Articles | Volume 19, issue 19
https://doi.org/10.5194/acp-19-12569-2019
https://doi.org/10.5194/acp-19-12569-2019
Research article
 | 
09 Oct 2019
Research article |  | 09 Oct 2019

Enhanced heterogeneous uptake of sulfur dioxide on mineral particles through modification of iron speciation during simulated cloud processing

Zhenzhen Wang, Tao Wang, Hongbo Fu, Liwu Zhang, Mingjin Tang, Christian George, Vicki H. Grassian, and Jianmin Chen

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Cited articles

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Andreae, M. O. and Rosenfeld, D.: Aerosol-cloud-precipitation interactions. Part 1. The nature and sources of cloud-active aerosols, Earth Sci. Rev., 89, 13–41, https://doi.org/10.1016/j.earscirev.2008.03.001, 2008. 
Baker, A. R. and Croot, P. L.: Atmospheric and marine controls on aerosol iron solubility in seawater, Mar. Chem., 120, 4–13, https://doi.org/10.1016/j.marchem.2008.09.003, 2010. 
Behra, P., Sigg, L., and Stumm, W.: Dominating influence of NH3 on the oxidation of aqueous SO2: the coupling of NH3 and SO2 in atmospheric water, Atmos. Environ., 23, 2691–2707, https://doi.org/10.1016/0004-6981(89)90549-0, 1989. 
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This study confirmed that SO2 uptake on mineral particles could be greatly enhanced during cloud processing. The large pH fluctuations between the cloud-aerosol modes could significantly modify the microphysical properties of particles, and triggered the formation of reactive Fe particles to accelerate sulfate formation via a self-amplifying process. Results of this study could partly explain the missing source of sulfate and improve agreement between models and field observations.
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