Articles | Volume 19, issue 7
https://doi.org/10.5194/acp-19-5033-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Special issue:
https://doi.org/10.5194/acp-19-5033-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
New particle formation from sulfuric acid and ammonia: nucleation and growth model based on thermodynamics derived from CLOUD measurements for a wide range of conditions
Andreas Kürten
CORRESPONDING AUTHOR
Institute for Atmospheric and Environmental Sciences, Goethe University
Frankfurt, 60438 Frankfurt am Main, Germany
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- Boundary layer versus free tropospheric submicron particle formation: A case study from NASA DC-8 observations in the Asian continental outflow during the KORUS-AQ campaign D. Park et al. 10.1016/j.atmosres.2021.105857
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- Structural Diversity of Protonated Citric Acid-Ammonia Clusters and Its Atmospheric Implication S. Zhou et al. 10.1021/acs.jpca.3c05160
- Exploring the hydrogen-bonded interactions of vanillic acid with atmospheric bases: a DFT study T. de Oliveira et al. 10.1007/s11224-024-02307-3
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- Reduction of anthropogenic emissions enhanced atmospheric new particle formation: Observational evidence during the Beijing 2022 Winter Olympics W. Zhu et al. 10.1016/j.atmosenv.2023.120094
- Evidence of nitrate-based nighttime atmospheric nucleation driven by marine microorganisms in the South Pacific G. Chamba et al. 10.1073/pnas.2308696120
- Potential enhancement in atmospheric new particle formation by amine-assisted nitric acid condensation at room temperature K. Chen et al. 10.1016/j.atmosenv.2022.119252
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Short summary
New particle formation and growth are important processes affecting climate and air quality. A significant fraction of newly formed particles originates from sulfuric acid, water, and ammonia. The present study introduces a new process model for the calculation of aerosol nucleation and growth rates for the sulfuric acid–ammonia system. The thermodynamic parameters enabling these calculations are derived from laboratory (CLOUD chamber) measurements.
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