Secondary organic aerosol formation during the photooxidation of toluene:: NOx dependence of chemical composition

The photooxidation of toluene is a potential source of secondary organic aerosol (SOA) in urban air, but only a small portion of the compounds present in SOA have been identified. In this study, we analyzed the chemical compositions of SOA produced by photoirradiation of the toluene/NOx/air system in laboratory chamber experiments by a combination of liquid chromatography -mass spectrometry, hybrid high-performance liquid chromatography -mass spectrometry, and iodometry-spectrophotometry. The dependence of the chemical composition on the initial NO, concentration was examined at initial NO concentrations ([NO](0)) of 0.2 and 1 ppmv. Fifteen semivolatile products, including aromatic and ring-cleavage compounds, were quantified. However, the quantified products comprised only a small portion (similar to 1 wt %) of the total aerosol mass. The total SOA yield (similar to 13 wt %), the ratio of organic peroxides to total SOA mass (similar to 17 wt %), and the density of SOA (similar to 1.4 g cm(-3)) were independent of the NOx level, suggesting that the reaction mechanisms of the formation of major SOA products at [NO](0) = 0.2 and 1 ppmv are essentially the same. The negative-ion mass spectra of SOA samples showed that ion signals attributed to hemiacetal oligomers and/or decomposition products of peroxy hemiacetal oligomers were detected in the range of mass-to-charge ratios (m/z) between 200 and 500. The highest signals were detected at m/z = 155 and 177, and these were tentatively assigned to C-7 unsaturated oxacyclic oxocarboxylic acids and C-7 unsaturated oxacyclic dicarboxylic acids, respectively. We conclude that the major chemical components of the aerosol are hemiacetal and peroxy herniacetal oligomers and low-molecular-weight dicarboxylic acids.