气溶胶
成核
粒子(生态学)
白天
粒子数
硫酸
航程(航空)
分析化学(期刊)
大气科学
环境化学
环境科学
材料科学
化学
气象学
物理
等离子体
无机化学
地质学
海洋学
有机化学
量子力学
复合材料
作者
Liangduo Chen,Ximeng Qi,Guangdong Niu,Yuanyuan Li,Chong Liu,Shiyi Lai,Wei Nie,Wei Nie,Chao Yan,Jiaping Wang,Xuguang Chi,Pauli Paasonen,Tareq Hussein,Katrianne Lehtipalo,Veli‐Matti Kerminen,Tuukka Petäj̈ä,Markku Kulmala,Aijun Ding
摘要
Abstract Observations of atmospheric sub‐3 nm particles are essential for understanding the initial stages of new particle formation (NPF) and the origin of aerosol particles. In this study, 3 years (2018–2020) of measurements of sub‐3 nm particles were conducted in the Yangtze River Delta (YRD) of eastern China. High concentrations of sub‐3 nm particles were observed, with number concentration in the range from 10 3 to 10 6 cm −3 . During the daytime, the sub‐3 nm particle concentration was found to peak at around the noon, indicating strong photochemical nucleation processes. The formation rates of sub‐3 nm particles were high during the NPF event days, with an average value of 86 cm −3 s −1 , and this rate was related to the sulfuric acid (SA) concentration. The particle growth rates below 3 nm were about 1–2 nm h −1 , much lower than the growth rates of larger particles. At nighttime, sub‐3 nm particle concentrations remained relatively high (3 × 10 3 to 1.2 × 10 4 cm −3 ) and were related to the NO x concentration, suggesting traffic emission to be a significant source. The sub‐3 nm proxy was developed to estimate the contributions of NPF and traffic emission. During the daytime, 74.8% and 12.4% of the sub‐3 nm particles were estimated to originate from SA‐driven NPF and traffic emissions, respectively. However, other sources were estimated to contribute 61.8% of sub‐3 nm particles at nighttime, suggesting the formation mechanisms of sub‐3 nm particles are still unclear in this environment. Our study sheds more light on the characteristics and sources of sub‐3 nm particles in polluted environments.
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