4994 J. Phys. Chem. A, Vol. 101, No. 27, 1997
Lindholm and Hershberger
approaches in ref 25 and this work. There are two possible
explanations for this discrepancy. One is that the experiments
of ref 25 were performed at a total pressure of ∼30 Torr, while
our data are at ∼2 Torr pressure. It is possible that the
branching ratio depends on pressure, although this would be
quite surprising, since the total rate constant displays no pressure
dependence.15,24 Another difference between their study and
ours lies in the radical densities employed. Meunier et al. quote
[F]0 ) 5.7 × 1014 molecules/cm3, in contrast to our typical [CN]0
of ∼(2-4) × 1013. At such high densities, we believe that the
reaction
experiments. Obviously, additional experiments are necessary
to resolve this issue.
Conclusions
The branching ratios of the NH2 + NO2 reaction were
measured by infrared detection of products. The most important
result of this study is that we believe it represents the first
reliable estimate of the contribution of the major NO formation
channel. This study also confirms earlier reports that N2O +
H2O formation represents only a minor channel, although the
measured value of the contribution of this channel is somewhat
greater than that obtained in our previous determination.
F + NH2 f HF + NH
(8)
Acknowledgment. The authors thank J. Park and M. C. Lin
of Emory University for valuable discussions and for making a
manuscript available prior to publication. This work was
supported by the Division of Chemical Sciences, Office of Basic
Energy Sciences of the Department of Energy, Grants DE-FG06-
93ER14390 and DE-FG03-96ER14645). Acknowledgment is
also made to the donors of the Petroleum Research Fund,
administered by the American Chemical Society, for partial
support of this work.
is significant in their experiments and cannot be ignored. No
direct measurements of the rate constant for this reaction have
been reported, although Fagerstroem et al. inferred k8 ) 1.16
× 10-10 cm3 molecule-1 s-1 by fitting a kinetic model to
experimental data38 and Donaldson et al. performed energy
disposal experiments on the HF products of this reaction.39 It
seems quite likely, in any case, that this reaction proceeds much
faster than F + NH3 (although we note that there is significant
disagreement in the literature regarding the F + NH3 rate
constant).40-42 Since the [NO2]/[F]0 ratio in the experiments
of ref 25 was only about 10, reaction 8 may be able to compete
with the title reaction for NH2 radicals. The NH + NO2 reaction
has been previously estimated in our laboratory to produce N2O
+ OH in 41% yield.32 The reaction F + NH f N + HF may
further complicate this system. It is therefore quite possible
that much of the N2O observed in the experiments of ref 25
was due to the NH + NO2 and possibly N + NO2 reactions.
Simple kinetic modeling calculations on their system suggest
that N2O formation from these secondary reactions can be
significant, although the detailed comparisons depend on the
values of the rate constants used as well as initial reagent
concentrations.
References and Notes
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One significant source of uncertainty in all measurements of
φ1b is the fate of the H2NO radicals. We are not aware of any
direct kinetic measurements of this species, although Bulatov
et al. estimated k ) 2.0 × 10-14 cm3 molecule-1 s-1 for the
H2NO + O3 reaction from kinetic modeling of NH3/O3 flash
photolysis data.43 This suggests that H2NO + NO2 is also very
slow and probably not a source of additional NO in our