Rate Constant for the HO2 + NO Reaction
J. Phys. Chem., Vol. 100, No. 10, 1996 4031
cessfully coupled to turbulent flow tube systems for chemical
kinetic studies at relatively high pressures and low temperatures,
that is, under conditions outside the operating range of the well-
established conventional fast flow technique.
Acknowledgment. The research described in this article was
supported by a grant from the NASA Upper Atmospheric
Research Program to the Massachusetts Institute of Technology.
References and Notes
(1) Wennberg, P. O.; Cohen, R. C.; Stimpfle, R. M.; Koplow, J. P.;
Anderson, J. G.; Salawitch, R. D.; Fahey, D. W.; Woodbridge, E. L.; Keim,
E. R.; Gao, R. S.; Webster, C. R.; May, R. D.; Toohey, D. W.; Avallone,
L. M.; Proffitt, M. H.; Lowenstein, M.; Podolske, J. R.; Chan, K. R.; Wofsy,
S. C. Science 1994, 266, 398.
(2) Cohen, R. C.; Wennberg, P. O.; Stimpfle, R. M.; Koplow, J. P.;
Anderson, J. G.; Fahey, D. W.; Woodbridge, E. L.; Keim, E. R.; Gao, R.
S.; Proffitt, M. H.; Lowenstein, M.; Chan, K. R. Geophys. Res. Lett. 1994,
2
1, 2539.
(3) Howard, C. J.; Evenson, K. M. Geophys. Res. Lett. 1977, 4, 437.
Figure 7. Arrhenius plot for the reaction HO
2
+ NO. The open circles
(4) Cheng, B. M.; Lee, J. W.; Lee, Y. P. J. Phys. Chem. 1991, 95,
are experimental data from this work, and the line is the resulting
2814.
(5) Burkholder, J. B.; Hammer, P. D.; Howard, C. J. J. Phys. Chem.
987, 91, 2136.
6) Seeley, J. V.; Jayne, J. T.; Molina, M. J. Int. J. Chem. Kinet. 1993,
5, 571.
(7) Seeley, J. V.; Jayne, J. T.; Molina, M. J. Submitted for publication.
(8) Harrison, A. G. Chemical Ionization Mass Spectrometry, 2nd ed.,
CRC Press: Boca Raton, FL, 1992.
9) Streit, G. E. J. Chem. Phys. 1982, 77, 826.
10) Lovejoy, E. R.; Murrells, T. P.; Ravishankara, A. R.; Howard, C.
J. J. Phys. Chem. 1990, 94, 2386.
1
3
Arrhenius fit. The data of Howard are represented by filled circles.
1
(
thorough temperature dependence study for T < 300 K; a
comparison of his results with the results of this study is also
shown in Figure 7. Given the close agreement between
Howard’s low pressure results and our higher pressure values,
we conclude that the rate constant does not have a significant
pressure dependence for temperatures between 200 and 300 K.
If Howard’s data set is combined with our data set, an Arrhenius
2
(
(
(
(
(
11) Fehsenfeld, F. C.; Ferguson, E. E. J. Chem. Phys. 1974, 61, 3181.
12) Leu, M. T. J. Chem. Phys. 1979, 70, 1662.
13) Howard, C. J. J. Chem. Phys. 1979, 71, 2352.
(14) Jemi-Alade, A. A.; Thrush, B. A. J. Chem. Soc., Faraday Trans.
990, 86, 3355.
15) Abbatt, J. P. D.; Demerjian, K. L.; Anderson, J. G. J. Phys. Chem.
990, 94, 4566.
16) Eisele, F. L.; Tanner, D. J. J. Geophys. Res. 1991, 96, 9295.
(17) (a) Seeley, J. V.; Molina, M. J. Manuscript in preparation for
submission to Int. J. Chem. Kinet. (b) Seeley, J. V. Experimental Studies
of Gas Phase Radical Reactions Using the Turbulent Flow Tube Technique,
Ph.D. Thesis, MIT, 1994.
-
12
3
expression of (2.67 ( 0.31) × 10
exp[(316 ( 30)/T] cm
molecule-
1
s
-1
is obtained.
1
1
The negative temperature dependency for the rate constant
for reaction 1 indicates that the reaction proceeds through the
formation of an intermediate; the absence of a measurable
pressure dependency points out that such an intermediate is too
short-lived to be affected by collisions with the carrier gas. The
magnitude of a possible pressure effect is expected to increase
as the temperature is lowered; however, we see no evidence
for such an effect down to 200 K. It is also possible that species
such as water vapor or oxygen give rise to a pressure effect
which is larger than that due to nitrogen, as is the case, for
example, with the HO2 self-reaction.26 Additional studies of
such pressure effects would be useful.
(
(
(18) Chang, J. S.; Kaufmann, F. J. Phys. Chem. 1978, 82, 1683.
19) Previously, we have reported that in turbulent flow conditions the
(
plug flow approximation yields rate constants which are approximately 12%
6,7,17
less than the actual value.
In these cases the greater predicted deviation
was a result of using a detection technique (resonance fluorescence) which
preferentially samples the faster moving central portion of the flow tube
cross section.
(
20) Margitan, J. J.; Anderson, J. G. Results presented at 13th Informal
Conference on Photochemistry, Clearwater Beach, FL, 1978.
(21) Kaufman, F.; Reimann, B. Results presented at 13th Informal
Conference on Photochemistry, Clearwater Beach, FL, 1978.
Conclusions
Our data indicate that reaction 1 does not have a substantial
pressure dependence at temperatures between 200 and 300 K.
Our results are in excellent agreement with previous results
obtained in low-pressure discharge flow systems. This work
also shows that key radical species, such as HO2 and OH, can
be monitored using chemical ionization mass spectrometry with
greater sensitivity than that provided by conventional electron
impact mass spectrometers; work in progress in our laboratory
also indicates that many stable species can be monitored as well
with superb sensitivity. Furthermore, our results show that high-
pressure chemical ionization mass spectrometry can be suc-
(
22) Glaschick-Schimpf, I.; Leiss, A.; Monkhouse, P. B.; Schurath, U.;
Becker, K. H.; Fink, E. H. Chem. Phys. Lett. 1979, 67, 318.
23) Hack, W.; Preuss, W.; Temps, F.; Wagner, H. G. G. Int. J. Chem.
Kinet. 1980, 12, 850.
24) Thrush, B. A.; Wilkinson, J. P. T. Chem. Phys. Lett. 1981, 81, 1.
(
(
(25) Jemi-Alade, A. A.; Thrush, B. A. J. Chem. Soc., Faraday Trans.
990, 86, 3355.
1
(26) DeMore, W. B.; Sander, S. P.; Howard, C. J.; Ravishankara, A.
R.; Golden, D. M; Kolb, C. E.; Hampson, R. F.; Kurylo, M. J.; Molina, M.
J. Chemical Kinetics and Photochemical Data for Use in Stratospheric
Modeling; JPL Publication 94-26; Jet Propulsion Laboratory: Pasadena,
CA, 1994.
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