Surface FormationPathway of Nitrogen- and Sulfur-ContainingOrganic 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.

Publication Details

Journal
Figshare
Published
2025-03-13
DOI
https://doi.org/10.1021/acs.jpca.5c00332.s001
Primary Topic
Atmospheric chemistry and aerosols
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article
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article

Surface FormationPathway of Nitrogen- and Sulfur-ContainingOrganic Compounds on Ammonium Sulfate

Figshare
Atmospheric chemistry and aerosols
article

Surface FormationPathway of Nitrogen- and Sulfur-ContainingOrganic Compounds on Ammonium Sulfate

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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.

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