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Source apportionment of wintertime secondary organic aerosol during the California regional PM10/PM2.5 air quality study
被引:42
|作者:
Chen, Jianjun
[1
]
Ying, Qi
[2
]
Kleeman, Michael J.
[1
]
机构:
[1] Univ Calif Davis, Dept Civil & Environm Engn, Davis, CA 95616 USA
[2] Texas A&M Univ, Zachry Dept Civil Engn, College Stn, TX 77843 USA
基金:
美国国家环境保护局;
关键词:
CACM;
CRPAQS;
Secondary organic aerosol;
Source apportionment;
UCD/CIT air quality model;
POLLUTION SOURCES;
PARTICULATE MATTER;
EMISSIONS;
MODEL;
SCALE;
MECHANISM;
GASOLINE;
WIND;
C-1;
D O I:
10.1016/j.atmosenv.2009.07.010
中图分类号:
X [环境科学、安全科学];
学科分类号:
08 ;
0830 ;
摘要:
The UCD/CIT air quality model with the Caltech Atmospheric Chemistry Mechanism (CACM) was used to predict source contributions to secondary organic aerosol (SOA) formation in the San Joaquin Valley (SJV) from December 15, 2000 to January 7, 2001. The predicted 24-day average SOA concentration had a maximum value of 4.26 mu g m(-3) 50 km southwest of Fresno. Predicted SOA concentrations at Fresno, Angiola, and Bakersfield were 2.46 mu g m(-3), 1.68 mu g m(-3), and 2.28 mu g m(-3), respectively, accounting for 6%, 37%, and 4% of the total predicted organic aerosol. The average SOA concentration across the entire SJV was 1.35 mu g m(-3), which accounts for approximately 20% of the total predicted organic aerosol. Averaged over the entire SJV, the major SOA sources were solvent use (28% of SOA), catalyst gasoline engines (25% of SOA), wood smoke (16% of SOA), non-catalyst gasoline engines (13% of SOA), and other anthropogenic sources (11% of SOA). Diesel engines were predicted to only account for approximately 2% of the total SOA formation in the SJV because they emit a small amount of volatile organic compounds relative to other sources. In terms of SOA precursors within the SJV, long-chain alkanes were predicted to be the largest SOA contributor, followed by aromatic compounds. The current study identifies the major known contributors to the SOA burden during a winter pollution episode in the SJV, with further enhancements possible as additional formation pathways are discovered. (C) 2009 Elsevier Ltd. All rights reserved.
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页码:1331 / 1340
页数:10
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