Bready Conor J, Sorescu Alexandra E, Glick Caroline S, Shields George C
Department of Chemistry, Furman University, 3300 Poinsett Highway, Greenville, South Carolina 29613, United States.
ACS Omega. 2025 Jun 6;10(23):24811-24831. doi: 10.1021/acsomega.5c01981. eCollection 2025 Jun 17.
A central question in the formation of secondary aerosols is whether organic molecules participate in the formation of prenucleation clusters or are they only adsorbed after formation of larger aerosols? The difficulty in understanding the role of organic molecules in aerosol formation is that there are very few studies of prenucleation clusters produced from various organics and sulfuric acid, so it is uncertain whether organic compounds form prenucleation clusters. Isoprene is the most abundant volatile biogenic organic compound (VOC) emitted into the atmosphere, accounting for about 70% of biogenic VOC emissions, excluding methane. Each year, approximately 600 teragrams of isoprene enter the atmosphere, primarily from natural sources like vegetation. This makes it a significant component of atmospheric organic molecules, much more prevalent than other VOCs emitted by plants or anthropogenic activities. Photooxidation of isoprene produces the diastereomeric tetrols, 2-methylthreitol and 2-methylerythritol, which contain four hydroxyl groups. We completed a comprehensive conformational search of both tetrols, and extensively explored the potential energy surfaces of these tetrols complexed with sulfuric acid and water. We report the vast ensemble of structures that are within 1 kcal/mol of the DLPNO-CCSD-(T)/CBS//ωB97X-D/6-31++G** minimum for each system. These high level Δ° values for each system were used to estimate the concentrations of all the possible complexes from these molecules in the lower troposphere. At the upper limit of tetrol concentration, we find that the two diastereomers will bind to one to three water molecules in high concentrations. However, formation of sulfuric acid-tetrol-water complexes lead to lower concentrations, leading us to suggest that these tetrols are unlikely to be involved in the formation of prenucleation clusters that will lead to further aerosol growth. Researchers should continue the search for organic molecules that lead to prenucleation.
二次气溶胶形成过程中的一个核心问题是有机分子是参与预成核团簇的形成,还是仅在较大气溶胶形成后才被吸附?理解有机分子在气溶胶形成中作用的困难在于,对由各种有机物和硫酸产生的预成核团簇的研究非常少,因此不确定有机化合物是否形成预成核团簇。异戊二烯是排放到大气中的最丰富的挥发性生物源有机化合物(VOC),占生物源VOC排放的约70%(不包括甲烷)。每年约有600太克异戊二烯进入大气,主要来自植被等自然源。这使其成为大气有机分子的重要组成部分,比植物或人为活动排放的其他VOC更为普遍。异戊二烯的光氧化产生非对映体四醇,即2-甲基苏糖醇和2-甲基赤藓糖醇,它们含有四个羟基。我们完成了对这两种四醇的全面构象搜索,并广泛探索了这些四醇与硫酸和水络合的势能面。我们报告了每个系统在DLPNO-CCSD-(T)/CBS//ωB97X-D/6-31++G**最小值1千卡/摩尔范围内的大量结构集合。每个系统的这些高水平Δ°值用于估计对流层下部这些分子所有可能络合物的浓度。在四醇浓度上限时,我们发现这两种非对映体将在高浓度下与一到三个水分子结合。然而,硫酸 - 四醇 - 水络合物的形成导致浓度降低,这使我们认为这些四醇不太可能参与导致进一步气溶胶生长的预成核团簇的形成。研究人员应继续寻找导致预成核的有机分子。