School of Energy and Environment, City University of Hong Kong, Tat Chee Avenue, Kowloon, Hong Kong, China.
Faculty of Frontier Engineering, Institute of Science and Engineering, Kanazawa University, Kakuma-machi, Kanazawa 920-1192, Japan.
Environ Sci Technol. 2021 May 4;55(9):5711-5720. doi: 10.1021/acs.est.0c08199. Epub 2021 Apr 16.
Particulate nitrate photolysis can produce oxidants (i.e., OH, NO, and NO/HNO) in aqueous droplets and may play a potential role in increased atmospheric oxidative capacity. Our earlier works have reported on the SO oxidation promoted by nitrate photolysis to produce sulfate. Here, we used glyoxal as a model precursor to examine the role of particulate nitrate photolysis in the formation of secondary organic aerosol (SOA) from particle-phase oxidation of glyoxal by OH radicals. Particles containing sodium nitrate and glyoxal were irradiated at 300 nm. Interestingly, typical oxidation products of oxalic acid, glyoxylic acid, and higher-molecular-weight products reported in the literature were not found in the photooxidation process of glyoxal during nitrate photolysis in the particle phase. Instead, formic acid/formate production was found as the main oxidation product. At glyoxal concentration higher than 3 M, we found that the formic acid/formate production rate increases significantly with increasing glyoxal concentration. Such results suggest that oxidation of glyoxal at high concentrations by OH radicals produced from nitrate photolysis in aqueous particles may not contribute significantly to SOA formation since formic acid is a volatile species. Furthermore, recent predictions of formic acid/formate concentration from the most advanced chemical models are lower than ambient observations at both the ground level and high altitude. The present study reveals a new insight into the production of formic acid/formate as well as a sink of glyoxal in the atmosphere, which may partially narrow the gap between model predictions and field measurements in both species.
颗粒态硝酸盐光解可以在水相液滴中产生氧化剂(例如 OH、NO 和 NO/HNO),并可能在增加大气氧化性方面发挥潜在作用。我们之前的工作已经报道了硝酸盐光解促进 SO 氧化生成硫酸盐。在这里,我们使用乙二醛作为模型前体,考察了颗粒态硝酸盐光解在 OH 自由基引发的乙二醛颗粒相氧化生成二次有机气溶胶(SOA)过程中的作用。含有硝酸钠和乙二醛的颗粒在 300nm 下进行辐照。有趣的是,在颗粒相中硝酸盐光解的乙二醛光氧化过程中,并未发现文献中报道的草酸、乙醛酸和高分子量产物等典型的氧化产物。相反,发现甲酸/甲酸盐的生成是主要的氧化产物。在乙二醛浓度高于 3M 时,我们发现甲酸/甲酸盐的生成速率随着乙二醛浓度的增加而显著增加。这些结果表明,由水相颗粒中硝酸盐光解产生的 OH 自由基氧化高浓度的乙二醛可能不会显著促进 SOA 的形成,因为甲酸是一种挥发性物质。此外,最近最先进的化学模型对甲酸/甲酸盐浓度的预测低于地面和高空的环境观测值。本研究揭示了在大气中甲酸/甲酸盐生成以及乙二醛消耗的新见解,这可能部分缩小了这两种物质在模型预测和现场测量之间的差距。