Surface Formation Pathway of Nitrogen- and Sulfur-Containing Organic Compounds on Ammonium Sulfate

The formation of nitrogen- and sulfur-containing organic compounds (N-Org and S-Org) is important for atmospheric secondary organic aerosol (SOA) production, thereby influencing air quality and global climate. However, the mechanisms underlying N-Org and S-Org formation on aerosol particle surfaces are poorly understood due to the limited availability of surface-sensitive analytical techniques. This study investigates the surface interactions of glyoxal (GL), a known SOA precursor, with ammonium sulfate (NH<sub>4</sub>)<sub>2</sub>SO<sub>4</sub>, under varying relative humidity (RH) conditions, using ambient-pressure X-ray photoelectron spectroscopy (APXPS), near-edge X-ray absorption fine structure (NEXAFS) spectroscopy, and molecular dynamics (MD) simulations. N-Org species, such as imines, a key intermediate in brown carbon (BrC) formation, are identified on the (NH<sub>4</sub>)<sub>2</sub>SO<sub>4</sub> surface at low RH (≤13.3%). The formed S-Org species cannot be specified due to the difficulties in distinguishing S-Org from inorganic sulfate in the XPS spectra. Elemental ratios on (NH<sub>4</sub>)<sub>2</sub>SO<sub>4</sub> surface across the entire probing depth show increased S/O and N/O ratios upon GL exposure, indicating the formation of N-Org and S-Org species. NEXAFS measurements further confirm the surface changes of (NH<sub>4</sub>)<sub>2</sub>SO<sub>4</sub> associated with the adsorption of GL and water. These findings provide compelling evidence of surface-driven N-Org and S-Org formation pathways, demonstrating that heterogeneous reactions on (NH<sub>4</sub>)<sub>2</sub>SO<sub>4</sub> particle surfaces could be an active source of atmospheric BrC and SOA.

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Publication Details

Journal
The Journal of Physical Chemistry A
Published
2025-03-13
DOI
https://doi.org/10.1021/acs.jpca.5c00332
Citations
4
Primary Topic
Atmospheric chemistry and aerosols
Type
article
Field-Weighted Citation Impact
5.20

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article

Surface Formation Pathway of Nitrogen- and Sulfur-Containing Organic Compounds on Ammonium Sulfate

Nicolas Fauré, Zamin Abdulali Kanji, Ivan Gladich, Erik S. Thomson et al.
4 citations
The Journal of Physical Chemistry A
Atmospheric chemistry and aerosols
5.20
article

Surface Formation Pathway of Nitrogen- and Sulfur-Containing Organic Compounds on Ammonium Sulfate

Nicolas Fauré, Zamin Abdulali Kanji, Ivan Gladich, Erik S. Thomson, Robert H. Temperton, Xiangrui Kong, Jie Chen, George Wandera Kisimbiri
article en
4 citations

Abstract

The formation of nitrogen- and sulfur-containing organic compounds (N-Org and S-Org) is important for atmospheric secondary organic aerosol (SOA) production, thereby influencing air quality and global climate. However, the mechanisms underlying N-Org and S-Org formation on aerosol particle surfaces are poorly understood due to the limited availability of surface-sensitive analytical techniques. This study investigates the surface interactions of glyoxal (GL), a known SOA precursor, with ammonium sulfate (NH<sub>4</sub>)<sub>2</sub>SO<sub>4</sub>, under varying relative humidity (RH) conditions, using ambient-pressure X-ray photoelectron spectroscopy (APXPS), near-edge X-ray absorption fine structure (NEXAFS) spectroscopy, and molecular dynamics (MD) simulations. N-Org species, such as imines, a key intermediate in brown carbon (BrC) formation, are identified on the (NH<sub>4</sub>)<sub>2</sub>SO<sub>4</sub> surface at low RH (≤13.3%). The formed S-Org species cannot be specified due to the difficulties in distinguishing S-Org from inorganic sulfate in the XPS spectra. Elemental ratios on (NH<sub>4</sub>)<sub>2</sub>SO<sub>4</sub> surface across the entire probing depth show increased S/O and N/O ratios upon GL exposure, indicating the formation of N-Org and S-Org species. NEXAFS measurements further confirm the surface changes of (NH<sub>4</sub>)<sub>2</sub>SO<sub>4</sub> associated with the adsorption of GL and water. These findings provide compelling evidence of surface-driven N-Org and S-Org formation pathways, demonstrating that heterogeneous reactions on (NH<sub>4</sub>)<sub>2</sub>SO<sub>4</sub> particle surfaces could be an active source of atmospheric BrC and SOA.

The Journal of Physical Chemistry AVol. 129(12)
Lund University (SE), ETH Zurich (CH), Institute of Atmospheric Sciences and Climate (IT), MAX IV Laboratory (SE), European Centre for Living Technology (IT), Hamad bin Khalifa University (QA), University of Gothenburg (SE), Qatar Foundation (QA)
Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung, Swedish Foundation for International Cooperation in Research and Higher Education, VINNOVA, Svenska Forskningsrådet Formas, Carl Tryggers Stiftelse för Vetenskaplig Forskning, Vetenskapsrådet
Openalex Percentile: Top 5%
Atmospheric chemistry and aerosols
5.20
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