Abstract
Chlorine atoms (Cl) are highly reactive and can strongly influence the abundances of climate and air quality-relevant trace gases. Despite extensive research on molecular chlorine (Cl2), a Cl precursor, in the polar atmosphere, its sources in other regions are still poorly understood. Here we report the daytime Cl2 concentrations of up to 1 ppbv observed in a coastal area of Hong Kong, revealing a large daytime source of Cl2 (2.7 pptv s−1 at noon). Field and laboratory experiments indicate that photodissociation of particulate nitrate by sunlight under acidic conditions (pH < 3.0) can activate chloride and account for the observed daytime Cl2 production. The high Cl2 concentrations significantly increased atmospheric oxidation. Given the ubiquitous existence of chloride, nitrate, and acidic aerosols, we propose that nitrate photolysis is a significant daytime chlorine source globally. This so far unaccounted for source of chlorine can have substantial impacts on atmospheric chemistry.
Original language | English |
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Article number | 939 |
Journal | Nature Communications |
Volume | 13 |
Issue number | 1 |
DOIs | |
State | Published - Dec 2022 |
Externally published | Yes |
Funding
We thank the Hong Kong Environmental Protection Department for providing space at its supersite for our field measurements and for the provision of some VOCs and aerosol composition data. We thank Chung Hon Larry Suen for the help in the field measurements. We thank Bobo Wang, W.S. Lam, Yanlin Zhang, and Prof. Wei Chu for their help in the laboratory experiments. This research is supported by the Hong Kong Research Grants Council (T24-504/17-N and A-PolyU502/16 to T.W.), the Agence Nationale de la Recherche (ANR-16-CE01-0013 to C.G.), the Swedish Research Council (2013-6917 to M.H. and C.M.S), and the European Research Council Executive Agency under the European Union s Horizon 2020 Research and Innovation programme (Project ‘ERC-2016-COG726349 CLIMAHAL’ to Q.L. and A.S-L.). We thank the Hong Kong Environmental Protection Department for providing space at its supersite for our field measurements and for the provision of some VOCs and aerosol composition data. We thank Chung Hon Larry Suen for the help in the field measurements. We thank Bobo Wang, W.S. Lam, Yanlin Zhang, and Prof. Wei Chu for their help in the laboratory experiments. This research is supported by the Hong Kong Research Grants Council (T24-504/17-N and A-PolyU502/16 to T.W.), the Agence Nationale de la Recherche (ANR-16-CE01-0013 to C.G.), the Swedish Research Council (2013-6917 to M.H. and C.M.S), and the European Research Council Executive Agency under the European Union s Horizon 2020 Research and Innovation programme (Project ‘ERC-2016-COG726349 CLIMAHAL’ to Q.L. and A.S-L.).