Articles | Volume 9, issue 14
Atmos. Chem. Phys., 9, 5093–5105, 2009
https://doi.org/10.5194/acp-9-5093-2009
Atmos. Chem. Phys., 9, 5093–5105, 2009
https://doi.org/10.5194/acp-9-5093-2009

  28 Jul 2009

28 Jul 2009

In-cloud processes of methacrolein under simulated conditions – Part 1: Aqueous phase photooxidation

Yao Liu1, I. El Haddad1, M. Scarfogliero2, L. Nieto-Gligorovski1, B. Temime-Roussel1, E. Quivet1, N. Marchand1, B. Picquet-Varrault2, and A. Monod1 Yao Liu et al.
  • 1Universités d'Aix-Marseille I, II et III – CNRS, UMR 6264, Laboratoire Chimie Provence, Equipe: IRA, 3 place Victor Hugo, 13331 Marseilles Cedex 3, France
  • 2Laboratoire Interuniversitaire des Systèmes Atmosphériques (UMR 7583), Université Paris, France

Abstract. The photooxidation of methacrolein was studied in the aqueous phase under simulated cloud droplet conditions. The obtained rate constant of OH-oxidation of methacrolein at 6°C in unbuffered solutions was 5.8(±0.9)×109 M−1 s−1. The measured rate coefficient is consistent with OH-addition on the C=C bond. This was confirmed by the mechanism established on the study of the reaction products (at 25°C in unbuffered solutions) where methylglyoxal, formaldehyde, hydroxyacetone and acetic acid/acetate were the main reaction products. An upper limit for the total carbon yield was estimated to range from 53 to 85%, indicating that some reaction products remain unidentified. A possible source of this mismatch is the formation of higher molecular weight compounds as primary reaction products which are presented in El Haddad et al. (2009) and Michaud et al. (2009).

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