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首页> 外文期刊>Atmospheric chemistry and physics >Organic molecular tracers in the atmospheric aerosols from Lumbini, Nepal, in the northern Indo-Gangetic Plain: influence of biomass burning
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Organic molecular tracers in the atmospheric aerosols from Lumbini, Nepal, in the northern Indo-Gangetic Plain: influence of biomass burning

机译:来自尼泊尔北部的北部北部的大气气溶胶中的有机分子示踪剂,在北印度北部:生物质燃烧的影响

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摘要

To better understand the characteristics of biomass burning in the northern Indo-Gangetic Plain (IGP), total suspended particles were collected in a rural site, Lumbini, Nepal, during April 2013 to March 2014 and analyzed for the biomass burning tracers (i.e., levoglucosan, mannosan, vanillic acid). The annual average concentration of levoglucosan was 734 +/- 1043 ng m(-3) with the maximum seasonal mean concentration during post-monsoon season (2206 +/- 1753 ng m(-3)), followed by winter (1161 +/- 1347 ng m(3)), pre-monsoon (771 +/- 524 ng m(-3)) and minimum concentration during monsoon season (212 +/- 279 ng m(-3)). The other biomass burning tracers (mannosan, galactosan, p-hydroxybenzoic acid, vanillic acid, syringic acid and dehydroabietic acid) also showed the similar seasonal variations. There were good correlations among levoglucosan, organic carbon (OC) and elemental carbon (EC), indicating significant impact of biomass burning activities on carbonaceous aerosol loading throughout the year in Lumbini area. According to the characteristic ratios, levoglucosan / mannosan (lev / man) and syringic acid / vanillic acid (syr / van), we deduced that the high abundances of biomass burning products during nonmonsoon seasons were mainly caused by the burning of crop residues and hardwood while the softwood had less contribution. Based on the diagnostic tracer ratio (i.e., lev / OC), the OC derived from biomass burning constituted large fraction of total OC, especially during post-monsoon season. By analyzing the MODIS fire spot product and 5-day airmass back trajectories, we further demonstrated that organic aerosol composition was not only related to the local agricultural activities and residential biomass usage but also impacted by the regional emissions. During the post-monsoon season, the emissions from rice residue burning in western India and eastern Pakistan could impact particulate air pollution in Lumbini and surrounding regions in southern Nepal. Therefore, our finding is meaningful and has a great importance for adopting the appropriate mitigation measures, not only at the local level but also by involving different regions and nations, to reduce the biomass burning emissions in the broader IGP region nations.
机译:为了更好地了解北部印度难道平原(IGP)的生物质燃烧的特征,在2013年4月至2014年4月期间,在农村遗址,尼泊尔尼泊尔收集了总悬浮颗粒,并分析了生物量燃烧的示踪剂(即左葡聚糖,人群,香草酸)。左葡聚糖的年平均浓度为734 +/- 1043 ng m(-3),季风季节期间最高季节性平均浓度(2206 +/- 1753 ng m(-3)),其次是冬季(1161 + / - 1347 ng m(3)),季风前(771 +/- 524ng m(-3))和季风季节期间的最小浓度(212 +/- 279 ng m(-3))。其他生物质燃烧的示踪剂(甘露烷,半乳糖,对羟基苯甲酸,香草,注射酸和脱氢酸)也显示出类似的季节变化。 Levoglucosan,有机碳(OC)和元素碳(EC)之间存在良好的相关性,表明生物量燃烧活性对莱姆尼地区全年含碳气溶胶荷载量的显着影响。根据特征比,左葡聚糖/甘露南(LEV / MAN)和注射酸/香草酸(SYR / VAN),我们推导出在非常温季节期间的生物量燃烧产品的高丰度主要是由作物残留和硬木燃烧引起的虽然软木的贡献较少。基于诊断示踪率(即,LEV / OC),oc来自生物量燃烧的oc构成大部分总OC,特别是在季风季节期间。通过分析Modis Fire Spect产品和5天的Airmass背面轨迹,我们进一步证明了有机气溶胶组合物不仅与当地农业活动和住宅生物量使用有关,还受到区域排放的影响。在季风季节期间,印度西部和巴基斯坦东部燃烧的水稻残留物的排放可能会影响尼泊尔南部伦尼尼和周边地区的微粒空气污染。因此,我们的发现是有意义的,并且非常重视采用适当的缓解措施,不仅在地方一级,而且还通过涉及不同的地区和国家,减少更广泛的IGP地区国家的生物量燃烧排放。

著录项

  • 来源
    《Atmospheric chemistry and physics》 |2017年第14期|共19页
  • 作者单位

    Chinese Acad Sci Inst Tibetan Plateau Res Key Lab Tibetan Environm Changes &

    Land Surface P Beijing 100101 Peoples R China;

    Chinese Acad Sci Northwest Inst Ecoenvironm &

    Resources State Key Lab Cryospher Sci Lanzhou 730000 Gansu Peoples R China;

    Chinese Acad Sci Northwest Inst Ecoenvironm &

    Resources State Key Lab Cryospher Sci Lanzhou 730000 Gansu Peoples R China;

    Chinese Acad Sci Inst Tibetan Plateau Res Key Lab Tibetan Environm Changes &

    Land Surface P Beijing 100101 Peoples R China;

    Chinese Acad Sci Inst Tibetan Plateau Res Key Lab Tibetan Environm Changes &

    Land Surface P Beijing 100101 Peoples R China;

    Chinese Acad Sci Inst Tibetan Plateau Res Key Lab Tibetan Environm Changes &

    Land Surface P Beijing 100101 Peoples R China;

    Chinese Acad Sci Northwest Inst Ecoenvironm &

    Resources State Key Lab Cryospher Sci Lanzhou 730000 Gansu Peoples R China;

    Chinese Acad Sci Northwest Inst Ecoenvironm &

    Resources State Key Lab Cryospher Sci Lanzhou 730000 Gansu Peoples R China;

    IASS D-14467 Potsdam Germany;

    Int Ctr Integrated Mt Dev ICIMOD Kathmandu Nepal;

    Shanghai Univ Sch Environm &

    Chem Engn Shanghai 200444 Peoples R China;

    Chubu Univ Chubu Inst Adv Studies Kasugai Aichi 4878501 Japan;

    Chinese Acad Sci Inst Tibetan Plateau Res Key Lab Tibetan Environm Changes &

    Land Surface P Beijing 100101 Peoples R China;

    Chinese Acad Sci Inst Tibetan Plateau Res Key Lab Tibetan Environm Changes &

    Land Surface P Beijing 100101 Peoples R China;

    Chinese Acad Sci Inst Tibetan Plateau Res Key Lab Tibetan Environm Changes &

    Land Surface P Beijing 100101 Peoples R China;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 大气科学(气象学);
  • 关键词

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