1574 Inorganic Chemistry, Vol. 39, No. 7, 2000
Shea and Westmoreland
Ru10 (Cp* ) pentamethylcyclopentadienyl anion; MeCp ) methyl-
invariably contaminated with ruthenocene and octamethylruthenocene.
Addition of a substoichiometric amount of [Cp2
11,12
cyclopentadienyl anion), (R4N)X2Y, and (R4N)X3
(R ) Me, Et,
RuX]+ preferentially
n-Bu; X, Y ) Cl, Br, I).
oxidizes the octamethylruthenocene present in the sample. Once the
octamethylruthenocene has been quantitatively converted to haloocta-
methylruthenocenium, additional [Cp2RuX]+ oxidizes tetramethyl-
ruthenocene only. Similarly, hexamethylruthenocene can be selectively
oxidized in the presence of pentamethylruthenocene contamination.
CD3CN for kinetic measurements was obtained from Cambridge
Isotopes in sealed glass ampules and contained <1% water as
determined by NMR. For other NMR experiments, CD3CN from
Aldrich or Cambridge Isotopes was distilled over CaH2 prior to use.
Reported chemical shifts are referenced to the solvent peak (CHD2CN
at 1.93 ppm). A Hewlett-Packard 8451A diode array UV-vis spec-
trophotometer was used for optical absorbance measurements.
Detailed preparative procedures and analytical data for all the new
complexes are available elsewhere.15 1H NMR and optical absorbance
spectral data for all oxidized metallocenes are available in the
Supporting Information.
(Me4Cp)CpRu (Me4Cp ) 1,2,3,4-Tetramethylcyclopentadienyl
Anion). Tetramethylruthenocene has not been previously reported but
can be approached by modification of published routes to pentadienyl
complexes.13 RuCl3‚xH2O (5.00 g, 24 mmol) was added under N2 to
100 mL of degassed (three freeze-thaw cycles) EtOH and was stirred
until complete dissolution had occurred to yield a green-brown solution
(2-3 h). Exactly 1.59 mL of cyclopentadiene (23.7 mmol) was added
followed by 8.00 g (65.5 mmol) of tetramethylcyclopentadiene. It is
critical that a 1:1 ratio of RuCl3 to HCp is used. If an excess of
cyclopentadiene is present, then a significant increase in the yield of
ruthenocene is observed. If there is too little, octamethylruthenocene
becomes the major product of the reaction. An amount of 15.8 g of Zn
dust was added slowly, and the solution was heated at reflux for 6 h.
The solvent and other volatiles were removed under vacuum. The solid
residue was extracted with hot hexanes, and the extracts were filtered
through a Celite pad. The filtrate was then loaded onto a short, basic
Al2O3 column and eluted with hexanes. The solvent was removed from
the combined metallocene-containing fractions by rotary evaporation
to give an oil containing (Me4Cp)CpRu (46.7%), Cp2Ru (21.4%), and
(Me4Cp)2Ru (31.9%). Separation of the metallocenes proved to be
difficult, and the mixture was used for subsequent experiments requiring
NMR Kinetics. All NMR data were collected on a Varian Gemini
300 MHz spectrometer. Integrations of 1D and 2D data were performed
using routines supplied by Varian.
For exchange rates greater than about 104 M-1 s-1, standard line
broadening techniques16 based on a temperature-dependent line width
analysis in a near-fast exchange limit were employed. For slower rates,
2D exchange spectroscopy (EXSY)17 was used to measure the rates.
To obtain kinetic data, appropriate amounts of a haloruthenocenium
salt and its corresponding reduced form were weighed into an NMR
tube and CD3CN was added to give final concentrations of the two
species near 5 mM. For tetramethylruthenocene and hexamethylrutheno-
cene, however, purified samples were not available and the oxidations
were performed in situ. In these cases, the mixture of reduced
metallocenes was placed in an NMR tube with CD3CN, and [Cp2RuX]+
was added until there were approximately equal amounts of the oxidized
and reduced forms of the compound of interest. The relative concentra-
tions of the exchanging species were determined from a 1D NMR
spectrum of the solution. The absolute concentrations were determined
after the kinetic data were obtained from optical absorbance data and
the molar absorptivities of the haloruthenoceniums.
1
tetramethylruthenocene and its derivatives. H NMR (CD3CN, ppm)
of (Me4Cp)CpRu: 4.39 (s, 1H), 4.24 (s, 5H), 1.93 (s, 6H), 1.88 (s,
6H).
A standard EXSY pulse sequence was used to acquire two-
dimensional exchange data.17 For each experiment, 256 1024W free
induction decays of eight scans each over a sweep width of 1800-
2000 Hz with a recycle delay of 0.5-20.0s were collected in phase-
sensitive mode. The integrated EXSY peak intensities were used to
determine the exchange rate constants and variances as described
elsewhere.6,17 After each EXSY experiment, the 1D spectrum was
reacquired to ensure that no decomposition had occurred. A tabulation
of the 2D integrals is given in the Supporting Information.
