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青岛春节期间大气污染特征及烟花燃放一、二次贡献分析
摘要点击 2233  全文点击 910  投稿时间:2020-02-22  修订日期:2020-04-16
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中文关键词  颗粒物累积  烟花燃放  硝酸盐  硫酸盐  二次生成
英文关键词  particulate accumulations  firework burning  nitrate  sulfate  secondary formation
作者单位E-mail
方天歌 中国海洋大学海洋环境与生态教育部重点实验室, 青岛 266100 fangtiange@stu.ouc.edu.cn 
姚小红 中国海洋大学海洋环境与生态教育部重点实验室, 青岛 266100
青岛海洋科学与技术国家实验室海洋生态与环境科学功能实验室, 青岛 266071 
xhyao@ouc.edu.cn 
孟赫 山东省青岛生态环境监测中心, 青岛 266003  
陈春强 中国海洋大学海洋环境与生态教育部重点实验室, 青岛 266100  
中文摘要
      我国北方地区冬季采暖期大气污染事件频发,期间硝酸盐成为促进PM2.5增加的主要因素.然而在烟花燃放期间,硫酸盐的累积却强于硝酸盐,形成不同的污染特征.对春节期间(2019年2月2~10日)青岛近郊在线离子色谱观测数据,结合国控自动监测站数据进行综合分析.结果表明,研究期间观测到大气颗粒物累积事件、沙尘过境事件和烟花燃放事件.烟花燃放高峰期,其对PM2.5和PM10的一次贡献率分别为69.8%和63.8%.相比颗粒物累积期间硝酸盐有更明显的累积,硫酸盐在烟花燃放期间先于硝酸盐生成,并存在更强的累积.分离得到烟花燃放的一次贡献因子n(SO42-)/n(K+)和n(NO3-)/n(K+)特征摩尔比分别为1.2和1.3;利用该比值估算得到对SO42-和NO3-二次贡献因子,在较稳定的气象条件下分别为一次贡献因子的2.1倍和1.6倍;但在强的干冷空气过境时,二次贡献因子大幅降低,与一次贡献因子相当.
英文摘要
      Atmospheric pollution frequently occurs in northern China during winter heating period, wherein nitrate became the dominant driver for PM2.5 accumulations. However, sulfate accumulation was found to be significantly higher than that of nitrate during firework burning events and exhibited different pollution characteristics. Online data available from February 2, 2019 to February 10, 2019, including observation data measured from AIM-IC in suburban Qingdao and meteorological data from national automatic monitoring station, were analyzed. The results showed that particulate accumulation, dust and firework burning events were observed. The primary contribution rates of the most intensive firework burning to PM2.5 and PM10 were 69.8% and 63.8%, respectively. In contrast to a severe accumulation of nitrate during the particulate accumulation event, the sulfate formed prior and exhibited more severe accumulation than nitrate during the firework burning events. The primary contribution factors n(SO42-)/n(K+) and n(NO3-)/n(K+) of firework burnings was 1.2 and 1.3 (molar ratios), respectively. The secondary contribution factors were 2.1 and 1.6 times, under relatively stable meteorological conditions. However, during the transit of dry and cold air, the value of secondary contribution factors decreased substantially and exhibited nearly the same values as the primary ones.

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