Atmos. Chem. Phys. Discuss., 9, 22993-23020, 2009
www.atmos-chem-phys-discuss.net/9/22993/2009/
doi:10.5194/acpd-9-22993-2009
© Author(s) 2009. This work is distributed
under the Creative Commons Attribution 3.0 License.
Review Status
This discussion paper has been under review for the journal Atmospheric Chemistry and Physics (ACP). Please refer to the corresponding final paper in ACP.
Characterization of non-photochemically formed oligomers from methylglyoxal: a pathway to produce secondary organic aerosol through cloud processing during night-time
F. Yasmeen1,2, N. Sauret1, J. F. Gal1, P.-C. Maria1, L. Massi3, W. Maenhaut4, and M. Claeys2
1Laboratoire de Radiochimie Sciences Analytique et Environnement, Institut de Chimie de Nice (CNRS, FR 3037), University of Nice Sophia-Antipolis, Faculty des Sciences, Parc Valrose, 06108 Nice Cedex 2, France
2Department of Pharmaceutical Sciences, University of Antwerp (Campus Drie Eiken), Universiteitsplein 1, 2610 Antwerp, Belgium
3Plate-forme Technologique-Spectrométrie de Masse, Institut de Chimie de Nice, Université de Nice Sophia-Antipolis, Parc Valrose, 06108 Nice Cedex 2, France
4Department of Analytical Chemistry, Institute for Nuclear Sciences, Ghent University, Proeftuinstraat 86, 9000 Gent, Belgium

Abstract. Aqueous-phase oligomer formation from methylglyoxal, a major atmospheric photooxidation product, has been investigated in a simulated cloud matrix under dark conditions. The aim of this study was to explore an additional path producing secondary organic aerosol (SOA) through cloud processes without photochemistry during night-time. Indeed, atmospheric models still underestimate SOA formation, as field measurements have revealed more SOA than predicted. Soluble oligomers (n=1–8) formed in the course of acid-catalyzed aldol condensation and acid-catalyzed hydration followed by acetal formation have been detected and characterized by positive and negative ion electrospray ionization mass spectrometry. Aldol condensation proved to be a favorable mechanism under simulated cloud conditions, while hydration/acetal formation was found to strongly depend on the pH of the system. The aldol oligomer series starts with a β-hydroxy ketone via aldol condensation, where oligomers are formed by multiple additions of C3H4O2 units (72 Da) to the parent β-hydroxy ketone. Ion trap mass spectrometry experiments were performed to structurally characterize the major oligomer species. A mechanistic pathway for the growth of oligomers under cloud conditions and in the absence of UV-light and OH radicals, which could substantially enhance in-cloud SOA yields, is proposed here for the first time.

Citation: Yasmeen, F., Sauret, N., Gal, J. F., Maria, P.-C., Massi, L., Maenhaut, W., and Claeys, M.: Characterization of non-photochemically formed oligomers from methylglyoxal: a pathway to produce secondary organic aerosol through cloud processing during night-time, Atmos. Chem. Phys. Discuss., 9, 22993-23020, doi:10.5194/acpd-9-22993-2009, 2009.
 
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