Atmospheric oxidation chemistry and ozone production: Results from SHARP 2009 in Houston, Texas

Ozone (O3) and secondary fine particles come from the atmospheric oxidation chemistry that involves the hydroxyl radical (OH) and hydroperoxyl radical (HO2), which are together called HOx. Radical precursors such as nitrous acid (HONO) and formaldehyde (HCHO) significantly affect the HOx budget in u...

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Veröffentlicht in:Journal of geophysical research. Atmospheres 2013-06, Vol.118 (11), p.5770-5780
Hauptverfasser: Ren, Xinrong, van Duin, Diana, Cazorla, Maria, Chen, Shuang, Mao, Jingqiu, Zhang, Li, Brune, William H., Flynn, James H., Grossberg, Nicole, Lefer, Barry L., Rappenglück, Bernhard, Wong, Kam W., Tsai, Catalina, Stutz, Jochen, Dibb, Jack E., Thomas Jobson, B., Luke, Winston T., Kelley, Paul
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container_end_page 5780
container_issue 11
container_start_page 5770
container_title Journal of geophysical research. Atmospheres
container_volume 118
creator Ren, Xinrong
van Duin, Diana
Cazorla, Maria
Chen, Shuang
Mao, Jingqiu
Zhang, Li
Brune, William H.
Flynn, James H.
Grossberg, Nicole
Lefer, Barry L.
Rappenglück, Bernhard
Wong, Kam W.
Tsai, Catalina
Stutz, Jochen
Dibb, Jack E.
Thomas Jobson, B.
Luke, Winston T.
Kelley, Paul
description Ozone (O3) and secondary fine particles come from the atmospheric oxidation chemistry that involves the hydroxyl radical (OH) and hydroperoxyl radical (HO2), which are together called HOx. Radical precursors such as nitrous acid (HONO) and formaldehyde (HCHO) significantly affect the HOx budget in urban environments. These chemical processes connect surface anthropogenic and natural emissions to local and regional air pollution. Using the data collected during the Study of Houston Atmospheric Radical Precursors (SHARP) in spring 2009, we examine atmospheric oxidation chemistry and O3 production in this polluted urban environment. A numerical box model with five different chemical mechanisms was used to simulate the oxidation processes and thus OH and HO2 in this study. In general, the model reproduced the measured OH and HO2 with all five chemical mechanisms producing similar levels of OH and HO2, although midday OH was overpredicted and nighttime OH and HO2 were underpredicted. The calculated HOx production was dominated by HONO photolysis in the early morning and by the photolysis of O3 and oxygenated volatile organic compounds (OVOCs) in the midday. On average, the daily HOx production rate was 24.6 ppbv d−1, of which 30% was from O3 photolysis, 22% from HONO photolysis, 15% from the photolysis of OVOCs (other than HCHO), 14% from HCHO photolysis, and 13% from O3 reactions with alkenes. The O3 production was sensitive to volatile organic compounds (VOCs) in the early morning but was sensitive to NOx for most of afternoon. This is similar to the behavior observed in two previous summertime studies in Houston: the Texas Air Quality Study in 2000 (TexAQS 2000) and the TexAQS II Radical and Aerosol Measurement Project in 2006 (TRAMP 2006). Ozone production in SHARP exhibits a longer NOx‐sensitive period than TexAQS 2000 and TRAMP 2006, indicating that NOx control may be an efficient approach for the O3 control in springtime for Houston. Results from this study provide additional support for regulatory actions to reduce NOx and reactive VOCs in Houston in order to reduce O3 and other secondary pollutants. Key Points The model reproduced the measured OH and HO2 with all five chemical mechanisms. HOx production was dominated by HONO photolysis in the early morning. P(O3) was VOC sensitive in the morning and NOx sensitive for most of afternoon.
