Characteristics and formation mechanism of regional haze episodes in the Pearl River Delta of China

被引:48
|
作者
Li, Wenguang [1 ]
Liu, Xingang [1 ]
Zhang, Yuanhang [2 ]
Sun, Kang [2 ]
Wu, Yusheng [2 ]
Xue, Rui [2 ]
Zeng, Limin [2 ]
Qu, Yu [3 ]
An, Junling [3 ]
机构
[1] Beijing Normal Univ, Sch Environm, State Key Lab Water Environm Simulat, Beijing 100875, Peoples R China
[2] Peking Univ, Coll Environm Sci & Engn, State Key Joint Lab Environm Simulat & Pollut Con, Beijing 100871, Peoples R China
[3] Chinese Acad Sci, Inst Atmospher Phys, State Key Lab Atmospher Boundary Layer Phys & Atm, Beijing 100029, Peoples R China
基金
中国国家自然科学基金;
关键词
Haze episodes; Chemical characteristics; Formation mechanism; PRD; SECONDARY ORGANIC AEROSOL; CHEMICAL-COMPOSITION; EVOLUTION PROCESSES; PM2.5; CONCENTRATION; RELATIVE-HUMIDITY; ABSORPTION-MODEL; AIR-POLLUTION; JANUARY; 2013; VISIBILITY; ATMOSPHERE;
D O I
10.1016/j.jes.2017.03.018
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
To investigate the characteristics and the specific mechanism of continuous haze, comprehensive measurements were conducted from 15 October to 19 November in the Atmospheric Environment Monitoring Super-Station in Heshan of Guangdong province. Five haze episodes occurred in October and November 2014 in the Pearl River Delta (PRD) region. The meteorological parameters, gas data, chemical compositions, and optical parameters of the aerosols were obtained. Among these events, the second haze episode, with the highest concentration of PM2.5 of 187.51 mu g/m(3), was the most severe. NO3- was always higher than SO42-, which indicated that motor vehicles played an important role in the haze, even though the oxidation rate from SO2 to SO42- was faster than that of NOX to NO3-. The difference between the hourly averages of Na+ and K+ during the haze episode and clean days was small, implying that straw combustion and sea salt had no significant effect on the occurrence of haze, and the backward trajectories of the air masses also conformed with this result. The air pollutants were difficult to disperse because of the significant decrease in the planetary boundary layer (PBL) height. Relative humidity played a crucial role in the formation of haze by leading to hygroscopic growth of the diameter of aerosols. (C) 2017 The Research Center for Eco-Environmental Sciences, Chinese Academy of Sciences. Published by Elsevier B.V.
引用
收藏
页码:236 / 249
页数:14
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