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

IF 2.8 2区 化学 Q3 CHEMISTRY, PHYSICAL The Journal of Physical Chemistry A Pub Date : 2025-03-27 Epub Date: 2025-03-13 DOI:10.1021/acs.jpca.5c00332
Jie Chen, George Wandera Kisimbiri, Ivan Gladich, Nicolas Fauré, Erik S Thomson, Robert Temperton, Zamin A Kanji, Xiangrui Kong
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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 (NH4)2SO4, 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 (NH4)2SO4 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 (NH4)2SO4 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 (NH4)2SO4 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 (NH4)2SO4 particle surfaces could be an active source of atmospheric BrC and SOA.

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含氮、含硫有机化合物在硫酸铵表面形成途径的研究。
含氮和含硫有机化合物(N-Org和S-Org)的形成对大气二次有机气溶胶(SOA)的产生至关重要,从而影响空气质量和全球气候。然而,由于表面敏感分析技术的有限可用性,人们对气溶胶颗粒表面上N-Org和S-Org形成的机制知之甚少。本研究利用大气压x射线光电子能谱(APXPS)、近边缘x射线吸收精细结构(NEXAFS)光谱和分子动力学(MD)模拟,研究了已知的SOA前体乙二醛(GL)与硫酸铵(NH4)2SO4在不同相对湿度(RH)条件下的表面相互作用。在低相对湿度(≤13.3%)条件下,在(NH4)2SO4表面发现了N-Org物质,如亚胺,这是棕色碳(BrC)形成的关键中间体。由于在XPS光谱中难以区分S-Org和无机硫酸盐,因此无法确定形成的S-Org种类。在整个探测深度上,(NH4)2SO4表面的元素比显示GL暴露后S/O和N/O比增加,表明N- org和S- org物质的形成。NEXAFS测量进一步证实了(NH4)2SO4的表面变化与GL和水的吸附有关。这些发现为表面驱动的N-Org和S-Org形成途径提供了令人信服的证据,表明(NH4)2SO4颗粒表面的非均相反应可能是大气BrC和SOA的活跃来源。
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来源期刊
The Journal of Physical Chemistry A
The Journal of Physical Chemistry A 化学-物理:原子、分子和化学物理
CiteScore
5.20
自引率
10.30%
发文量
922
审稿时长
1.3 months
期刊介绍: The Journal of Physical Chemistry A is devoted to reporting new and original experimental and theoretical basic research of interest to physical chemists, biophysical chemists, and chemical physicists.
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