乙二醛和乙醇醛在水溶液气溶胶模拟物中的交叉反应:对褐碳产物形成的影响

Brian P. Henesey, Stephanie M. Ingwer, Hope S. Tracey, Elizabeth G. Obarow, Rachael E. Holappa, Adelaide M. King, Heidi P. Hendrickson, Daniel R. Griffith and Melissa M. Galloway*, 
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引用次数: 0

摘要

棕色碳(BrC)在含水大气气溶胶中的形成是有充分文献记载的,通常归因于醛-氨反应。然而,许多研究都集中在单个醛前体上,忽视了有机气溶胶的复杂组成,有机气溶胶由多种有机和无机化合物组成。为了解决这个问题,通过生成含有乙二醛(Gly)、乙醇醛(GAld)和硫酸铵的含水大气气溶胶模拟物,研究了一个复杂的BrC系统。超临界液相色谱-质谱(SFC-MS)结构分析表明,调整Gly:GAld摩尔比会导致BrC产物的组成和丰度发生变化。值得注意的是,芳香杂环(例如咪唑和吡嗪)以及无环羰基低聚物被鉴定为在不同浓度下形成,这取决于Gly: gld摩尔比。紫外可见光谱分析表明,这些混合Gly + GAld + AS体系的光吸收不能用Gly:GAld摩尔比的简单加权平均值来建模;观察到的光吸收变化可以用溶液成分的变化来解释。这些观察结果表明,溶液中的Gly和gld之间正在发生交叉反应,可能导致气溶胶物理性质的变化。鉴于在大气气溶胶中发现的数千种活性化合物,这些发现可能对我们理解气溶胶中的有机反应具有重要意义。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Cross-Reactions of Glyoxal and Glycolaldehyde in Aqueous Aerosol Mimics: Implications for Brown Carbon Product Formation

Cross-Reactions of Glyoxal and Glycolaldehyde in Aqueous Aerosol Mimics: Implications for Brown Carbon Product Formation

The formation of brown carbon (BrC) in aqueous atmospheric aerosols is well-documented and often attributed to aldehyde-ammonia reactions. However, many studies have focused on individual aldehyde precursors, overlooking the complex composition of organic aerosols, which comprise a diverse mix of organic and inorganic compounds. To address this, a complex BrC system was investigated by generating aqueous atmospheric aerosol mimics containing glyoxal (Gly), glycolaldehyde (GAld), and ammonium sulfate. Structural analysis using supercritical fluid chromatography–mass spectrometry (SFC-MS) showed that adjusting the Gly:GAld mole ratio leads to variations in the composition and abundance of BrC products formed. Notably, aromatic heterocycles (e.g., imidazoles and pyrazines) as well as acyclic carbonyl oligomers were identified to form at different concentrations depending on the Gly:GAld mole ratio. UV–visible spectroscopy analysis demonstrated that light absorption in these mixed Gly + GAld + AS systems cannot be modeled as a simple weighted average of the Gly:GAld mole ratio; observed changes in light absorbance can be explained by compositional changes in solution. These observations indicate that cross-reactions are occurring between the Gly and GAld in solution, potentially leading to changes in the physical properties of the aerosol. Given the thousands of reactive compounds found in atmospheric aerosol, these findings could have important implications for our understanding of organic reactions within the aerosol.

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