V.F. Andersen et al. / Chemical Physics Letters 472 (2009) 23–29
29
the peak from NO2 decreased. This is illustrated in the residual
Acknowledgements
spectra in Fig. 5. One of the primary products could be CH3C(O)O-
CH2ONO2 formed from addition of NO to peroxyl radicals [12]. The
yield of acetic acid and acetic formic anhydride in the experiments
performed in the presence of NO do not change over the range of
O2 concentrations used (206 to 980 mbar), which is consistent with
the work of Christensen et al. [12].
The authors thank the Copenhagen Center for Atmospheric Re-
search, sponsored by the Danish Natural Science Research Council
and the Villum Kann Rasmussen Fund, for its generous support.
Furthermore, we thank Dr. Timothy Wallington and the reviewers
for helpful advice.
6. Implications for atmospheric chemistry
Appendix A. Supplementary material
The degradation of methyl esters in the atmosphere is primarily
initiated by hydroxyl radicals because of the combination of high
reactivity with the concentration of this radical. Reaction with
NO3 as well as photolytic breakdown are additional possible re-
moval processes for methyl acetate. These processes have been
studied by Langer et al. and Benayada et al., and both were found
to be negligible compared to reaction with OH [24,25]. Atmo-
spheric lifetimes of the esters can, therefore, be determined from
their reaction rates with the hydroxyl radical. From the rate con-
stants determined in this study and an OH concentration of
1 ꢀ 106 molecule cmꢁ3, the following lifetime is expected for
methyl acetate:
Supplementary data associated with this article can be found, in
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