Two elevated particle number/mass growth events associated with Aitken-mode particles were observed during a sampling campaign (13-29 September 2004) at the Duke University Free-Air CO 2 Enrichment facility, a forested field site located in suburban central North Carolina. Aerosol growth rates between 1.2 and 4.9 nm hr -1 were observed, resulting in net increases in geometric mean diameter of 21 and 37 nm during events. Growth was dominated by addition of oxidized organic compounds. Campaign-average aerosol mass concentrations measured by an Aerodyne quadrupole aerosol mass spectrometer (Q-AMS) were 1.9 ± 1.6 (s), 1.6 ± 1.9, 0.1 ± 0.1, and 0.4 ± 0.4 mg m-3 for organic mass (OM), sulfate, nitrate, and ammonium, respectively. These values represent 47%, 40%, 3%, and 10%, respectively, of the measured submicron aerosol mass. Based on Q-AMS spectra, OM was apportioned to hydrocarbon-like organic aerosol (HOA, likely representing primary organic aerosol) and two types of oxidized organic aerosol (OOA-1 and OOA-2), which constituted on average 6%, 58%, and 36%, respectively, of the apportioned OM. OOA-1 probably represents aged, regional secondary organic aerosol (SOA), while OOA-2 likely reflects less aged SOA. Organic aerosol characteristics associated with the events are compared to the campaign averages. Particularly in one event, the contribution of OOA-2 to overall OM levels was enhanced, indicating the likelihood of less aged SOA formation. Statistical analyses investigate the relationships between HOA, OOA-1, OOA-2, other aerosol components, gas-phase species, and meteorological data during the campaign and individual events. No single variable clearly controls the occurrence of a particle growth event. Copyright 2010 by the American Geophysical Union.
CITATION STYLE
Ziemba, L. D., Griffin, R. J., Cottrell, L. D., Beckman, P. J., Zhang, Q., Varner, R. K., … Talbot, R. W. (2010). Characterization of aerosol associated with enhanced small particle number concentrations in a suburban forested environment. Journal of Geophysical Research Atmospheres, 115(12). https://doi.org/10.1029/2009JD012614
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