Environmental Science & Technology · 2010 · 134 citations · 37 references
Natural SciencesChemistryAtmospheric ChemistryAtmospheric ScienceSpectroscopyAerosol ChemistryAerosol ScienceAtmospheric CompositionMass SpectrometrySecondary Aerosol FormationSecondary Organic AerosolsAerosol Chemical CompositionAtmospheric Aerosol ChemistryLight AbsorptionMethylglyoxal FormationOrganic Aerosol ChemistryOrganic Aerosol CompositionOrganic AerosolsSecondary Organic Aerosol Formation
Glyoxal (G) and methylglyoxal (MG) are potentially important secondary organic aerosol (SOA) precursors. Previous studies of SOA formation by G and MG have focused on either species separately; however, G and MG typically coexist in the atmosphere. We studied the formation of secondary organic material in aqueous aerosol mimic mixtures containing G and MG with ammonium sulfate. We characterized the formation of light-absorbing products using UV-vis spectrophotometry. We found that absorption at 280 nm can be described well using models for the formation of light-absorbing products by G and MG in parallel. Pendant drop tensiometry measurements showed that surface tension depression by G and MG in these solutions can be modeled as a linear combination of the effects of G and MG alone. Product species were identified using chemical ionization mass spectrometry with a volatilization flow tube inlet (Aerosol CIMS). Peaks consistent with G-MG cross-reaction products were observed, accounting for a significant fraction of detected product mass, but most peaks could be attributed to self-reaction. We conclude that cross-reactions contribute to SOA mass from uptake of G and MG, but they are not required to accurately model the effects of this process on aerosol surface tension or light absorption.
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Physical chemistry of surfaces
Choice Reviews Online · 1998 · 11.7K citations
Identification of Polymers as Major Components of Atmospheric Organic Aerosols
Markus Kalberer, D. Paulsen, M. Sax et al. · Science · 2004 · 1.2K citations