doi_str_mv 10.1002/jgrd.50342
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Radical precursors such as nitrous acid (HONO) and formaldehyde (HCHO) significantly affect the HOx budget in urban environments. These chemical processes connect surface anthropogenic and natural emissions to local and regional air pollution. Using the data collected during the Study of Houston Atmospheric Radical Precursors (SHARP) in spring 2009, we examine atmospheric oxidation chemistry and O3 production in this polluted urban environment. A numerical box model with five different chemical mechanisms was used to simulate the oxidation processes and thus OH and HO2 in this study. In general, the model reproduced the measured OH and HO2 with all five chemical mechanisms producing similar levels of OH and HO2, although midday OH was overpredicted and nighttime OH and HO2 were underpredicted. The calculated HOx production was dominated by HONO photolysis in the early morning and by the photolysis of O3 and oxygenated volatile organic compounds (OVOCs) in the midday. On average, the daily HOx production rate was 24.6 ppbv d−1, of which 30% was from O3 photolysis, 22% from HONO photolysis, 15% from the photolysis of OVOCs (other than HCHO), 14% from HCHO photolysis, and 13% from O3 reactions with alkenes. The O3 production was sensitive to volatile organic compounds (VOCs) in the early morning but was sensitive to NOx for most of afternoon. This is similar to the behavior observed in two previous summertime studies in Houston: the Texas Air Quality Study in 2000 (TexAQS 2000) and the TexAQS II Radical and Aerosol Measurement Project in 2006 (TRAMP 2006). Ozone production in SHARP exhibits a longer NOx‐sensitive period than TexAQS 2000 and TRAMP 2006, indicating that NOx control may be an efficient approach for the O3 control in springtime for Houston. Results from this study provide additional support for regulatory actions to reduce NOx and reactive VOCs in Houston in order to reduce O3 and other secondary pollutants. Key Points The model reproduced the measured OH and HO2 with all five chemical mechanisms. HOx production was dominated by HONO photolysis in the early morning. P(O3) was VOC sensitive in the morning and NOx sensitive for most of afternoon.</description><identifier>ISSN: 2169-897X</identifier><identifier>EISSN: 2169-8996</identifier><identifier>DOI: 10.1002/jgrd.50342</identifier><language>eng</language><publisher>Hoboken, NJ: Blackwell Publishing Ltd</publisher><subject>Air pollution ; Air quality ; Alkenes ; Anthropogenic factors ; Atmospheric chemistry ; Atmospherics ; Chemistry ; Computer simulation ; Earth, ocean, space ; Emission measurements ; Exact sciences and technology ; External geophysics ; Geophysics ; Houston ; Hydroxyl radicals ; Mathematical models ; Meteorology ; Morning ; Nitric acids ; Nitrogen compounds ; Nitrous acid ; Organic compounds ; Outdoor air quality ; Oxidation ; Oxides ; Ozone ; Ozone Production ; Photochemsitry ; Photolysis ; Pollutants ; Radicals ; SHARP ; Urban environments ; VOCs ; Volatile organic compounds</subject><ispartof>Journal of geophysical research. 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Atmospheres</title><addtitle>J. Geophys. Res. Atmos</addtitle><description>Ozone (O3) and secondary fine particles come from the atmospheric oxidation chemistry that involves the hydroxyl radical (OH) and hydroperoxyl radical (HO2), which are together called HOx. Radical precursors such as nitrous acid (HONO) and formaldehyde (HCHO) significantly affect the HOx budget in urban environments. These chemical processes connect surface anthropogenic and natural emissions to local and regional air pollution. Using the data collected during the Study of Houston Atmospheric Radical Precursors (SHARP) in spring 2009, we examine atmospheric oxidation chemistry and O3 production in this polluted urban environment. A numerical box model with five different chemical mechanisms was used to simulate the oxidation processes and thus OH and HO2 in this study. 