(
)
46
G.P. Rosini et al.rJournal of Organometallic Chemistry 554 1998 41–47
d CHE-d10 rdt
K2 a k4 a
K2 k4
ments were performed with a temperature-programmed
s
s
s0.10 no CO
14
Ž
.
Ž
.
Ž
Varian 3400 using a 50-m HP-1 cross-linked methylsil-
d CHE-h10 rdt
d CHE-d10 rdt
d CHE-h10 rdt
.
icone gum phase capillary column and a flame ioniza-
k2 a k4 a
k2 k4
tion detector. Authentic cyclooctene and cyclohexene
were used to generate calibration curves which encom-
passed the experimental concentration range. Baseline
separation of the cyclohexane isotopomers was achieved;
the identity of C6 D10 was confirmed by comparison
with authentic C6 D10 generated from dedeuterogenation
of C6 D12. Irradiations were conducted using a 500 W
Hg-arc Oriel lamp, and the desired wavelengths were
s0.24 high CO pressure
Ž
.
.
15
Ž
w
x
In the low- CO limit, the alkyl hydride isotopomers
exist in a pre-equilibrium and the product ratio reflects
Ž
Ž
.
.
the equilibrium constant K2a rK2 and the ratio of
w
x
rates of b-H elimination k4a rk4 . In the high- CO
Ž
achieved using filters obtained from FJ Gray Corning
7-83 for 366 nm and 0-56 for l)280 nm .
limit, the alkyl hydride most frequently reacts with CO
.
Ž
.
unproductively ; elimination of alkane is kinetically
insignificant. In this case, the product ratio reflects the
3.2. Typical photolysis conditions
Ž
.
relative rates of C–H addition k2a rk2 and the relative
Ž
.
rates of b-H elimination k4a rk4 . Thus both limits are
dependent upon the relative rates of b-H elimination;
however, in the high-pressure case b-H elimination is
predominantly in competition with CO addition, while
in the low-pressure case it occurs predominantly in
competition with elimination or exchange of alkane.
Stock solutions of 2.0 mM 1 were prepared in cy-
clooctane, cyclohexane, and d12-cyclohexane. In gen-
eral, 1.5-ml samples were prepared using the appropri-
ate mixture of stock solutions. The samples were placed
in a quartz cuvette sealed to a ballast used to maintain
constant partial gas pressures and equipped with ports
for attachment to a vacuum line and for removal of
microliter samples for GC analysis. The samples were
2.3. Conclusions
Ž
placed under a total pressure of 800 torr mixtures of Ar
Varying CO pressure significantly affects the inter-
.
and CO , and then irradiated at 508C. The samples were
Ž
molecular selectivity cyclooctanercyclohexane or
then analyzed at various times by GC for alkene forma-
tion. Product ratios COE:CHE and CHE-d10 :CHE-h10
were found to remain constant with time.
.
C6 D12rC6 H12 of 1-catalyzed alkane dehydrogenation,
with saturation being observed at ca. 400 torr CO. In
conjunction with previous mechanistic studies, this ef-
fect can only be explained by a mechanism in which
CO attacks the respective alkane adducts — even if CO
addition to the different adducts is assumed to occur at
Acknowledgements
Ž
equal rates as is the case in the C6 D12rC6 H12 compe-
We thank the Division of Chemical Sciences, Office
of Basic Energy Sciences, Office of Energy Research,
US Department of Energy for support of this work.
A.S.G. thanks the Camille and Henry Dreyfus Founda-
tion for a Teacher Scholar Award and the Alfred P.
Sloan Foundation for a Research Fellowship.
.
tition . An inverse isotope effect for loss of alkane from
the adduct is calculated, kh-12rkd-12 s0.42; this strongly
Ž
.
suggests that the adducts are alkyl hydrides deuterides
rather than solvated or s-bound species. Since the reac-
tion of CO with other species such as solvated or
s-bound RhL2Cl does not occur to a kinetically signifi-
cant extent, it may be inferred that such species are not
present in significant concentration relative to the alkyl
hydrides. This implies that formation of the alkyl hy-
drides, i.e. oxidative addition to the RhL2Cl photo-
product, is both kinetically very facile and thermody-
namically very favorable.
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ously 4 . Gas chromatographic analyses for all experi-