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Chemical characteristics and source apportionment of PM2.5 using PMF modelling coupled with 1-hr resolution online air pollutant dataset for Linfen, China

薄雾 煤燃烧产物 气溶胶 生物质燃烧 环境科学 环境化学 总有机碳 污染物 分摊 空气质量指数 大气科学 硫酸盐 硝酸盐 空气污染 化学 燃烧 微粒 污染 碳纤维 早晨 气象学 季节性 生物量(生态学) 环境工程 排放清单 时间分辨率 化学输运模型
作者
Yafei Li,Baoshuang Liu,Zhigang Xue,Yufen Zhang,Xiaoyun Sun,Congbo Song,Qili Dai,Ruichen Fu,Yonggang Tai,Jinyu Gao,Yajun Zheng,Yinchang Feng
出处
期刊:Environmental Pollution [Elsevier]
卷期号:263 (Pt B): 114532-114532 被引量:55
标识
DOI:10.1016/j.envpol.2020.114532
摘要

The chemical species in PM2.5 and air pollutant concentration data with 1-hr resolution were monitored synchronously between 15 November 2018 and 20 January 2019 in Linfen, China, which were analysed for multiple temporal patterns, and PM2.5 source apportionment using positive matrix factorisation (PMF) modelling coupled with online chemical species data was conducted to obtain the apportionment results of distinct temporal patterns. The mean concentration of PM2.5 was 124 μg/m3 during the heating period, and NO3− and organic carbon (OC) were the dominant species. The concentrations and percentages of NO3−, SO42−, and OC increased notably during the growth periods of haze events, thereby indicating secondary particle formation. Six factors were identified by the PMF model during the heating period, including vehicular emissions (VE: 26.5%), secondary nitrate (SN: 16.5%), coal combustion and industrial emissions (CC&IE: 25.7%), secondary sulfate and secondary organic carbon (SS&SOC: 24.4%), biomass burning (BB: 1.0%), and crustal dust (CD: 5.9%). The primary sources of PM2.5 on clean days were CD (33.3%), VE (23.1%), and SS&SOC (20.6%), while they were CC&IE (32.9%) and SS&SOC (28.3%) during the haze events. The contributions of secondary sources and CC&IE increased rapidly during the growth periods of haze events, while that of CD increased during the dissipation period. Diurnal variations in the contribution of secondary sources were mainly related to the accumulation and transformation of corresponding gaseous precursors. In comparison, contributions of CC&IE and VE varied as a function of the domestic heating load and peak levels occurred during the morning and evening rush hours. High contributions of major sources (CC&IE and SS&SOC) during haze events originated mainly from the north and south, while high contribution of a major source (CD) on clean days was from the northwest.
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