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Sources and atmospheric processing of size segregated aerosol particles revealed by stable carbon isotope ratios and chemical speciation

机译:稳定的碳同位素比和化学形态揭示了大小分离的气溶胶颗粒的来源和大气过程

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摘要

Size-segregated aerosol particles were collected during winter sampling campaigns at a coastal (55 degrees 37' N, 21 degrees 03'E) and an urban (54 degrees 64' N, 25 degrees 18' E) site. Organic compounds were thermally desorbed from the samples at different temperature steps ranging from 100 degrees C to 350 degrees C. The organic matter (OM) desorbed at each temperature step is analysed for stable carbon isotopes using an isotope ratio mass spectrometer (IRMS) and for individual organic compounds using a Proton Transfer Reaction Time-of-Flight Mass Spectrometer (PTR-MS). The OM desorbed at temperatures 200 degrees C was classified as less refractory carbon and the OM desorbed at temperatures between 200 degrees C and 350 degrees C was classified as more refractory carbon. At the coastal site, we identified two distinct time periods. The first period was more frequently influenced by marine air masses than the second time period, which was characterized by Easterly wind directions and continental air masses. During the first period OM contained a large fraction of hydrocarbons and had a carbon isotopic signature typical of liquid fossil fuels in the region. Organic mass spectra provide strong evidence that shipping emissions are a significant source of OM at this coastal site. The isotopic and chemical composition of OM during the second period at the coastal site was similar to the composition at the urban site. There was a clear distinction in source contribution between the less refractory OM and the more refractory OM at these sites. According to the source apportionment method used in this study, we were able to identify fossil fuel burning as predominant source of the less refractory OM in the smallest particles (D-50 0.18 mu m), and biomass burning as predominant source of the more refractory OM in the larger size range (0.32 D-50 1 mu m). (C) 2018 Elsevier Ltd. All rights reserved.
机译:在冬季采样活动期间,在沿海(北纬55度37度,东经21度03度)和城市(北纬54度64度,东25度18度)地点采集了大小分离的气溶胶颗粒。在100℃至350℃的不同温度步骤下,从样品中热解吸有机化合物。使用同位素比质谱仪(IRMS)分析每个温度步骤下解吸的有机物(OM)的稳定碳同位素,并分析使用质子转移反应飞行时间质谱仪(PTR-MS)分离单个有机化合物。在<200摄氏度的温度下解吸的OM被归类为难熔碳,而在200摄氏度和350摄氏度之间的温度下解吸的OM被归为难熔碳。在沿海地区,我们确定了两个不同的时间段。与第二时间段相比,第一时间段受海洋气团的影响更频繁,第二时间段的特征是东风和大陆气团。在第一阶段,OM含有大量的碳氢化合物,并具有该地区典型的液态化石燃料的碳同位素特征。有机质谱提供了有力的证据,表明在此沿海地点,船舶排放物是OM的重要来源。在第二个时期,沿海地区的OM的同位素和化学成分与城市地区的相似。在这些地点,难熔性较低的OM和难熔性较高的OM在源贡献上有明显区别。根据本研究中使用的源分配方法,我们能够确定化石燃料燃烧是最小颗粒(D-50 <0.18μm)中难熔性较低的有机质的主要来源,而生物质燃烧是更多难燃性材料的主要来源。较大尺寸范围内的耐火材料OM(0.32

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  • 来源
    《Environmental Pollution》 |2018年第9期|286-296|共11页
  • 作者单位

    Ctr Phys Sci & Technol, State Res Inst, Vilnius, Lithuania;

    Univ Utrecht, Inst Marine & Atmospher Res Utrecht IMAU, Utrecht, Netherlands;

    Natl Univ Ireland Galway, Sch Phys, Galway, Ireland;

    Ctr Phys Sci & Technol, State Res Inst, Vilnius, Lithuania;

    Ctr Phys Sci & Technol, State Res Inst, Vilnius, Lithuania;

    Univ Utrecht, Inst Marine & Atmospher Res Utrecht IMAU, Utrecht, Netherlands;

    Univ Utrecht, Inst Marine & Atmospher Res Utrecht IMAU, Utrecht, Netherlands;

  • 收录信息 美国《科学引文索引》(SCI);美国《工程索引》(EI);美国《生物学医学文摘》(MEDLINE);美国《化学文摘》(CA);
  • 原文格式 PDF
  • 正文语种 eng
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