Atmos. Chem. Phys. Discuss., 11, 8595-8623, 2011
www.atmos-chem-phys-discuss.net/11/8595/2011/
doi:10.5194/acpd-11-8595-2011
© Author(s) 2011. This work is distributed
under the Creative Commons Attribution 3.0 License.
Review Status
This discussion paper has been under review for the journal Atmospheric Chemistry and Physics (ACP). Please refer to the corresponding final paper in ACP.
VOC reactivity and its effect on ozone production during the HaChi summer campaign
L. Ran1, C. S. Zhao1, W. Y. Xu1, X. Q. Lu2, M. Han2, W. L. Lin3, P. Yan3, X. B. Xu3, Z. Z. Deng1, N. Ma1, P. F. Liu1, J. Yu4,*, W. D. Liang4, and L. L. Chen4
1Department of Atmospheric and Oceanic Sciences, School of Physics, Peking University, Beijing, China
2Tianjin Academy of Environmental Sciences, Tianjin, China
3Key Laboratory for Atmospheric Chemistry, Center for Atmosphere Watch and Services, Chinese Academy of Meteorological Sciences, China Meteorological Administration, Beijing, China
4Wuqing Meteorological Bureau of Tianjin, China
*now at: Tanggu Meteorological Bureau of Tianjin, China

Abstract. Measurements of ozone and its precursors conducted within the HaChi (Haze in China) project in summer 2009 were analyzed to characterize volatile organic compounds (VOCs) and their effects on ozone photochemical production at a suburban site in the North China Plain. Ozone episodes, during which running 8-h average ozone concentrations exceeding 80 ppbv lasted for more than 4 h, occurred on about two thirds of the observational days during the 5-week field campaign. This suggests continuous ozone exposure risks in this region during the summer. The average concentrations of nitrogen oxides (NOx) and VOCs are about 20 ppbv and 650 ppbC, respectively. Total VOC reactivity is dominated by anthropogenic VOCs, including aromatics, alkanes and most alkenes. The contribution of biogenic VOCs to total ozone-forming potential, however, is also considerable in the daytime. 2-butenes, isoprene, trimethylbenzenes, xylenes, 3-methylhexane, n-hexane and toluene are key species associated with ozone photochemical production. Formation of ozone is found to be NOx-limited as indicated by measured VOCs/NOx ratios and further confirmed by a sensitivity study using a photochemical box model NCAR_MM. The Model simulation suggests that ozone production is also sensitive to changes in VOC reactivity under the NOx-limited regime, although this sensitivity depends strongly on how much NOx is present.

Citation: Ran, L., Zhao, C. S., Xu, W. Y., Lu, X. Q., Han, M., Lin, W. L., Yan, P., Xu, X. B., Deng, Z. Z., Ma, N., Liu, P. F., Yu, J., Liang, W. D., and Chen, L. L.: VOC reactivity and its effect on ozone production during the HaChi summer campaign, Atmos. Chem. Phys. Discuss., 11, 8595-8623, doi:10.5194/acpd-11-8595-2011, 2011.
 
Search ACPD
Discussion Paper
    XML
    Citation
    Final Revised Paper
    Share