Publication | Open Access
A study of secondary organic aerosol formation in the anthropogenic‐influenced southeastern United States
623
Citations
35
References
2007
Year
EngineeringAir Pollution MeasurementUrban Air QualityAir QualityEarth ScienceAir Pollution DispersionEnvironmental ChemistryAerosol TransportAtmospheric ScienceAerosol SamplingAir Quality MonitoringVehicle Emission TracersPollutant TransportSoutheastern United StatesChemical EmissionHazardous PollutantsHealth SciencesAerosol FormationSecondary Organic AerosolChemical ContaminantsAir Pollution
The study investigates secondary organic aerosol formation in the southeastern United States by comparing it with northeastern urban plumes. WSOC measurements of fine‑particle organic compounds were used to assess SOA. WSOC concentrations were correlated with vehicle tracers yet not directly emitted, and radiocarbon data show 70–80 % modern carbon, indicating that in northern Georgia SOA is primarily secondary from modern biogenic VOCs but strongly linked to anthropogenic sources, suggesting control strategies should target these sources.
The formation of secondary organic aerosol (SOA) in an anthropogenic‐influenced region in the southeastern United States is investigated by a comparison with urban plumes in the northeast. The analysis is based on measurements of fine‐particle organic compounds soluble in water (WSOC) as a measure of secondary organic aerosol. Aircraft measurements over a large area of northern Georgia, including the Atlanta metropolitan region, and in plumes from New York City and surrounding urban regions in the northeast show that fine‐particle WSOC are spatially correlated with vehicle emission tracers (e.g., CO), yet the measurements indicate that vehicles do not directly emit significant particulate WSOC. In addition to being correlated, WSOC concentrations were in similar proportions to anthropogenic tracers in both regions, despite biogenic volatile organic compounds (VOCs) that were on average 10–100 times higher over northern Georgia. In contrast, radiocarbon analysis on WSOC extracted from integrated filters deployed in Atlanta suggests that roughly 70–80% of the carbon in summertime WSOC is modern. If both findings are valid, the combined results indicate that in northern Georgia, fine‐particle WSOC was secondary and formed through a process that involves mainly modern biogenic VOCs but which is strongly linked to an anthropogenic component that may largely control the mass of SOA formed. Independent of the radiocarbon results, a strong association between SOA and anthropogenic sources has implications for control strategies in urban regions with large biogenic VOC emissions.
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