Composition and reactivity of volatile organic compounds in the South Coast Air Basin and San Joaquin Valley of California

被引:7
|
作者
Liu, Shang [1 ]
Barletta, Barbara [2 ]
Hornbrook, Rebecca S. [3 ]
Fried, Alan [4 ]
Peischl, Jeff [5 ,6 ]
Meinardi, Simone [2 ]
Coggon, Matthew [5 ,6 ]
Lamplugh, Aaron [5 ,6 ]
Gilman, Jessica B. [6 ]
Gkatzelis, Georgios, I [5 ,6 ,7 ]
Warneke, Carsten [6 ]
Apel, Eric C. [3 ]
Hills, Alan J. [3 ]
Bourgeois, Ilann [5 ,6 ]
Walega, James [4 ]
Weibring, Petter [4 ]
Richter, Dirk [4 ]
Kuwayama, Toshihiro [1 ]
FitzGibbon, Michael [1 ]
Blake, Donald [2 ]
机构
[1] Calif Air Resources Board, Res Div, Sacramento, CA 95814 USA
[2] Univ Calif Irvine, Dept Chem, Irvine, CA 92697 USA
[3] Natl Ctr Atmospher Res, Atmospher Chem Observat & Modeling Lab, Boulder, CO 80301 USA
[4] Univ Colorado, Inst Arctic & Alpine Res, Boulder, CO 80303 USA
[5] Univ Colorado, Cooperat Inst Res Environm Sci, Boulder, CO 80309 USA
[6] NOAA, Chem Sci Lab, Boulder, CO 80305 USA
[7] Forschungszentrum Julich, Inst Energy & Climate Res, IEK 8 Troposphere, D-52428 Julich, Germany
基金
美国国家科学基金会;
关键词
GAS-PHASE REACTIONS; TOTAL OH REACTIVITY; ATMOSPHERIC CHEMISTRY; PHOTOCHEMICAL DATA; HYDROCARBON EMISSIONS; BIOGENIC ISOPRENE; VOC REACTIVITY; DAIRY-COWS; FORMALDEHYDE; OZONE;
D O I
10.5194/acp-22-10937-2022
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Comprehensive aircraft measurements of volatile organic compounds (VOCs) covering the South Coast Air Basin (SoCAB) and San Joaquin Valley (SJV) of California were obtained in the summer of 2019. Combined with the CO, CH4, and NOx data, the total calculated gas-phase hydroxyl radical reactivity (cOHR(TOTAL)) was quantified to be 6.1 and 4.6 s(-1) for the SoCAB and SJV, respectively. VOCs accounted for similar to 60 %-70 % of the cOHR(TOTAL) in both basins. In particular, oxygenated VOCs (OVOCs) contributed >60 % of the cOHR of total VOCs (cOHR(VOC)) and the total observed VOC mixing ratio. Primary biogenic VOCs (BVOCs) represented a minor fraction (<2 %) of the total VOC mixing ratio but accounted for 21 % and 6 % of the cOHR(VOC) in the SoCAB and SJV, respectively. Furthermore, the contribution of BVOCs to the cOHR(VOC) increased with increasing cOHR(VOC) in the SoCAB, suggesting that BVOCs were important ozone precursors during high ozone episodes. Spatially, the trace gases were heterogeneously distributed in the SoCAB, with their mixing ratios and cOHR being significantly greater over the inland regions than the coast, while their levels were more evenly distributed in SJV. The results highlight that a better grasp of the emission rates and sources of OVOCs and BVOCs is essential for a predictive understanding of the ozone abundance and distribution in California.
引用
收藏
页码:10937 / 10954
页数:18
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