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Ozone production in SHARP exhibits a longer NOx‐sensitive period than TexAQS 2000 and TRAMP 2006, indicating that NOx control may be an efficient approach for the O3 control in springtime for Houston. Results from this study provide additional support for regulatory actions to reduce NOx and reactive VOCs in Houston in order to reduce O3 and other secondary pollutants. Key Points The model reproduced the measured OH and HO2 with all five chemical mechanisms. HOx production was dominated by HONO photolysis in the early morning. 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Atmos</addtitle><date>2013-06-16</date><risdate>2013</risdate><volume>118</volume><issue>11</issue><spage>5770</spage><epage>5780</epage><pages>5770-5780</pages><issn>2169-897X</issn><eissn>2169-8996</eissn><abstract>Ozone (O3) and secondary fine particles come from the atmospheric oxidation chemistry that involves the hydroxyl radical (OH) and hydroperoxyl radical (HO2), which are together called HOx. Radical precursors such as nitrous acid (HONO) and formaldehyde (HCHO) significantly affect the HOx budget in urban environments. These chemical processes connect surface anthropogenic and natural emissions to local and regional air pollution. Using the data collected during the Study of Houston Atmospheric Radical Precursors (SHARP) in spring 2009, we examine atmospheric oxidation chemistry and O3 production in this polluted urban environment. A numerical box model with five different chemical mechanisms was used to simulate the oxidation processes and thus OH and HO2 in this study. In general, the model reproduced the measured OH and HO2 with all five chemical mechanisms producing similar levels of OH and HO2, although midday OH was overpredicted and nighttime OH and HO2 were underpredicted. The calculated HOx production was dominated by HONO photolysis in the early morning and by the photolysis of O3 and oxygenated volatile organic compounds (OVOCs) in the midday. On average, the daily HOx production rate was 24.6 ppbv d−1, of which 30% was from O3 photolysis, 22% from HONO photolysis, 15% from the photolysis of OVOCs (other than HCHO), 14% from HCHO photolysis, and 13% from O3 reactions with alkenes. The O3 production was sensitive to volatile organic compounds (VOCs) in the early morning but was sensitive to NOx for most of afternoon. This is similar to the behavior observed in two previous summertime studies in Houston: the Texas Air Quality Study in 2000 (TexAQS 2000) and the TexAQS II Radical and Aerosol Measurement Project in 2006 (TRAMP 2006). Ozone production in SHARP exhibits a longer NOx‐sensitive period than TexAQS 2000 and TRAMP 2006, indicating that NOx control may be an efficient approach for the O3 control in springtime for Houston. Results from this study provide additional support for regulatory actions to reduce NOx and reactive VOCs in Houston in order to reduce O3 and other secondary pollutants. Key Points The model reproduced the measured OH and HO2 with all five chemical mechanisms. HOx production was dominated by HONO photolysis in the early morning. P(O3) was VOC sensitive in the morning and NOx sensitive for most of afternoon.</abstract><cop>Hoboken, NJ</cop><pub>Blackwell Publishing Ltd</pub><doi>10.1002/jgrd.50342</doi><tpages>11</tpages><oa>free_for_read</oa></addata></record>
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source Wiley Free Content; Wiley Online Library Journals Frontfile Complete; Alma/SFX Local Collection
subjects Air pollution
Air quality
Alkenes
Anthropogenic factors
Atmospheric chemistry
Atmospherics
Chemistry
Computer simulation
Earth, ocean, space
Emission measurements
Exact sciences and technology
External geophysics
Geophysics
Houston
Hydroxyl radicals
Mathematical models
Meteorology
Morning
Nitric acids
Nitrogen compounds
Nitrous acid
Organic compounds
Outdoor air quality
Oxidation
Oxides
Ozone
Ozone Production
Photochemsitry
Photolysis
Pollutants
Radicals
SHARP
Urban environments
VOCs
Volatile organic compounds
title Atmospheric oxidation chemistry and ozone production: Results from SHARP 2009 in Houston, Texas
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