Contribution of isoprene to formaldehyde and ozone formation based on its oxidation products measurement in Beijing,China |
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| Authors: | Xiaobing Pang Yujing Mu Yujie Zhang Xinqing Lee Juan Yuan |
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| Institution: | 1. Yale-NUIST Center on Atmospheric Environment, International Joint Laboratory on Climate and Environment Change, Nanjing University of Information Science and Technology, Nanjing, 210044, China;2. Key Laboratory of Meteorological Disaster; Ministry of Education & Collaborative Innovation Center on Forecast and Evaluation of Meteorological Disaster, Nanjing University of Information Science and Technology, Nanjing, 210044, China;3. Jiangsu Provincial Key Laboratory of Agricultural Meteorology, College of Applied Meteorology, Nanjing University of Information Science & Technology, Nanjing 210044, China;1. Beijing Weather Modification Office, Beijing, China;2. Institute of Urban Meteorology, Chinese Meteorological Administration, Beijing, China;3. Beijing Key Laboratory of Cloud, Precipitation, and Atmospheric Water Resources, Beijing, China;4. Beijing Cloud Laboratory and Observational Utilities Deployment Base, Beijing, China;5. Weather Modification Center, Chinese Meteorological Administration, Beijing, China |
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| Abstract: | The atmospheric mixing ratios of methacrolein (MACR) and methyl vinyl ketone (MVK), the two specific products from isoprene oxidation in the atmosphere, were measured in Beijing from March to November, 2006. Distinct amounts of MACR and MVK were detected during vegetable growing seasons from April to October with ambient levels of 0.11–0.67 ppbv and 0.19–1.36 ppbv, respectively. The reacted isoprene and its ozone formation potentials (OFPs) in Beijing were evaluated in the range of 0.49–3.46 ppbv and 6.4–44.7 ppbv, respectively, from April to October. OFP of the reacted isoprene accounted for 10.6–23.6% of the total OFPs of VOCs (including carbonyls and isoprene) and 6.38–29.9% of the photo-chemically produced ozone. The maximum OFP of the original emitted isoprene prior to its photo-oxidation was calculated as 56.0 ppbv in August. The contribution from the reacted isoprene in Beijing to HCHO formation was also estimated to be in the range of 0.35–2.45 ppbv from April to October, which accounted for 4.6–11.5% of ambient HCHO. |
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