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城市北京新粒子形成和增长的季节性特征。

Seasonal Characteristics of New Particle Formation and Growth in Urban Beijing.

机构信息

State Key Joint Laboratory of Environment Simulation and Pollution Control, School of Environment, Tsinghua University, 100084 Beijing, China.

Institute for Atmospheric and Earth System Research Physics, Faculty of Science, University of Helsinki, 00014 Helsinki, Finland.

出版信息

Environ Sci Technol. 2020 Jul 21;54(14):8547-8557. doi: 10.1021/acs.est.0c00808. Epub 2020 Jul 1.

Abstract

Understanding the atmospheric new particle formation (NPF) process within the global range is important for revealing the budget of atmospheric aerosols and their impacts. We investigated the seasonal characteristics of NPF in the urban environment of Beijing. Aerosol size distributions down to ∼1 nm and HSO concentration were measured during 2018-2019. The observed formation rate of 1.5 nm particles () is significantly higher than those in the clean environment, e.g., Hyytiälä, whereas the growth rate is not significantly different. Both and NPF frequency in urban Beijing show a clear seasonal variation with maxima in winter and minima in summer, while the observed growth rates are generally within the same range around the year. We show that ambient temperature is a governing factor driving the seasonal variation of . In contrast, the condensation sink and the daily maximum HSO concentration show no significant seasonal variation during the NPF periods. In all four seasons, condensation of HSO and (HSO)(amine) clusters contributes significantly to the growth rates in the sub-3 nm size range, whereas it is less important for the observed growth rates of particles above 3 nm. Therefore, other species are always needed for the growth of larger particles.

摘要

了解全球范围内大气中新粒子形成(NPF)的过程对于揭示大气气溶胶的预算及其影响非常重要。我们研究了北京城市环境中 NPF 的季节性特征。在 2018-2019 年期间,我们测量了气溶胶的大小分布直至约 1nm 以及 HSO 浓度。观测到的 1.5nm 颗粒的形成速率()明显高于例如 Hyytiälä 等清洁环境中的速率,而生长速率则没有明显差异。城市北京的和 NPF 频率都表现出明显的季节性变化,冬季最高,夏季最低,而观测到的生长速率在一年中通常处于相同范围内。我们表明环境温度是驱动形成季节性变化的主要因素。相比之下,在 NPF 期间,凝结阱和每日最大 HSO 浓度没有明显的季节性变化。在所有四个季节中,HSO 和(HSO)(胺)簇的凝结对亚 3nm 尺寸范围内的生长速率有重要贡献,而对观测到的 3nm 以上颗粒的生长速率则不太重要。因此,对于较大颗粒的生长,总是需要其他物质。

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