Investigation of the SiH2 + H2O (and D2O) Reaction
J. Phys. Chem. A, Vol. 107, No. 50, 2003 11055
in excess of the threshold energy for redissociation to SiH2 +
H2O, reaction (-1). Thus, our calculations confirm the fact that,
after reaction 1 has occurred, there is no easy pathway for the
reaction to continue further. The calculations thus support the
experimental findings of a pressure dependent association
reaction, without involvement of an H-transfer process in the
rate determining step. The calculations provide the value for
Eo, the dissociation (or critical) energy for the RRKM modeling
studies.
those of the SiH2 + ROR′ systems. AKL19 have rationalized
this modeling outcome by arguing that, in the case of reaction
of SiH2 with O-donor molecules, there may be a long-range
interaction giving rise to higher than usual reaction cross
sections. Furthermore, they rationalize a positive activation
energy by involving a centrifugal potential barrier which is
important because of the extended nature of the Si‚‚‚O bond
and the weak binding energy of the zwitterion complex.
Although we have no evidence against these propositions, we
remain cautious about them, because it seems possible to us
that the SiH2 + ROR′ systems can nevertheless be explained
within the framework of loose but normal transition states which
seem to fit other SiH2 reaction systems5-10,12,15,17,18 and also
GeH2 reaction systems36-42 where more weakly bound com-
plexes are generally involved.
RRKM Modeling Studies. Before discussing the results of
the calculations in detail, we show that our RRKM modeling
can be made to fit the results of AKL.19 Using TSb (and Eo )
54 kJ mol-1), we repeated one calculation at 296 K but with
∆E down ) 3.6 kJ mol-1 (300 cm-1), a reasonable value for Ar
bath gas. The result is shown in Figure 8 where it can be seen
that good agreement with the experimental data of AKL19 is
It should be added that we have not undertaken variational
transition state theory calculations of the isotope effects because
of the lack of information about the activated complex. We could
have attempted this, as we did for the SiH2 (SiD2) + CH3CHO
reaction.18 However, the exercise undertaken in that work, with
a better defined activation complex set of structures, demon-
strated that the isotope effects for different degrees of freedom
were largely self-canceling, leading to values of kH/kD in the
range of 1.005-1.122 at the temperatures and pressures of the
present work. The calculations in that work combined the high
pressure limiting values, 1.097 (296 K) and 1.135 (339 K), with
the pressure dependent values (inverse isotope effect) which
reduced them by up to 10%. Such an outcome in the present
study would be entirely consistent with the experimental results.
Finally, it is interesting to note the conclusion that, in the
gas-phase both in this and related systems,19,21 the reaction
effectively stops at the zwitterion stage; that is, the zwitterion
is the actual reaction product! The idea of such species as
intermediates in reactions of silylenes with O-donor molecules
goes back to the 1980s and the solution studies of Weber’s
group.43-45 Clearly in solution, the zwitterions find ways to react
further, and the solvent plays an important role. In the gas phase,
the fate of the zwitterions is unclear. We suspect a wall or
otherwise catalyzed reaction, which is too slow to affect our
measurements.
obtained. The calculation (from Figure 3) with ∆E
) 12
down
kJ mol-1 (1000 cm-1) is also shown for comparison.
The calculations presented here show that a number of
activated complex models can be made to fit (approximately)
the experimental data. There are, however, two problems. First,
the fit to the data (regardless of model) is not very good. The
models all show that in the region of measurement the reaction
is approaching its third order region of pressure dependence.
The experimental rate constants, particularly at the lower
pressures (10 and 30 Torr) do not show such a strong trend
with pressure. Increases in k1 are less than a factor of 2, whereas
the pressure change is a factor of 3. It should be acknowledged
that, at 10 Torr, the substrate H2O or D2O forms a significant
proportion of the total gas mixture and differences of collision
efficiency between SF6 and H2O (or D2O) may play a role. The
measurements of AKL19 fit their (and our) RRKM calculations
better, but the lowest pressure used was 50 Torr and their total
pressure range was necessarily limited (50-200 Torr) because
of the low collision efficiency of the argon bath gas. The
behavior we observe can sometimes arise in complex systems
when a non-pressure-dependent competing side reaction be-
comes significant at low pressures. Although this remains
possible, the occurrence of a direct reaction to SiH3OH or H2
+ HSiOH can be ruled out, not only because the PE surface
shows the barriers to be too high but also because such processes
involve H-migration and therefore primary isotope effects would
become evident at low pressures. Thus, we believe there is some,
as yet unexplained, experimental contribution to the rate.35 The
second problem concerns the RRKM model. Our modeling
shows that the data can be fitted within a range of loose
transition states and corresponding critical energies. These
models incorporate both internal rotational modes and overall
active rotations. None of the fitting is definitive, because we
do not have reliable information about the activated complex.
This arises in this system because the high-pressure limit which
would provide such information does not occur until pressures
that are ca. 104-105 times those accessible in our experiments.
Because of their preference for a Gorin-type model, AKL19
Acknowledgment. R.B. and R.W. thank Dow Corning for
a grant in support of the experimental work. R.B. also thanks
the Spanish DGICYT for support under Projects BQU2000-
1163-C02-01 and BQU2002-03381.
References and Notes
(1) Jasinski, J. M.; Becerra, R.; Walsh, R. Chem. ReV. 1995, 95, 1203.
(2) Becerra, R.; Walsh, R. Kinetics & mechanisms of silylene reac-
tions: A prototype for gas-phase acid/base chemistry. In Research in
Chemical Kinetics; Compton, R. G., Hancock, G., Eds.; Elsevier: Amster-
dam, 1995; Vol. 3, p 263.
(3) Gaspar, P. P.; West, R. Silylenes. In The Chemistry of Organic
Silicon Compounds; Rappoport, Z., Apeloig, Y., Eds.; Wiley: Chichester,
U.K., 1998; Vol. 2, Chapter 43, p 2463.
(4) Becerra, R.; Frey, H. M.; Mason, B. P.; Walsh, R. Chem. Phys.
Lett. 1991, 185, 415.
∞
found that for their choice of Eo value (64.9 kJ mol-1) k1 is
1.3 × 10-9 cm3 molecule-1 s-1 at 294 K. This is in line with
their other modeling studies of SiH2 + CD3OD19 and SiH2 +
Me2O.21 The results from these studies have been rationalized
with models which produce very high rate constants and positive
activation energies at high pressures. The modeling produces a
crossover effect in which activation energies switch from
negative to positive at a certain pressure. This effect has never
been observed by us in any of the SiH2 systems we have studied,
many of which were much closer to the high-pressure limit than
(5) Becerra, R.; Walsh, R. Int. J. Chem. Kinet. 1994, 26, 45.
(6) Al-Rubaiey, N.; Walsh, R. J. Phys. Chem. 1994, 98, 5303.
(7) Becerra, R.; Frey, H. M.; Mason, B. P.; Walsh, R.; Gordon, M. S.
J. Chem. Soc., Faraday Trans. 1995, 91, 2723.
(8) Becerra, R.; Frey, H. M.; Mason, B. P.; Walsh, R. J. Organomet.
Chem. 1996, 521, 343.
(9) Al-Rubaiey, N.; Carpenter, I. W.; Walsh, R.; Becerra, R.; Gordon,
M. S. J. Phys. Chem. A 1998, 102, 8564.
(10) Becerra, R.; Boganov, S. E.; Walsh, R. J. Chem. Soc., Faraday
Trans. 1998, 94, 3569.
(11) Becerra, R.; Walsh, R. Int. J. Chem. Kinet. 1999, 31, 393.