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Organic Molecular Compositions and Size Distributions of Chinese Summer and Autumn Aerosols from Nanjing: Characteristic Haze Event Caused by Wheat Straw Burning

机译:南京中国夏秋季气溶胶的有机分子组成和粒径分布:麦秸燃烧引起的典型霾事件

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摘要

Size-segregated aerosol samples were collected in urban Nanjing, China during summer and autumn of 2007 including a period of hazy days during June 1-5. Organic aerosols in the haze event were characterized by elevated concentrations of levoglucosan, high molecular weight (HMW) n-alkanes, and HMW fatly acids due to the emissions from field burning of wheat straw. In contrast organic aerosols on nonhazy days were characterized by a predominance of fossil fuel combustion products. Levoglucosan (4030 ng m~(-3)), n-alkanes (1520 ng m~(-3)), fatty acids (2629 ng m~(-3)), and PAHs (57 ng m~(-3)) in the haze samples were 3-40 times more abundant than those in noneventsamples. Approximately 30-90% ofthe organics during the haze period can be attributed to wheat straw burning. Concentrations of paniculate material (PM) mass, n-alkanes, and low molecular weight (LMW) PAHs showed a unimodal size distribution, peaking at 0.7-1.1 μm during the hazy days, and a bimodal distribution, peaking at 0.7-1.1 μm and 4.7-5.8 μm during nonhazy days. The geometric mean diameters (GMDs) of organic aerosols are larger in the fine mode (<2.1 μm) during the hazy days, suggesting aerosols emitted from the wheat straw burning are larger than those from fossil fuel combustion, and fine particle coagulation and organic compound repartitioning were enhanced.
机译:在2007年夏季和秋季,在中国南京市区收集了按大小分类的气溶胶样品,其中包括6月1-5日的朦胧天。霾事件中的有机气溶胶的特征是由于麦草田间燃烧产生的排放,左旋葡聚糖,高分子量(HMW)正构烷烃和HMW脂肪酸的浓度升高。相反,在非朦胧的日子里,有机气溶胶的特征是化石燃料燃烧产物占主导地位。左旋葡聚糖(4030 ng m〜(-3)),正构烷烃(1520 ng m〜(-3)),脂肪酸(2629 ng m〜(-3))和PAHs(57 ng m〜(-3)) )在雾度样品中的含量是非活动样品中含量的3-40倍。霾期间约有30-90%的有机物归因于麦秸燃烧。颗粒状物质(PM),正构烷烃和低分子量(LMW)多环芳烃的浓度表现出单峰尺寸分布,在朦胧的日子中达到峰值0.7-1.1μm,而双峰分布则达到0.7-1.1μm,达到峰值。在非朦胧的日子里为4.7-5.8μm。在朦胧的日子里,有机气溶胶的几何平均直径(GMDs)在精细模式下(<2.1μm)较大,表明麦秸燃烧产生的气溶胶比化石燃料燃烧产生的气溶胶大,细颗粒凝结和有机化合物重新分区得到增强。

著录项

  • 来源
    《Environmental Science & Technology》 |2009年第17期|6493-9499|共7页
  • 作者单位

    State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences, Xi'an 710075, China Institute of Low Temperature Science, Hokkaido University, Sapporo 060-0819, Japan School of the Environment, State Key Laboratory of Pollution Control and Resources Reuse, Nanjing University, Nanjing 210093, China,;

    Institute of Low Temperature Science, Hokkaido University, Sapporo 060-0819, Japan;

    School of the Environment, State Key Laboratory of Pollution Control and Resources Reuse, Nanjing University, Nanjing 210093, China,;

    School of the Environment, State Key Laboratory of Pollution Control and Resources Reuse, Nanjing University, Nanjing 210093, China,;

    State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences, Xi'an 710075, China;

    State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences, Xi'an 710075, China;

    State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences, Xi'an 710075, China Division of Atmospheric Sciences, Desert Research Institute, Reno, Nevada 89512-1095;

    State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences, Xi'an 710075, China Division of Atmospheric Sciences, Desert Research Institute, Reno, Nevada 89512-1095;

  • 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);
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  • 正文语种 eng
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  • 入库时间 2022-08-17 14:04:50

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