Summertime ambient ammonia and its effects on ammonium aerosol in urban Beijing, China

被引:35
|
作者
Meng, Zhaoyang [1 ,2 ]
Lin, Weili [3 ]
Zhang, Renjian [4 ]
Han, Zhiwei [4 ]
Jia, Xiaofang [3 ]
机构
[1] Chinese Acad Meteorol Sci, State Key Lab Severe Weather, Beijing 100081, Peoples R China
[2] Chinese Acad Meteorol Sci, Key Lab Atmospher Chem CMA, Beijing 100081, Peoples R China
[3] CMA Meteorol Observat Ctr, Beijing 100081, Peoples R China
[4] Chinese Acad Sci, Inst Atmospher Phys, Beijing 100029, Peoples R China
基金
中国国家自然科学基金;
关键词
Ambient ammonia; Ammonium in PM2.5 particulates; Gas-to-particle conversion; Urban Beijing; AIR-MASS HISTORY; ATMOSPHERIC AMMONIA; GASEOUS-POLLUTANTS; INORGANIC-IONS; ACIDIC GASES; EMISSIONS; PM2.5; NH3; REDUCTIONS; TRANSPORT;
D O I
10.1016/j.scitotenv.2016.11.159
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
To improve the understanding of NH3 variation in urban Beijing, high temporal resolution (1-min averaged) NH3 data derived during the summer of 2009 were analyzed. The results indicated that after rain there was generally an increase in NH3 concentration. The analysis of the 1-min data revealed that a weak but significant linear correlation existed between NH3 and NOx in August, indicating a connection between NH3 concentrations and traffic levels during summer. This was further supported by peak NH3 levels approximately coinciding with morning rush hours. The daily NH3 concentrations were weakly correlated with NH4+ concentrations, suggesting that NH3 played an important precursor role in NH4+ in PM2.5 formation. The mean mass ratio of NH3/NHx was 0.76 +/- 0.13. This revealed that NHx (NH3 + NH4+) was influenced by local sources during the summer period and that NH3 dry deposition could contribute substantially to NHx deposition. A high temperature, relative humidity, and degree of oxidization could increase photochemical reactions and aqueous processing, having the important effect of SO2 to SO42- and NH3 to NH4+ conversion in summer. The back trajectory analysis indicates that the transport of airmasses fromthe North China Plain region contributed to the atmospheric NH3 and NH4+ aerosol variations in Beijing. (C) 2016 Elsevier B.V. All rights reserved.
引用
收藏
页码:1521 / 1530
页数:10
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