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High-molecular-weight esters in α-pinene ozonolysis secondary organic aerosol: Structural characterization and mechanistic proposal for their formation from highly oxygenated molecules

机译:α-pine烯臭氧分解二次有机气溶胶中的高分子量酯:由高氧分子形成的结构表征和机理建议

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Stable high-molecular-weight esters are present in α-pinene ozonolysis secondary organic aerosol (SOA) with the two most abundant ones corresponding to a diaterpenylic ester of cis-pinic acid with a molecular weight (MW) of 368 C19H28O7) and a hydroxypinonyl ester of cis-pinic acid with a MW of 358 (C17H26O8). However, their molecular structures are not completely elucidated and their relationship with highly oxygenated molecules (HOMs) in the gas phase is still unclear. In this study, liquid chromatography in combination with positive ion electrospray ionization mass spectrometry has been performed on high-molecular-weight esters present in α-pinene/O3 SOA with and without derivatization into methyl esters. Unambiguous evidence could be obtained for the molecular structure of the MW 368 ester in that it corresponds to an ester of cis-pinic acid where the carboxyl substituent of the dimethylcyclobutane ring and not the methylcarboxyl substituent is esterified with 7-hydroxypinonic acid. The same linkage was already proposed in previous work for the MW 358 ester (Yasmeen et al., 2010), but could be supported in the present study. Guided by the molecular structures of these stable esters, we propose a formation mechanism from gas-phase HOMs that takes into account the formation of an unstable C19H28O11 product, which is detected as a major species in α-pinene ozonolysis experiments as well as in the pristine forest atmosphere by chemical ionization – atmospheric pressure ionization – time-of-flight mass spectrometry with nitrate clustering (Ehn et al., 2012, 2014). It is suggested that an acyl peroxy radical related to cis-pinic acid (RO2?) and an alkoxy radical related to 7- or 5-hydroxypinonic acid (R'O?) serve as key gas-phase radicals and combine according to a RO2??+?R'O??→?RO3R' radical termination reaction. Subsequently, the unstable C19H28O1119H28O7 (MW 368) and C17H26O8 (MW 358), respectively. The proposed mechanism is supported by several observations reported in the literature. On the basis of the indirect evidence presented in this study, we hypothesize that RO2??+?R'O??→?RO3R; chemistry is at the underlying molecular basis of high-molecular-weight ester formation upon α-pinene ozonolysis and may thus be of importance for new particle formation and growth in pristine forested environments.
机译:稳定的高分子量酯存在于α-pine烯臭氧分解二次有机气溶胶(SOA)中,两种最丰富的酯分别对应于分子量(MW)为368 C19H28O7的顺式松香酸的二戊烯基酯和羟基松香酰基分子量为358的顺式-顺式乙酸酯(C17H26O8)。但是,它们的分子结构尚未完全阐明,它们与气相中高氧分子(HOMs)的关系仍不清楚。在这项研究中,已经对存在于α-pine烯/ O3 SOA中的高分子量酯进行了液相色谱结合正离子电喷雾电离质谱的研究,有无衍生化成甲酯。对于MW 368酯的分子结构,可以获得明确的证据,因为它对应于顺式-松酸的酯,其中二甲基环丁烷环的羧基取代基而不是甲基-羧基取代基被7-羟基松酸酯化。在以前的工作中已经为MW 358酯提出了相同的联系(Yasmeen等人,2010),但在本研究中可能得到支持。根据这些稳定酯的分子结构,我们提出了一种由气相HOMs形成的机制,其中考虑到了不稳定的C19H28O11产物的形成,该产物在α-烯臭氧分解实验以及通过化学电离–大气压力电离–具有硝酸盐簇的飞行时间质谱法对原始森林大气进行分析(Ehn等,2012,2014)。建议与顺式-pinic酸(RO2′)有关的酰基过氧自由基和与7-或5-羟基己酸(R′O2)有关的烷氧基作为关键的气相自由基,并根据RO2进行结合。 ?? +?R'O ??→?RO3R'自由基终止反应。随后,不稳定的C19H28O1119H28O7(MW 368)和C17H26O8(MW 358)分别出现。所提出的机制得到了文献报道的一些观察的支持。根据本研究提出的间接证据,我们假设RO2α+ ΔR′Oβ→ΔRO3R;化学是α-pine烯臭氧分解时形成高分子量酯的基本分子基础,因此对于原始森林环境中新颗粒的形成和生长可能具有重要意义。

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