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首页> 外文期刊>Atmospheric chemistry and physics >Secondary organic aerosol formation from the photooxidation of isoprene, 1,3-butadiene, and 2,3-dimethyl-1,3-butadiene under high NOsubx/sub conditions
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Secondary organic aerosol formation from the photooxidation of isoprene, 1,3-butadiene, and 2,3-dimethyl-1,3-butadiene under high NOsubx/sub conditions

机译:在高NO x 条件下异戊二烯,1,3-丁二烯和2,3-二甲基-1,3-丁二烯的光氧化形成次生有机气溶胶

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Secondary organic aerosol (SOA) formation from atmospheric oxidation ofisoprene has been the subject of multiple studies in recent years; however,reactions of other conjugated dienes emitted from anthropogenic sourcesremain poorly understood. SOA formation from the photooxidation of isoprene,isoprene-1-13C, 1,3-butadiene, and 2,3-dimethyl-1,3-butadiene isinvestigated for high NOx conditions. The SOA yield measured in the1,3-butadiene/NOx/H2O2 irradiation system (0.089–0.178) wasclose to or slightly higher than that measured with isoprene under similarNOx conditions (0.077–0.103), suggesting that the photooxidation of1,3-butadiene is a possible source of SOA in urban air. In contrast, a verysmall amount of SOA particles was produced in experiments with2,3-dimethyl-1,3-butadiene. Off-line liquid chromatography – massspectrometry analysis revealed that the signals of oligoesters comprise amajor fraction (0.10–0.33) of the signals of the SOA products observed fromall dienes investigated. The oligoesters originate from the unsaturatedaldehyde gas phase diene reaction products; namely, semi-volatile compounds producedby the oxidation of the unsaturated aldehyde undergo particle-phaseoligoester formation. Oligoesters produced by the dehydration reactionbetween nitrooxypolyol and 2-methylglyceric acid monomer or its oligomerwere also characterized in these experiments with isoprene as the startingdiene. These oligomers are possible sources of the 2-methyltetrols found inambient aerosol samples collected under high NOx conditions.Furthermore, in low-temperature experiments also conducted in this study,the SOA yield measured with isoprene at 278 K was 2–3 times as high as thatmeasured at 300 K under similar concentration conditions. Althougholigomerization plays an important role in SOA formation from isoprenephotooxidation, the observed temperature dependence of SOA yield is largelyexplained by gas/particle partitioning of semi-volatile compounds.
机译:近年来,异戊二烯的大气氧化形成次生有机气溶胶(SOA)已成为多项研究的主题。然而,从人为来源发出的其他共轭二烯的反应仍然知之甚少。研究了异戊二烯,异戊二烯-1- 13 C,1,3-丁二烯和2,3-二甲基-1,3-丁二烯的光氧化形成的SOA,以获取高NO 条件。在1,3-丁二烯/ NO x / H 2 O 2 辐射系统(0.089–0.178)中测得的SOA产量接近或略有高于异戊二烯在类似NO x 条件下的测量值(0.077–0.103),这表明1,3-丁二烯的光氧化作用可能是城市空气中SOA的来源。相反,在用2,3-二甲基-1,3-丁二烯进行的实验中产生了非常少量的SOA颗粒。离线液相色谱-质谱分析表明,低聚酯信号占所研究的所有二烯中SOA产品信号的绝大部分(0.10-0.33)。所述低聚酯源自不饱和醛气相二烯反应产物。即,通过不饱和醛的氧化产生的半挥发性化合物经历了颗粒相低聚酯的形成。在这些实验中,还以异戊二烯为起始二烯表征了通过硝基氧基多元醇与2-甲基甘油酸单体或其低聚物之间的脱水反应而产生的低聚酯。这些低聚物可能是在高NO x 条件下收集的气溶胶样品中发现的2-甲基四醇的来源。此外,在这项研究中还进行了低温实验,在278 K下用异戊二烯测量SOA收率在相同的浓度条件下,其值是300 K下的2–3倍。尽管低聚在异戊二烯光氧化形成SOA中起着重要作用,但观察到的SOA产率的温度依赖性在很大程度上由半挥发性化合物的气体/颗粒分配所解释。

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