Spatio-Temporal Evolution Characteristics and Source Apportionment of O3 and NO2 in Shijiazhuang

被引：2

作者：

Wang S. ^{[1
]}

Nie S.-S. ^{[1
]}

Feng Y.-P. ^{[1
]}

Cui J.-S. ^{[1
]}

Chen J. ^{[2
]}

Liu D.-X. ^{[1
]}

Shi W.-Y. ^{[2
]}

机构：

[1] School of Environmental Science and Engineering, Hebei University of Science and Technology, Shijiazhuang

[2] Shijiazhuang Meteorological Bureau, Shijiazhuang

来源：

Huanjing Kexue/Environmental Science | 2021年 / 42卷 / 06期

关键词：

Backward-trajectory(HYSPLIT); NO[!sub]2[!/sub; Ozone(O[!sub]3[!/sub]); Shijiazhuang; Volatile organic compounds(VOCs);

D O I：

10.13227/j.hjkx.202011090

中图分类号：

学科分类号：

摘要：

Ground-level O3, NO2, and meteorological (temperature, humidity, wind speed, precipitation, and sunshine duration) data from 18 counties in Shijiazhuang City from 2014 to 2017, and volatile organic compounds (VOCs) data for Summer 2017, were analyzed to explore the spatial patterns, evolution, influencing factors, and source apportionment of O3 and NO2 in Shijiazhuang City. Network analysis and inverse distance weighted (IDW) spatial autocorrelation and backward trajectories analyses were performed. The results indicate that O3 concentrations increased between 2014 and 2017, and monthly variations showed a unimodal trend. The typical period of peak O3 pollution (O3≥160 μg•m-3) was from May to September, characterized by high temperatures, low humidity, weak winds, and strong solar radiation. The O3 concentrations were negatively correlated with the NO2. Furthermore, O3 concentrations increased year-on-year since 2015 in main urban area, and the dominant pollutant type had changed from NO2 (2014 to 2016) to VOCs (2016 and 2017). However, the O3 concentration of county-areas limited by the VOCs. The main factors affecting O3 concentrations were industry, agriculture, economy, and population, and centers of O3 pollution associated with secondary industry appeared in the main urban areas of Shijiazhuang and Luancheng. Moreover, VOCs trajectories during the summer monitoring period were clustered in three source directions: (A) East-northeast, 26.67%; (B) Northwest-west, 43.33%; and (C) Southeast-south, 30%). Trajectories (A) and (C) were the dominant directions of VOC transmission (east-southeast). © 2021, Science Press. All right reserved.

引用

页码：2679 / 2690

页数：11

共 39 条

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