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首页> 外文期刊>The Science of the Total Environment >Seasonal size distribution and mixing state of black carbon aerosols in a polluted urban environment of the Yangtze River Delta region, China
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Seasonal size distribution and mixing state of black carbon aerosols in a polluted urban environment of the Yangtze River Delta region, China

机译:长江三角洲污染城市环境中黑碳气溶胶的季节分布和混合状态

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摘要

The optical properties of black carbon aerosols (BC) are determined by the particles size and the associated non-BC materials, which may be source-related or modified during secondary processing. The one-year long monitoring of BC was first conducted using a Single Particle Soot Photometer (SP2) from December 2013 to November 2014 in Nanjing, a megacity in the Yangtze River Delta region of China. The seasonal variation in the BC size distribution and mixing state were investigated. There was no apparent systematic variation in the mean BC core mass median diameter between seasons, as these values were 226 +/- 12 nm, 217 +/- 13 nm, 211 +/- 15 nm and 221 +/- 12 nm for winter, spring, summer and autumn respectively. The mixing state of BC was quantified as the bulk relative coating thickness (defined as particle size D(p )over core size D-c, D-p/D-c), which ranged from 1.05 to 2.65. The BC was found to be significantly more coated in the winter (D-p/D-c = 1.50 +/- 0.30) than in other seasons (D-p/D-c = 1.27 +/- 0.09, 1.28 +/- 0.10, 1.27 +/- 0.11 in spring, summer and autumn respectively). Higher levels of coating during the winter may due to the contributions of the primary source (with the highest BC mass loadings between seasons) or secondary processes such as low temperature that facilitated the condensation. It was found that the photochemical process may enhance the coatings on BC in summer. At nighttime, the reduced and stabilized planetary boundary layer and the nighttime secondary formation may also lead to BC becoming well mixed with other components. Moreover. BC was shown to be less coated when the NOx concentration was high. However, during all seasons, the BC coating was strongly correlated with other non-BC particulate mass, which suggests that at higher pollution levels BC was more significantly coated with other existing materials through coagulation or condensation by other secondary species. (C) 2018 Elsevier B.V. All rights reserved.
机译:炭黑气溶胶(BC)的光学特性由颗粒大小和相关的非BC材料决定,这些材料可能与来源有关或在二次加工过程中发生了变化。从2013年12月至2014年11月,在中国长江三角洲的特大城市南京,首次使用单颗粒碳烟光度计(SP2)对BC进行了为期一年的监测。研究了BC尺寸分布和混合状态的季节性变化。季节之间的平均BC核心质量中值直径没有明显的系统变化,因为冬天的这些值分别为226 +/- 12 nm,217 +/- 13 nm,211 +/- 15 nm和221 +/- 12 nm分别是春季,夏季和秋季。 BC的混合状态被量化为整体相对涂层厚度(定义为粒径D(p)超过芯尺寸D-c,D-p / D-c),范围为1.05至2.65。发现冬季的BC(Dp / Dc = 1.50 +/- 0.30)明显多于其他季节(Dp / Dc = 1.27 +/- 0.09,1.28 +/- 0.10,1.27 +/- 0.11)分别是春季,夏季和秋季)。在冬季,较高的涂料量可能归因于主要来源(季节之间具有最高的BC质量负载)或次要过程(如低温)的促成作用。已经发现,光化学过程可以在夏天增强BC上的涂层。在夜间,行星边界层的减少和稳定以及夜间的次级构造也可能导致BC与其他成分充分混合。此外。当NOx浓度高时,BC的涂层较少。但是,在所有季节中,BC涂层都与其他非BC颗粒质量密切相关,这表明在更高的污染水平下,BC通过其他次生物种的凝结或凝结而被其他现有材料显着覆盖。 (C)2018 Elsevier B.V.保留所有权利。

著录项

  • 来源
    《The Science of the Total Environment》 |2019年第1期|300-310|共11页
  • 作者单位

    Nanjing Univ Informat Sci & Technol, Key Lab Aerosol Cloud Precipitat, China Meteorol Adm, Sch Atmospher Phys, Nanjing 210044, Jiangsu, Peoples R China;

    Nanjing Univ Informat Sci & Technol, Key Lab Aerosol Cloud Precipitat, China Meteorol Adm, Sch Atmospher Phys, Nanjing 210044, Jiangsu, Peoples R China;

    Inst Natl Environm Ind & Risques, F-60550 Verneuil En Halatte, France|Univ Paris Saclay, Lab Sci Climat & Environm, UVSQ, CNRS,CEA, F-91191 Gif Sur Yvette, France;

    Nanjing Univ Informat Sci & Technol, Key Lab Aerosol Cloud Precipitat, China Meteorol Adm, Sch Atmospher Phys, Nanjing 210044, Jiangsu, Peoples R China;

    Nanjing Univ Informat Sci & Technol, Key Lab Aerosol Cloud Precipitat, China Meteorol Adm, Sch Atmospher Phys, Nanjing 210044, Jiangsu, Peoples R China;

    Zhejiang Univ, Sch Earth Sci, Dept Atmospher Sci, Hangzhou 310058, Zhejiang, Peoples R China|Univ Manchester, Ctr Atmospher Sci, Sch Earth Atmospher & Environm Sci, Manchester M13 9PL, Lancs, England;

    Xian Jiangtong Liverpoor Univ, Dept Environm Sci, Suzhou 215123, Peoples R China;

    Nanjing Univ Informat Sci & Technol, Jiangsu Collaborat Innovat Ctr Atmospher Environm, Sch Environm Sci & Engn, Nanjing 210044, Jiangsu, Peoples R China;

    Nanjing Univ Informat Sci & Technol, Jiangsu Collaborat Innovat Ctr Atmospher Environm, Sch Environm Sci & Engn, Nanjing 210044, Jiangsu, Peoples R China;

    Jiangsu Environm Monitoring Ctr, Nanjing 210036, Jiangsu, Peoples R China;

    Nanjing Univ Informat Sci & Technol, Jiangsu Collaborat Innovat Ctr Atmospher Environm, Sch Environm Sci & Engn, Nanjing 210044, Jiangsu, Peoples R China|Jiangsu Environm Monitoring Ctr, Nanjing 210036, Jiangsu, Peoples R China;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Black carbon; Size distribution; Mixing state; Seasonal variations; Yangtze River Delta;

    机译:黑炭;粒度分布;混合状态;季节变化;长江三角洲;

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