Assessing the importance of nitric acid and ammonia for particle growth in the polluted boundary layer†

IF 2.8 Q3 ENVIRONMENTAL SCIENCES Environmental science: atmospheres Pub Date : 2024-01-25 DOI:10.1039/D3EA00001J
Ruby Marten, Mao Xiao, Mingyi Wang, Weimeng Kong, Xu-Cheng He, Dominik Stolzenburg, Joschka Pfeifer, Guillaume Marie, Dongyu S. Wang, Miriam Elser, Andrea Baccarini, Chuan Ping Lee, Antonio Amorim, Rima Baalbaki, David M. Bell, Barbara Bertozzi, Lucía Caudillo, Lubna Dada, Jonathan Duplissy, Henning Finkenzeller, Martin Heinritzi, Markus Lampimäki, Katrianne Lehtipalo, Hanna E. Manninen, Bernhard Mentler, Antti Onnela, Tuukka Petäjä, Maxim Philippov, Birte Rörup, Wiebke Scholz, Jiali Shen, Yee Jun Tham, António Tomé, Andrea C. Wagner, Stefan K. Weber, Marcel Zauner-Wieczorek, Joachim Curtius, Markku Kulmala, Rainer Volkamer, Douglas R. Worsnop, Josef Dommen, Richard C. Flagan, Jasper Kirkby, Neil McPherson Donahue, Houssni Lamkaddam, Urs Baltensperger and Imad El Haddad
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Abstract

Aerosols formed and grown by gas-to-particle processes are a major contributor to smog and haze in megacities, despite the competition between growth and loss rates. Rapid growth rates from ammonium nitrate formation have the potential to sustain particle number in typical urban polluted conditions. This process requires supersaturation of gas-phase ammonia and nitric acid with respect to ammonium nitrate saturation ratios. Urban environments are inhomogeneous. In the troposphere, vertical mixing is fast, and aerosols may experience rapidly changing temperatures. In areas close to sources of pollution, gas-phase concentrations can also be highly variable. In this work we present results from nucleation experiments at −10 °C and 5 °C in the CLOUD chamber at CERN. We verify, using a kinetic model, how long supersaturation is likely to be sustained under urban conditions with temperature and concentration inhomogeneities, and the impact it may have on the particle size distribution. We show that rapid and strong temperature changes of 1 °C min−1 are needed to cause rapid growth of nanoparticles through ammonium nitrate formation. Furthermore, inhomogeneous emissions of ammonia in cities may also cause rapid growth of particles.

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评估硝酸和氨对污染边界层中颗粒物生长的重要性†。
尽管生长率和损耗率之间存在竞争,但气体到颗粒过程形成和生长的气溶胶是造成大城市烟雾和灰霾的主要因素。在典型的城市污染条件下,硝酸铵形成的快速增长速率有可能维持颗粒数量。这一过程需要气相氨和硝酸相对于硝酸铵饱和比的过饱和度。城市环境是不均匀的。在对流层中,垂直混合速度很快,气溶胶可能会经历快速变化的温度。在靠近污染源的地区,气相浓度也可能变化很大。在这项工作中,我们介绍了在欧洲核子研究中心的 CLOUD 实验室中进行的-10 °C和5 °C成核实验的结果。我们利用动力学模型验证了在温度和浓度不均匀的城市条件下,过饱和可能会持续多长时间,以及过饱和对粒径分布可能产生的影响。我们的研究表明,需要 1 °C min-1 的快速而强烈的温度变化,才能通过硝酸铵的形成导致纳米颗粒的快速增长。此外,城市中氨气的不均匀排放也可能导致颗粒的快速增长。
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