Radical Product Channel of CH3OCH2O2 + HO2
J. Phys. Chem. A, Vol. 114, No. 1, 2010 415
Simulations of all the experiments indicated that they were
well described using a value of k2c/k2 ) 0.19 ( 0.03, with these
uncertainty limits representing statistical errors alone. This was
based on a global fit to the experiments illustrated in Figure 7,
which are those in which high benzene concentrations (≈1 Torr)
were used. The results clearly indicate that the observed phenol
formation, particularly at low reagent conversions, cannot be
accounted for without the participation of the radical-propagating
channel, reaction 2c. The consistent performance of the mech-
anism across the complete range of [CH3OH]0/[CH3OCH3]0 also
confirms that the competition between reactions 2 and 17 for
CH3OCH2O2 is adequately described by the parameters applied.
This provides support for the relative production rates simulated
for CH3OCH2O2 and HO2, and for the rate coefficients applied
to reactions 2 and 17. Whereas k17 was measured directly in
our previous study,20 the applied value of k2 (1 × 10-11 cm3
molecule-1 s-1) is based on that inferred previously from the
relative steady state concentrations of CH3OCH2O2 and HO2
observed in molecular modulation experiments.20 On the basis
of this analysis, we report a value of k2c/k2 ) 0.19 ( 0.08, where
the error limits include a 25% contribution from possible
systematic errors in the above analysis. This figure is based on
an appraisal of the sensitivity of the system to varying the key
rate coefficients in Table 2 over realistic uncertainty ranges,
and includes uncertainties associated with the yield of phenol
from the OH-initiated oxidation of benzene.
Figure 7 also shows the results of simulations in which k2c/
k2 was set to values of 0.4 and zero. The latter case demonstrates
the contribution from other sources of OH in the system. These
are most notable at high [CH3OH]0/[CH3OCH3]0, where sub-
stantial secondary OH production results from the chemistry
of HOCH2O2 formed from the reaction of HO2 with HCHO, as
indicated above and characterized previously.11 In the absence
of CH3OH (i.e., [CH3OH]0/[CH3OCH3]0 ) 0), significant
formation of HCHO does not occur and the observed formation
of phenol is dominated throughout by the production of OH
via reaction 2c, which is simulated to account for 73% of the
integrated OH produced for a CH3OCH3 depletion of 5 mTorr
(i.e., about 20% depletion). The residual production of OH under
these conditions is partially accounted for by the secondary
removal of CH3OCH2OOH, as follows,
[CH3OCH3]0. The formation of CH3OCH2OOH and CH3OCHO
actually observed in the present experiments with [CH3OH]0/
[CH3OCH3]0 ≈ 15 was also used to provide optimized values
of k2a/k2 and (k2b + k2c)/k2. For this procedure, k2c/k2 was fixed
at a value of 0.19 on the basis of the results of the phenol
analysis above, and compensating changes were made to the
branching ratio not being optimized (i.e., k2b/k2 when optimizing
k2a/k2, and vice versa) to account for the balance of the reaction.
This provided optimized values of k2a/k2 ) 0.55 ( 0.05 and
(k2b + k2c)/k2 ) 0.39 ( 0.04. This analysis also confirmed that
the modest variations applied to k2a/k2 and k2b/k2 during this
procedure had a negligible impact on simulated formation of
phenol. After inclusion of 5% and 10% uncertainties associated
with the quantification of CH3OCHO and CH3OCH2OOH,19 this
leads to values of k2a/k2 ) 0.55 ( 0.08 and (k2b + k2c)/k2 )
0.39 ( 0.05. These branching ratios are therefore consistent
with channels 2a-2c accounting for the entire reaction, within
experimental uncertainties.
4. Conclusions and Atmospheric Implications
The results presented above provide further evidence that the
reactions of HO2 with selected oxygenated RO2 radicals proceed
partially via radical-propagating channels, thereby lessening their
perceived impact as chain terminating processes in the atmo-
sphere. The existence of such channels has previously been
reported for the reactions of HO2 with examples of acyl
8,11,13
(CH3C(O)O2
CH2O2
and C6H5C(O)O213), R-carbonyl (CH3C(O)-
and RO2 radicals produced from C2H5C(O)CH313),
12,13
and R-hydroxy (HOCH2O211) peroxy radicals. The present work
adds the simplest R-alkoxy peroxy radical, CH3OCH2O2, to this
list. It therefore appears that a channel producing OH radicals
exists for the reactions of HO2 with peroxy radicals containing
a number of oxygenated substitutions of atmospheric signifi-
cance. As indicated in section 1, it has been recognized recently
that such reactions probably make a contribution to the
unexpectedly high HOx concentrations observed in locations
where reaction with HO2 radicals is believed to be an important
fate of organic peroxy radicals.14-16 A precise estimation of this
contribution awaits a more detailed understanding of the factors
which influence organic oxidation chemistry under low NOx
conditions. Further experimental and theoretical work in this
area is needed.
Cl + CH3OCH2OOH f CH3OCHOOH + HCl
(18)
References and Notes
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667.
CH3OCHOOH f CH3OCHO + OH
(19)
(2) Lightfoot, P. D.; Cox, R. A.; Crowley, J. N.; Destriau, M.; Hayman,
G. D.; Jenkin, M. E.; Moortgat, G. K.; Zabel, F. Atmos. EnViron. 1992,
26A, 1805.
(3) Tyndall, G. S.; Cox, R. A.; Granier, C.; Lesclaux, R.; Moortgat,
G. K.; Pilling, M. J.; Ravishankara, A. R.; Wallington, T. J. J. Geophys.
Res. D 2001, 106, 12157.
which is simulated to account for about 15% of the integrated
OH produced. The remaining 12% is due to direct formation
from the minor channel of the reaction of CH3OCH2 with O2:
(4) Jenkin, M. E.; Clemitshaw, K. C. Atmos. EnViron. 2000, 34, 2499.
(5) Wallington, T. J. J. Chem. Soc., Faraday Trans. 1991, 87, 2379.
(6) Spittler, M.; Barnes, I.; Becker, K. H.; Wallington, T. J. Chem.
Phys. Lett. 2000, 321, 57.
CH3OCH2 + O2 f HCHO + HCHO + OH (8b)
(7) Elrod, M. J.; Ranschaert, D. L.; Schneider, N. J. Int. J. Chem. Kinet.
2001, 33, 363.
(8) Hasson, A. S.; Tyndall, G. S.; Orlando, J. J. J. Phys. Chem. A 2004,
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(9) Ravento´s-Duran, M. T.; Percival, C. J.; McGillen, M. R.; Hamer,
P. D.; Shallcross, D. E. Phys. Chem. Chem. Phys. 2007, 9, 4338.
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This accounts for 1.4% of this reaction at 700 Torr, based on
the parameters derived by Sehested et al.27 Support for this level
of contribution was provided by the observed formation of trace
amounts of HCHO, which agreed well with those simulated.
For the above analysis, the balance of reaction 2 was divided
between channels 2a and 2b, with branching ratios k2a/k2 ) 0.6
and k2b/k2 ) (0.4 - k2c/k2). These ratios correspond to respective
yields of CH3OCH2OOH and CH3OCHO of 0.6 and 0.4 from
reaction 2, which are broadly consistent with those reported
above, and previously,19 for experiments at high [CH3OH]0/
(12) Jenkin, M. E.; Hurley, M. D.; Wallington, T. J. Phys. Chem. Chem.
Phys. 2008, 10, 4274.
(13) Dillon, T. J.; Crowley, J. N. Atmos. Chem. Phys. 2008, 8, 4877.