Oxidation of Metallocenes. Two general pathways were employed
for metallocene oxidation. For chloro- or bromometalloceniums, the
metallocene may be oxidized by Fe(III) in the presence of the halide.3
In a typical preparation, a solution of ∼1.6 mmol metallocene in 30
mL of benzene was added to a solution containing an excess of Fe(III)
in 15 mL of dilute (∼4M) aqueous HX (X ) Cl, Br). After the solution
was vigorously stirred for several hours, the aqueous phase was
separated and washed with benzene and ether. An excess of NH4PF6
dissolved in a small amount of water was added, and the solution was
allowed to stand overnight. The product was collected as a powder by
filtration, washed with benzene and ether, and recrystallized from CH3-
CN/Et2O.
A second pathway for metallocene oxidation involved oxidation by
[Cp2RuX]PF6 (X ) Cl, Br, I). It has been established from potentio-
metric studies that for the complexes reported herein the oxidizing
ability of haloruthenocenium cations decreases with increasing number
of methyl groups.14 A substoichiometric amount of [Cp2RuX]PF6 was
added to a solution of the metallocene in CH2Cl2. The mixture was
stirred for 0.5 h, then the solvent was removed by rotary evaporation
and the reduced metallocenes were extracted from the powder using
hexanes. The oxidized product in the residue was then recrystallized
from CH3CN/Et2O.
Halide Substitution Equilibria. Equilibrium constants for the halide
substitution of haloruthenoceniums were obtained using procedures
described previously.6 CD3CN solutions of the haloruthenoceniums were
mixed with substoichiometric amounts (∼0.1 molar ratio) of (R4N)-
XY2 or (R4N)X3 (R ) Me, Et, n-Bu; X,Y ) Cl, Br, I) at 298 K. The
NMR spectrum and optical absorption of the mixture were monitored
periodically until no further change was detected (6-12 h, depending
on X and Y). The UV-vis absorption spectrum of the equilbrium
mixture was fit to a sum of reference spectra of the absorbing species
using a nonlinear least-squares fitting program18 to obtain the equilib-
rium concentrations of each species. Errors in calculated concentrations
range from 1% to 5% for reactions involving iodo and bromo species
and from 5% to 10% for reactions involving chloro species.19 The UV-
vis fits and equilibrium concentrations are provided in the Supporting
Information.
The atom-transfer oxidation method has advantages over the more
direct approaches when selective oxidation of a mixture of metallocenes
is required. For example, samples of tetramethylruthenocene were
(15) Shea, T. M. Ph.D. Dissertation, Wesleyan University, 1999.
(16) Martin, M. L.; Delpuech, J.-J.; Martin, G. J. Practical NMR Spec-
troscopy; Heyden and Son: Philadelphia, 1980; pp 293-310.
(10) See Supporting Information for the following. Bretschneider-Hurley,
A.; Winter, C. H. J. Am. Chem. Soc. 1994, 116, 6468-6469.
(11) Chattaway, F. D.; Hoyle, G. J. Chem. Soc. 1923, 123, 654-662.
(12) (a) Popov, A. I.; Geske, D. H. J. Am. Chem. Soc. 1958, 80, 1340-
1352. (b) Popov, A. I.; Geske, D. H. J. Am. Chem. Soc. 1958, 80,
5346-5349. (c) Iwamoto, R. T.; Nelson, I. V. J. Electroanal. Chem.
1964, 7, 218-221.
(17) (a) Jeener, J.; Meier, B. H.; Bachman, P.; Ernst, R. R. J. Chem. Phys.
1979, 71, 4546-4553. (b) Macura, S.; Ernst, R. R. Mol. Phys. 1980,
41, 95-117. (c) Mendz, G. L.; Robinson, G.; Kuchel, P. W. J. Am.
Chem. Soc. 1986, 108, 169-173. (d) Abel, E. W.; Coston, T. P. J.;
Orrell, K. G.; Sik, V.; Stephenson, D. J. Magn. Reson. 1986, 70, 34-
53. (e) Perrin, C. L.; Dwyer, T. J. Chem. ReV. 1990, 90, 935-967.
(18) Press, W. H.; Teukolsky, S. A.; Vetterling, W. T.; Flannery, B. P.
Program MRQMIN. In Numerical Recipes in Fortran, 2nd ed.;
Cambridge University Press: Cambridge, U.K., 1992; pp 678-683.
(19) The increased error for the fits involving the chloro species is due to
the difficulty of obtaining the spectrum of an analytically pure sample
of (R4N)Cl3 with no evidence of decomposition products.
(13) (a) Gleiter, R.; Hyla-Kryspin, I.; Ziegler, M. L.; Sergeson, G.; Green,
J. C.; Stahl, L.; Ernst, R. D. Organometallics 1989, 8, 298-306. (b)
Bosch, H. W.; Hund, H.-U.; Nietlispach, D.; Salzer, A. Organome-
tallics 1992, 11, 2087-2098.
(14) Xu, A. N.; Westmoreland, T. D. Manuscript in preparation.