Published March 2025 | Version Published
Journal Article Open

Atmospheric sulfate aerosol formation enhanced by interfacial anions

  • 1. ROR icon East China Normal University
  • 2. ROR icon Guangdong University of Technology
  • 3. ROR icon Chinese Research Academy of Environmental Sciences
  • 4. ROR icon Harbin Institute of Technology
  • 5. ROR icon Stanford University
  • 6. ROR icon California Institute of Technology

Contributors

Abstract

Heterogeneous oxidation of SO2 by NO2 on aerosols has recently been found to be one of the major formation pathways of sulfate in the polluted troposphere, but the chemical mechanisms and kinetics remain uncertain. By combining lab experiments, theoretical chemistry calculations, and field measurements, here we show that the SO2 oxidation by NO2 is critically dependent on anions at the air–aerosol aqueous interface. The reaction rate of NO2 with HSO (1.1 × 108–1.6 × 109 M−1 s−1) is more than four orders of magnitude larger than the traditionally held value for the bulk phase due to the abundant occurrence of chloride, nitrate, and carboxylic anions at the air–aqueous interface, which remarkably accelerates sulfate formation during China haze periods by enhancing the uptake of NO2 through interfacial electrostatic attraction. Atmospheric models not accounting for this aerosol interfacial process likely produce major misrepresentations of tropospheric sulfate aerosols under polluted conditions.

Copyright and License

This is an Open Access article distributed under the terms of the Creative Commons Attribution License (https://creativecommons.org/licenses/by/4.0/), which permits unrestricted reuse, distribution, and reproduction in any medium, provided the original work is properly cited.

Funding

This work was financially supported by the National Natural Science Foundation of China (nos. 42130704 and U23A2030) and the National Key Research and Development Program of China (2023YFC3706302).

Contributions

G.W. conceived and designed the research. S.Z., X.X., S.G., and G.W. conducted the lab chamber experiments. S.Z., S.G., and G.W. analyzed the chamber experiment data. T.Z., H.S., and G.W. performed the theoretical chemistry calculation. J.G., Y.R., and H.L. collected the field samples. C.W. and G.W. analyzed the field observation data. G.W. wrote the paper. Other authors contributed to this work with useful discussions and comments.

G.W. and S.Z. contributed equally to this work.

Data Availability

The chamber experiments and field observation data are available at https://doi.org/10.5281/zenodo.14898280, while all other data can be found at the Supplementary material.

Supplemental Material

pgaf058_Supplementary_Data

Additional Information

This manuscript was posted as a preprint at: https://doi.org/10.21203/rs.3.rs-2230064/v1.

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Additional details

Additional titles

Alternative title
Atmospheric sulfate formation from SO₂ oxidation by NO₂ is enhanced by charges at the air-aqueous interface

Identifiers

Related works

Describes
Journal Article: PMC11880798 (PMCID)
Is new version of
Discussion Paper: 10.21203/rs.3.rs-2230064/v1 (DOI)
Is supplemented by
Dataset: 10.5281/zenodo.14898280 (DOI)

Funding

National Natural Science Foundation of China
42130704
National Natural Science Foundation of China
U23A2030
National Key R&D Plan, Ministry of Science and Technology of China
2023YFC3706302

Dates

Accepted
2025-02-10
Available
2025-02-24
Published
Available
2025-03-05
Corrected and typeset

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Caltech groups
Division of Chemistry and Chemical Engineering (CCE)
Publication Status
Published