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青岛沿海地区夏季和冬季新粒子生成特征对比
引用本文:孙悦,朱玉姣,孟赫,刘兵,刘玉虹,董灿,姚小红,王文兴,薛丽坤. 青岛沿海地区夏季和冬季新粒子生成特征对比[J]. 环境科学, 2021, 42(5): 2133-2142
作者姓名:孙悦  朱玉姣  孟赫  刘兵  刘玉虹  董灿  姚小红  王文兴  薛丽坤
作者单位:山东大学环境研究院,青岛 266237;山东省青岛生态环境监测中心,青岛 266003;中国海洋大学海洋环境与生态教育部重点实验室,青岛 266100
基金项目:国家自然科学基金项目(41706122,41922051,41905113);江苏全球变化协同创新中心项目
摘    要:利用宽范围粒径谱仪(WPS)和电迁移率粒径分析仪(SMPS)对青岛沿海地区夏、冬两季大气颗粒物数浓度和粒径谱分布进行了实时测量,同时结合无机和有机气态前体物、大气颗粒物化学组分、气象参数以及后向气流轨迹,对新粒子生成(NPF)特征进行了分析对比.结果表明,在夏季,NPF事件发生频率较低,为18%.夏季NPF事件发生时,...

关 键 词:沿海地区  新粒子生成(NPF)  大气颗粒物数浓度  气态前体物  化学组成
收稿时间:2020-07-24
修稿时间:2020-10-12

New Particle Formation Events in Summer and Winter in the Coastal Atmosphere in Qingdao, China
SUN Yue,ZHU Yu-jiao,MENG He,LIU Bing,LIU Yu-hong,DONG Can,YAO Xiao-hong,WANG Wen-xing,XUE Li-kun. New Particle Formation Events in Summer and Winter in the Coastal Atmosphere in Qingdao, China[J]. Chinese Journal of Environmental Science, 2021, 42(5): 2133-2142
Authors:SUN Yue  ZHU Yu-jiao  MENG He  LIU Bing  LIU Yu-hong  DONG Can  YAO Xiao-hong  WANG Wen-xing  XUE Li-kun
Affiliation:Environment Research Institute, Shandong University, Qingdao 266237, China;Qingdao Eco-environment Monitoring Center of Shandong Province, Qingdao 266003, China;Key Laboratory of Marine Environmental Science and Ecology, Ministry of Education, Ocean University of China, Qingdao 266100, China
Abstract:Atmospheric particle number size distributions were measured by a wide-range particle size spectrometer and a scanning mobility particle size spectrometer in the summertime and wintertime in the coastal area of Qingdao (China). The inorganic and organic gaseous precursors and particulate chemical composition were measured to characterize new particle formation (NPF) events by combining meteorological parameters and backward trajectories. In summer, the occurrence frequency of NPF events was 18% lower. However, the atmospheric particle number concentration increased by approximately 1-4 times during the NPF events compared with those without NPF. The apparent formation rates and growth rates were (5.2±4.3) cm-3·s-1 and (6.5±2.2) nm·h-1, respectively, except for a special NPF event on July 20. The correlation analysis results implied that biogenic volatile organic compounds (BVOCs) seemingly favor NPF, and the reverse is true for anthropogenic volatile organic compounds (AVOCs). The occurrence frequency of NPF events of 27% in winter was clearly higher than that in summer. The apparent formation rates and growth rates, i.e., (3.3±3.1) cm-3·s-1 and (5.3±3.3) nm·h-1, decreased, although the decreases were not significant (P>0.05). The correlation analyses implied that AVOCs favored NPF. However, BVOCs had no correlation with NPF. For the cases in which new particles could grow to CCN sizes (>50 nm), the particle growth characteristics showed significant seasonal differences, i.e., in summer, new particles could grow to CCN sizes via photochemical reactions, whereas in winter, second-stage growth driven by the formation of nitrate aerosols was needed to grow new particles to CCN sizes.
Keywords:coastal area  new particle formation(NPF)  atmospheric particle number concentration  gaseous precursors  chemical composition
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