Secondary organic aerosol (SOA) is generated in an environmental chamber by the ozonolysis of a monoterpene precursor (typically alpha-pinene or limonene) in the presence of an OH radical scavenger. The particle mass and number distributions are measured with an SMPS, and organic concentrations are monitored using PTR-MS. Species identified with PTR-MS are consistent with results from filter-based measurements, and include limononaldehyde, 7-hydroxy-limononaldehyde, and 7-hydroxy-keto-limononaldehyde from limonene ozonolysis, and pinonaldeyhde, norpinonaldehyde, norpinonic acid, and pinonic acid from alpha-pinene ozonolysis.
Additionally, PTR-MS allows us to investigate the differences between dark chamber experiments conducted in the absence of NOx with experiments conducted in high-NOx environments or in the presence of UV light. We have previously observed that the gas-phase conditions (i.e., NOx concentration) can significantly affect SOA yield. Filter-based measurements allow little insight into the underlying gas-phase chemistry that controls SOA yield. The higher time resolution (and low detection limit) of the PTR-MS allows for the investigation of changes in organic speciation both during and after terpene consumption.
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