Characterization of individual particles and meteorological conditions during the cold season in Zhengzhou using a single particle aerosol mass spectrometer

气溶胶 薄雾 环境科学 相对湿度 大气科学 粒子(生态学) 风速 左旋葡糖 湿度 生物质燃烧 气象学 地理 物理 地质学 海洋学
作者
Shenbo Wang,Bing He,Minghao Yuan,Fangcheng Su,Shasha Yin,Qishe Yan,Nan Jiang,Ruiqin Zhang,Xiaoyan Tang
出处
期刊:Atmospheric Research [Elsevier BV]
卷期号:219: 13-23 被引量:14
标识
DOI:10.1016/j.atmosres.2018.12.021
摘要

To investigate the formation of haze during the cold season, continuous ambient air measurements were taken at an urban site in Zhengzhou from October 10, 2016 through December 31, 2016 using a single particle aerosol mass spectrometer. In total, 4,099,800 particles were analyzed and classified into eight major particle types: elemental carbon (EC, 36.7%), organic carbon (OC, 30.0%), ECOC (8.6%), K-rich (13.0%), levoglucosan (1.2%), metal (2.2%), NH4-K (2.1%), and dust (6.2%). By combining these measurements with correlation analysis and wind data, particle sources were determined to be vehicles, industrial emissions, coal combustion, biomass burning, secondary aerosols, agriculture, and dust. Additionally, analysis of mixing states indicated that particles underwent substantial aging and secondary OC particles were dominant OC species. Temporal profiles of meteorological parameters, mixing states, and particle types during a typical haze episode revealed that EC and OC particles were dominant components during haze formation, and a northeastern transport route (Anyang-Zhengzhou and Puyang-Xuchang) for OC particles was identified by potential source contribution function and concentration weighted trajectory analysis. Relatively higher humidity and lower temperature favored the formation of secondary inorganic aerosol. Wind direction and speed determined the transport, formation, and elimination of stagnant weather conditions. In sum, heavy haze during the cold season in Zhengzhou was observed due to extensive aerosol aging under adverse weather conditions (i.e., northeastern wind direction, wind speed <2 m s−1, temperature < 10 °C, relative humidity >60%, temperature inversion, and uniform pressure field).

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