RESOURCES AND ENVIRONMENT IN THE YANGTZE BASIN >> 2017, Vol. 26 >> Issue (05): 706-712.doi: 10.11870/cjlyzyyhj201705007

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SPATIOTEMPORAL CHARACTERISTICS OF NEGATIVE AIR IONS AND ITS RELATIONSHIP WITH METEOROLOGICAL CONDITIONS IN PUKOU, NANJING

LIU Yan1,3, WANG Ye-cheng2, WANG Rang-hui1,3, LIU Yuan2, YUAN Qi-fei2, LI Cheng3   

  1. 1. School of Environmental Science and Engineering, Nanjing University of Information Science & Technology, Nanjing 210044, China;
    2. Meteorology Bureau of Pukou, Nanjing 211800, China;
    3. Jiangsu Collaborative Innovation Center of Atmospheric Environment and Equipment Technology(CICAEET), Nanjing University of Information Science & Technology, Nanjing 210044, China
  • Received:2016-10-09 Revised:2017-01-01 Online:2017-05-20
  • Supported by:
    The Clean Development Mechanism Fund of China (2013013);The National Key Technology R&D Program of China (No. 2012BAD16B0305; 2012BAC23B01)

Abstract: Spatiotemporal characteristics of negative air ions concentrations and their relationships with meteorological factors in Pukou (Laoshan Forest, Nongzhaung, Pearl Spring, Shiqiaowancheng) were analyzed between Oct 2014 and Oct 2015. The results showed that:(1) The daily average concentration of negative air ions were 688/cm3 in Pukou (Nanjing), the maximum value of 986/cm3 appeared around 21:00; the minimum value of 610 appeared around 12:00; (2) The annual average concentration of negative air ions were 675/cm3 in Pukou (Nanjing), and the largest average concentration was 728/cm3 in summer, while the lowest was 728/cm3 in winter; (3) The negative air ions concentration was the largest in Nongzhuang, while the lowest in Shiqiaowancheng; (4) In different weather conditions, the relationships between negative air ions concentration and meteorological factors were different. In rainy, negative air ions were significantly correlated with precipitation, temperature and relative humidity (P < 0.01). In non-rainy days, negative air ions were significantly correlated with sunshine (P < 0.05).

Key words: negative air ion, concentration variation, spatial distribution, meteorological factors

CLC Number: 

  • X16
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