Atmospheric Chemistry and Physics (May 2011)

VOC reactivity and its effect on ozone production during the HaChi summer campaign

  • L. Ran,
  • C. S. Zhao,
  • W. Y. Xu,
  • X. Q. Lu,
  • M. Han,
  • W. L. Lin,
  • P. Yan,
  • X. B. Xu,
  • Z. Z. Deng,
  • N. Ma,
  • P. F. Liu,
  • J. Yu,
  • W. D. Liang,
  • L. L. Chen

DOI
https://doi.org/10.5194/acp-11-4657-2011
Journal volume & issue
Vol. 11, no. 10
pp. 4657 – 4667

Abstract

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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 (NCP). 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 in the summer. Average concentrations of nitrogen oxides (NO<sub>x</sub>) and VOCs are about 20 ppbv and 650 ppbC, respectively. On average, total VOC reactivity is dominated by anthropogenic VOCs. The contribution of biogenic VOCs to total ozone-forming potential, however, is also considerable in the daytime. Key species associated with ozone photochemical production are 2-butenes (18 %), isoprene (15 %), trimethylbenzenes (11 %), xylenes (8.5 %), 3-methylhexane (6 %), n-hexane (5 %) and toluene (4.5 %). Formation of ozone is found to be NO<sub>x</sub>-limited as indicated by measured VOCs/NO<sub>x</sub> 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 NO<sub>x</sub>-limited regime, although this sensitivity depends strongly on how much NO<sub>x</sub> is present.