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Acylperoxy Radicals as Key Intermediates in the Formation of Dimeric Compounds in α-Pinene Secondary Organic Aerosol
Environmental Science & Technology ( IF 10.8 ) Pub Date : 2022-09-30 , DOI: 10.1021/acs.est.2c02090
Yue Zhao 1 , Min Yao 1 , Yingqi Wang 1 , Ziyue Li 1 , Shunyao Wang 1 , Chenxi Li 1 , Huayun Xiao 1
Affiliation  

High molecular weight dimeric compounds constitute a significant fraction of secondary organic aerosol (SOA) and have profound impacts on the properties and lifecycle of particles in the atmosphere. Although different formation mechanisms involving reactive intermediates and/or closed-shell monomeric species have been proposed for the particle-phase dimers, their relative importance remains in debate. Here, we report unambiguous experimental evidence of the important role of acyl organic peroxy radicals (RO2) and a small but non-negligible contribution from stabilized Criegee intermediates (SCIs) in the formation of particle-phase dimers during ozonolysis of α-pinene, one of the most important precursors for biogenic SOA. Specifically, we find that acyl RO2-involved reactions explain 50–80% of total oxygenated dimer signals (C15–C20, O/C ≥ 0.4) and 20–30% of the total less oxygenated (O/C < 0.4) dimer signals. In particular, they contribute to 70% of C15–C19 dimer ester formation, likely mainly via the decarboxylation of diacyl peroxides arising from acyl RO2 cross-reactions. In comparison, SCIs play a minor role in the formation of C15–C19 dimer esters but react noticeably with the most abundant C9 and C10 carboxylic acids and/or carbonyl products to form C19 and C20 dimeric peroxides, which are prone to particle-phase transformation to form more stable dimers without the peroxide functionality. This work provides a clearer view of the formation pathways of particle-phase dimers from α-pinene oxidation and would help reduce the uncertainties in future atmospheric modeling of the budget, properties, and health and climate impacts of SOA.

中文翻译:

酰基过氧自由基作为 α-蒎烯二级有机气溶胶中二聚化合物形成的关键中间体

高分子量二聚化合物构成二次有机气溶胶 (SOA) 的重要组成部分,并对大气中颗粒的性质和生命周期产生深远影响。尽管已经为颗粒相二聚体提出了涉及反应性中间体和/或闭壳单体种类的不同形成机制,但它们的相对重要性仍然存在争议。在这里,我们报告了酰基有机过氧自由基 (RO 2 )的重要作用的明确实验证据,以及稳定的 Criegee 中间体 (SCI) 在 α-蒎烯臭氧分解过程中颗粒相二聚体形成中的小但不可忽略的贡献,生物源 SOA 最重要的先驱之一。具体来说,我们发现酰基 RO 2- 涉及的反应解释了总氧化二聚体信号的 50-80%(C 15 –C 20,O/C ≥ 0.4)和总氧化较少(O/C < 0.4)二聚体信号的 20-30%。特别是,它们有助于 70% 的 C 15 -C 19二聚酯形成,可能主要是通过由酰基 RO 2交叉反应产生的二酰基过氧化物的脱羧。相比之下,SCI 在 C 15 -C 19 二聚酯的形成中起次要作用,但与最丰富的 C 9和 C 10羧酸和/或羰基产物反应形成 C 19和 C 20二聚过氧化物,易于发生颗粒相变以形成更稳定的二聚体,而没有过氧化物官能团。这项工作为 α-蒎烯氧化形成颗粒相二聚体的途径提供了一个更清晰的视角,并将有助于减少未来大气建模中 SOA 的预算、性质、健康和气候影响的不确定性。
更新日期:2022-09-30
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