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Chinese Journal of Applied Ecology ›› 2016, Vol. 27 ›› Issue (6): 1811-1819.doi: 10.13287/j.1001-9332.201606.037

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Observation of ozone dry deposition in the field of winter wheat.

LI Shuo1*, ZHENG You-fei1,2.3, WU Rong-jun2, YIN Ji-fu3, XU Jing-xin3, ZHAO Hui1, SUN Jian4   

  1. 1College of Environmental Science and Engineering, Nanjing University of Information Science &
    Technology, Nanjing 210044, China;
    2Jiangsu Key Laboratory of Atmospheric Environment Motoring &
    Pollution Control, Nanjing 210044, China;
    3College of Atmospheric Physics, Nanjing University of Information Science &
    Technology, Nanjing 210044, China;
    4Minhang Meteorological Bureau, Shanghai 201199, China
  • Received:2015-12-23 Published:2016-06-18

Abstract: Ozone is one of the main atmospheric pollutants over surface layer, and its increasing surface ozone concentration and its impact on main crops have become the focus of the public. In order to explore ozone deposition law and environmental factors influencing ozone deposition process, this study used the micrometeorological methods and carried out the experiment under natural conditions. The results showed that during the observational period (the vigorously growing season of wheat), the mean value of ozone flux was -0.35 μg·m-2·s-1(the negative sign indicated that the deposition direction was toward the ground). The mean rate of ozone deposition was 0.55 cm·s-1. The mean value of aerodynamic resistance was 30 s·m-1, the mean value of sub-layer resistance was 257 s·m-1, and that of the canopy layer stomatic resistance was 163 s·m-1. All the test parameters presented distinct diurnal fluctuation. The ozone deposition resistance was influenced by friction velocity, solar radiation velocity, temperature, relative humidity and other factors.