manipulation of Air-sensitiVe Compounds; Robert
E. Krieger Publishing Company; Malabar, Florida, 1982).
Reaction mixtures for NMR measurements were prepared by
dissolving a weighed amount of solid zirconocene starting com-
pound, in an oven-dried J Young NMR tube, in benzene-d6 or
toluene-d8 under inert atmosphere. Aluminum reagents were added
as neat liquids via microliter syringes. NMR spectra were obtained
using Varian Inova 400, 500, or Mercury 300 spectrometers.
Chemical shifts are referenced to residual solvents peaks, 7.160
ppm for benzene and 7.000 ppm for the central aromatic proton
resonance of toluene.
ZrCl2/MAO reaction systems upon addition of HAliBu2,16b are
species of the type (SBI)Zr(Me · · ·MAO)(µ-H)2AlMe2, in which
the terminal Zr-Me group is bound, without being cationized,39
to a Lewis acidic Al site of MAO.40 Interaction of excess
AlMe3salways present in these reaction systemsswith minor
fractions of a MAO-free species (SBI)Zr(Me)(µ-H)2AlMe2, on
the other hand, might make side exchange in this species fast
enough to give the symmetrized ZrH2 signal observed for
zirconocene dihydride complexes in these reaction media.16b
Such a “mild” sequestration of the Zr-Me group would be
analogous to that observed in reaction systems (C5H5)2ZrMe2/
MAO at relatively low [Al]MAO/[Zr] ratios of 20-50,41 and
might be sufficient to suppress an otherwise prevalent methane
elimination, at least to a substantial degree. A residual extent
of CH4 release even from these MAO-stabilized complexes
might explain the ubiquitous formation of methane from
“working” zirconocene-based polymerization catalysts42 and,
likewise, the still enigmatic formation of zirconocene species
with a long-wavelength absorbance, at ca. 600 nm, possibly due
to a zirconocene species containing Zr in a reduced oxidation
state,43 in reaction systems containing (SBI)ZrCl2 and MAO
upon addition of HAliBu2.16b Further fates of such reduced
zirconocene species, i.e., their contribution to irreversible catalyst
deactivation and/or their reconversion to active cationic catalyst
species, remain a topic for future investigations.
Acknowledgment. This research was supported by USDOE
Office of Basic Energy Sciences (Grant No. DE-FG03-85ER13431),
by Fonds der Chemischen Industrie, and by BASELL Polyolefine
GmbH. We are grateful to Professor Peter Burger (University of
Hamburg) for DFT calculations on problems related to the work
reported here, to Dr. Heike Gregorius (BASELL, Frankfurt/Main)
for a gift of a sample of complex 16, and to Dr. Markus Ringwald
(MCAT, Konstanz) for gifts of samples of several zirconocene
complexes.
Supporting Information Available: Additional figures and
appendix outlining the analysis of changes in the chemical shift
of the ZrH2 signal of (SBI)ZrCl(µ-H)2AliBu2 upon addition of
Al2Me6. This material is available free of charge via the Internet
Experimental Section
All operations were carried out under a protective dinitrogen
atmosphere, either in a glovebox or on a vacuum manifold.
Benzene-d6, toluene-d8, and other solvents used were dried by
vacuum transfer either from sodium benzophenone or from “ti-
tanocene”.44 Zirconocene complexes used as starting materials were
either purchased from Strem Chemicals, Newburyport (1, 6, 12,
and 17), obtained as gifts from Dr. M. Ringwald, MCAT, Konstanz
((EBTHI)ZrF2,45 27, 28,46 and 3647) and from BASELL Polyolefins,
Frankfurt/Main (1648), or prepared in our laboratories according
to published procedures (3,49 8,50 10,51 13,52 18,5319,54 20,55 21,56
JA8054723
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(SBI)ZrCl2 and (SBI)ZrMe2, rather than to those of the cationic species
[(SBI)Zr(µ-Me)2AlMe2]+ MeMAO- or [(SBI)ZrMe+ · · ·MeMAO-]
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systems are quite similar to each other; both show broad absorbance
bands around 380 and 340 nm (ref 16b).
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