5988 J. Phys. Chem. A, Vol. 108, No. 28, 2004
Hasson et al.
The resultant methylglyoxal may then react with Cl atoms to
produce acetyl peroxy radicals which would then generate PAA,
MHP, and CO2 as discussed above
significant fraction of radicals are recycled in these reactions
(R8c). This may lead to higher concentrations of pollutants such
as OH radicals and ozone than is currently predicted by air
pollution models.
CH3C(O)CHO + Cl (+ O2) f
CH3C(O)O2 + CO + HCl (R25)
To investigate the potential impact of these reactions on
tropospheric ozone and OH concentrations, several simple box
model simulations were carried out using the OZIPR computer
program.34 In the first set of simulations, conditions typical of
a North American city during summer were chosen, and
concentrations of OH and ozone were monitored as the
branching ratios for reactions R8a and R8c were varied between
0 and 1. In these simulations, the branching ratios had a
negligible impact on the concentrations of these secondary
pollutants (typically less than 1%). In a second set of simula-
tions, the calculations were repeated but the NOx emission rates
were reduced by a factor of 10. With all of the RO2 + HO2
reactions set to YR8c ) 1, the peak OH radical concentration
increased from 3.3 × 106 molecules cm-3 to 4.7 × 106
molecules cm-3, while the change in the peak ozone concentra-
tion was small (<5%). Incorporating only the branching ratios
measured for acetyl and acetonyl peroxy radicals into the model
To investigate this possibility, simulations were carried out in
which branching ratios for R8a and R8d were set to 0.33 and
0.67, respectively (not shown). In these calculations the yields
of both MHP and PAA remained constant at about 0.08 as the
[CH3OH]0:[acetone]0 ratio was varied from 0 to 0.5. Because
the concentrations of methanol and acetone are high compared
to methylglyoxal during these experiments, Cl atoms predomi-
nantly react with methanol and acetone rather than methylgly-
oxal. Reaction R25 is thus too slow to generate the quantities
of MHP and PAA observed in the high [CH3OH]0 experiments,
and reaction R8d cannot account for the observed product
distributions. A significant branching ratio for R8c therefore
appears to be the best available explanation for the experimental
observations, although we cannot rule out a contribution from
R8d-ACN.
(iv) OH Radical Formation in the RO2 + HO2 Reactions.
From the discussion above, it is clear that the experimental data
are consistent with high yields of OH radicals in the reaction
between HO2 and acetyl peroxy radicals and in the reaction
between HO2 and acetonyl peroxy radicals. Given that the
relative rate constants for the reaction of acetone/methanol and
acetaldehyde/methanol are significantly different for OH- and
Cl-initiated reactions,31 the possibility was considered that
relative rate plots could be used as additional evidence for the
importance of reaction R8c in the high [CH3OH]0 experiments.
As the methanol concentration increases, the OH radical
concentration is also expected to increase, and thus a higher
fraction of methanol and the carbonyls will react with OH rather
than Cl in these experiments. The slope of the relative rate plots
would thus be expected to systematically change as the methanol
concentration is varied (see Figure 8 in ref 16). Experimental
relative rate plots do show a dependence on the methanol:
acetaldehyde ratio, but it is difficult to quantitatively assign this
to the occurrence of reaction 8c. This apparent discrepancy can
be explained by examining the Acuchem simulations described
above. In these simulations, it is apparent that OH formation
from the Cl-atom-initiated oxidation of hydroperoxides (e.g.,
reactions R19 and 20) is a larger OH source than reaction R8c,
and relative rate plots thus cannot easily be used as indirect
evidence for reaction channel R8c in these experiments. For
acetone, the product yields do not vary between [CH3OH]0/
[acetone]0 values of 0.1 and 0.5, indicating that even in the low
[CH3OH]0 experiments, acetonyl peroxy radicals reacted pre-
dominantly with HO2. The change in the slope of the relative
rate plots as the methanol concentration increases is thus
expected to be minimal, and the analysis could not be performed.
Furthermore, the large difference in relative rates for acetone
and methanol precludes an accurate measurement of this ratio.
(and with all other RO2 + HO2 branching ratios set to YR8a
)
1) had a much smaller impact on both ozone (<1%) and OH
(<5%). This result is not surprising since oxygenated organics
make up only a small fraction of total VOC emissions in these
simulations.
From the simulations described here, it appears that chain
propagation in RO2 + HO2 reactions (R8c) may have a small
impact on tropospheric chemistry under low NOx conditions.
The impact of these reactions on OH radical concentrations will
be greater for aged air, which typically contains higher
concentrations of oxygenated organics and lower levels of NOx.
To predict the extent of this impact, a more detailed database
of RO2 + HO2 branching ratios is needed. Finally, reaction 8
will not provide as strong an atmospheric source of acetic acid
as previously thought. Further investigations of the product
yields from these reactions as a function of temperature are
clearly required.
Acknowledgment. The authors thank Tim Wallington and
Mike Hurley for supplying spectra of peroxides. A.S.H. thanks
NCAR’s Atmospheric Chemistry Division for the award of a
Visiting Fellowship that enabled this work to be performed.
A.S.H. also thanks the donors of the Petroleum Research Fund
(American Chemical Society #37996-GB6) for financial support.
The National Center for Atmospheric Research is operated by
the University Corporation for Atmospheric Research, under
the sponsorship of the National Science Foundation. This work
was supported in part by a grant from the NASA Upper
Atmosphere Research Program.
References and Notes
(1) Finlayson-Pitts, B. J.; Pitts, J. N. Chemistry of the Upper and Lower
Atmosphere; Academic Press: San Diego, CA, 2000.
(2) Atkinson, R. Gas-Phase Tropospheric Chemistry of Volatile Organic
Compounds: 1. Alkanes and Alkenes. J. Phys. Chem. Ref. Data 1997, 26(2),
215.
Atmospheric Implications
(3) Wallington, T. J.; Japar, S. M. Reaction of CH3O2 + HO2 in Air
at 295 K: A Product Study. Chem. Phys. Lett. 1990, 167, 513-518.
(4) Wallington, T. J.; Japar, S. M. FTIR Product Study of the Reaction
of C2H5O2 + HO2 in Air at 295 K. Chem. Phys. Lett. 1990, 166, 495-
499.
(5) Lightfoot, P. D.; Roussel, P.; Caralp, F.; Lesclaux, R. Flash
Photolysis Study of the CH3O2 + CH3O2 and CH3O2 + HO2 Reactions
between 600 and 719 K: Unimolecular Decomposition of Methylhydro-
peroxide. J. Chem. Soc,. Faraday Trans. 1991, 87, 3213-3220.
As described in the Introduction, RO2 + HO2 reactions are
important chain termination processes that moderate the con-
centrations of radical species and ozone in the lower atmosphere.
In this work, evidence has been presented indicating that organic
peroxy radicals containing a carbonyl group at the R-position
(CH3C(O)O2) or â-position (CH3C(O)CH2O2) do not exclusively
react with HO2 to form a hydroperoxide (R8a) and that a