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Formation of secondary aerosols from gasoline vehicle exhaust when mixing with SO2

机译:在用SO2混合时,从汽油车排气形成二次气溶胶

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Sulfur dioxide (SO2) can enhance the formation of secondary aerosols from biogenic volatile organic compounds (VOCs), but its influence on secondary aerosol formation from anthropogenic VOCs, particularly complex mixtures like vehicle exhaust, remains uncertain. Gasoline vehicle exhaust (GVE) and SO2, a typical pollutant from coal burning, are directly co-introduced into a smog chamber, in this study, to investigate the formation of secondary organic aerosols (SOA) and sulfate aerosols through photooxidation. New particle formation was enhanced, while substantial sulfate was formed through the oxidation of SO2 in the presence of high concentration of SO2. Homogenous oxidation by OH radicals contributed a negligible fraction to the conversion of SO2 to sulfate, and instead the oxidation by stabilized Criegee intermediates (sCIs), formed from alkenes in the exhaust reacting with ozone, dominated the conversion of SO2. After 5 h of photochemical aging, GVE's SOA production factor revealed an increase by 60-200% in the presence of high concentration of SO2 . The increase could principally be attributed to acid-catalyzed SOA formation as evidenced by the strong positive linear correlation (R-2 = 0 : 97) between the SOA production factor and in situ particle acidity calculated by the AIM-II model. A high-resolution time-of-flight aerosol mass spectrometer (HR-TOF-AMS) resolved OA's relatively lower oxygen-to-carbon (O:C)(0.44 +/- 0.02) and higher hydrogen-to-carbon (H:C) (1.40 +/- 0.03) molar ratios for the GVE/SO2 mixture, with a significantly lower estimated average carbon oxidation state (OSc) of -0.51 +/- 0.06 than -0.19 +/- 0.08 for GVE alone. The relative higher mass loading of OA in the experiments with SO2 might be a significant explanation for the lower SOA oxidation degree.
机译:二氧化硫(SO2)可以增强生物挥发性有机化合物(VOC)的二次气溶胶的形成,但其对来自人为VOC的二次气溶胶形成的影响,特别是载体排气等复杂的混合物,仍然不确定。汽油车排气(GVE)和SO2,燃煤的典型污染物,在本研究中直接共同引入烟雾室,以研究通过光氧化的二次有机气溶胶(SOA)和硫酸盐气溶胶的形成。提高了新的颗粒形成,而在高浓度的SO 2存在下通过SO 2的氧化形成了大量硫酸盐。通过OH基团的均匀氧化将SO2转化为SO2至硫酸盐的差异,而不是通过稳定的Criegee中间体(SCI)的氧化,由臭氧与臭氧反应中的烯烃形成,主导了SO2的转化率。在光化学老化5小时后,GVE的SOA生产因子在高浓度的SO2存在下显示出60-200%。该增加主要是归因于酸催化的SOA形成,如通过AIM-II模型计算的SOA生产因子和原位颗粒酸度之间的强正线性相关(R-2 = 0:97)所证明的。高分辨率飞行时间气溶胶质谱仪(HR-TOF-AMS)分离OA的相对较低的氧 - 碳(O:C)(0.44 +/- 0.02)和更高的氢 - 碳(H: C)(1.40 +/- 0.03)GVE / SO2混合物的摩尔比,估计的平均碳氧化态(OSC)仅为-0.51 +/- 0.06至0.0.19 +/- 0.08。在SO2的实验中的OA的相对较高的质量负载可能是对较低的SOA氧化程度的显着解释。

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    Chinese Acad Sci Guangzhou Inst Geochem State Key Lab Organ Geochem Guangzhou 510640 Guangdong Peoples R China;

    Chinese Acad Sci Guangzhou Inst Geochem State Key Lab Organ Geochem Guangzhou 510640 Guangdong Peoples R China;

    Chinese Acad Sci Guangzhou Inst Geochem State Key Lab Organ Geochem Guangzhou 510640 Guangdong Peoples R China;

    Chinese Acad Sci Guangzhou Inst Geochem State Key Lab Organ Geochem Guangzhou 510640 Guangdong Peoples R China;

    Chinese Acad Sci Guangzhou Inst Geochem State Key Lab Organ Geochem Guangzhou 510640 Guangdong Peoples R China;

    Chinese Acad Sci Guangzhou Inst Geochem State Key Lab Organ Geochem Guangzhou 510640 Guangdong Peoples R China;

    Chinese Acad Sci Guangzhou Inst Geochem State Key Lab Organ Geochem Guangzhou 510640 Guangdong Peoples R China;

    Chinese Acad Sci Guangzhou Inst Geochem State Key Lab Organ Geochem Guangzhou 510640 Guangdong Peoples R China;

    Chinese Acad Sci Guangzhou Inst Geochem State Key Lab Organ Geochem Guangzhou 510640 Guangdong Peoples R China;

    Chinese Acad Sci Guangzhou Inst Geochem State Key Lab Organ Geochem Guangzhou 510640 Guangdong Peoples R China;

    Chinese Acad Sci Guangzhou Inst Geochem State Key Lab Organ Geochem Guangzhou 510640 Guangdong Peoples R China;

    Chinese Acad Sci Guangzhou Inst Geochem State Key Lab Organ Geochem Guangzhou 510640 Guangdong Peoples R China;

    Fudan Univ Dept Environm Sci &

    Engn Shanghai Key Lab Atmospher Particle Pollut &

    Prev Shanghai 200433 Peoples R China;

    Chinese Acad Sci Inst Atmospher Phys Beijing 100029 Peoples R China;

    Hong Kong Univ Sci &

    Technol Div Environm Kowloon Hong Kong Peoples R China;

    Chinese Acad Sci Guangzhou Inst Geochem State Key Lab Organ Geochem Guangzhou 510640 Guangdong Peoples R China;

    Chinese Acad Sci Guangzhou Inst Geochem State Key Lab Organ Geochem Guangzhou 510640 Guangdong Peoples R China;

    Chinese Acad Sci Guangzhou Inst Geochem State Key Lab Organ Geochem Guangzhou 510640 Guangdong Peoples R China;

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