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Characterization of aerosol associated with enhanced small particle of number concentrations in a suburban forested environment
被引:8
|作者:
Ziemba, L. D.
[1
]
Griffin, R. J.
[1
]
Cottrell, L. D.
[1
]
Beckman, P. J.
[1
]
Zhang, Q.
[2
,3
]
Varner, R. K.
[1
,4
]
Sive, B. C.
[1
]
Mao, H.
[1
]
Talbot, R. W.
[1
]
机构:
[1] Univ New Hampshire, Climate Change Res Ctr, Durham, NH 03824 USA
[2] SUNY Albany, Atmospher Sci Res Ctr, Albany, NY 12222 USA
[3] Univ Calif Davis, Dept Environm Toxicol, Davis, CA 95616 USA
[4] Univ New Hampshire, Complex Syst Res Ctr, Durham, NH 03824 USA
基金:
美国国家环境保护局;
关键词:
SECONDARY ORGANIC AEROSOL;
MASS-SPECTROMETER;
CONTROLLED DIMENSIONS;
BACKGROUND AEROSOL;
AERODYNAMIC LENSES;
NOZZLE EXPANSIONS;
LOBLOLLY-PINE;
GROWTH EVENTS;
UNITED-STATES;
SIZE;
D O I:
10.1029/2009JD012614
中图分类号:
P4 [大气科学(气象学)];
学科分类号:
0706 ;
070601 ;
摘要:
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 CO2 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 (sigma), 1.6 +/- 1.9, 0.1 +/- 0.1, and 0.4 +/- 0.4 mu g 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.
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