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首页> 外文期刊>TERI Information Digest on Energy and Environment >Understanding the origin of carbonaceous aerosols during periods of extensive biomass burning in northern India
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Understanding the origin of carbonaceous aerosols during periods of extensive biomass burning in northern India

机译:了解印度北部广泛生物质燃烧期间碳质气溶胶的起源

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This study explores the PM_(2.5) (particulate matter with aerodynamic diameter ≤2.5 μm) emissions during various time periods (pre-monsoon, monsoon, and post-monsoon) over the biomass burning source region in Beas, Punjab. The PM_(2.5) concentrations during the pre-monsoon period (106-458 μg/m~3) and the post-monsoon period (184-342 μg/m~3) were similar but much higher than concentrations during the monsoon season (23-95 μg/m~3) due to enhanced wet deposition. However, the carbonaceous aerosol fraction in PM_(2.5) was nearly double in the post-monsoon season (~27%) than in the pre-monsoon period (~15%). A higher contribution of secondary organic carbon (SOC) observed during the pre-monsoon season can be attributed to enhanced photochemical activity in dry conditions. The concentration of carbon fractions in sampled sources and aerosols suggests contribution of biofuels,resultinginenhancedPMconcentration at this location. δ~(13)C_(TC) values of pre- and post-monsoon samples show dominance of freshly emitted aerosols from local sources. Impact of biomass and biofuel combustion was also confirmed by biomass burning K~+_(BB) tracer, indicating that major agriculture residue burning occurred primarily during night-time. C_3 plant derived aerosols dominated at the sampling location during the entire sampling duration and contributed significantly during the pre-monsoon season. Both fossil fuel and C_3 plant combustion contributed to the total mass of carbonaceous aerosols during the post-monsoon and monsoon seasons.
机译:该研究探讨了在旁遮普篮板上的生物质燃烧源区的各种时间段(季风,季风和季风的季葡萄球菌≤2.5μm)排放的PM_(2.5)(颗粒状物质)排放。在季风前期的PM_(2.5)浓度(106-458μg/ m〜3)和季铵季期(184-342μg/ m〜3)相似但远远高于季风季节期间的浓度( 23-95μg/ m〜3)由于增强湿沉积。然而,PM_(2.5)中的碳质气溶胶级分在季风季节(〜27%)中几乎是两倍(〜27%),而不是在季风期(〜15%)中。在季风季节前观察到的二次有机碳(SOC)的贡献归因于在干燥条件下提高光化学活性。取样来源和气溶胶中的碳级分的浓度表明了生物燃料的贡献,结果为该位置。 δ〜(13)前和后季后样品的C_(TC)值显示出新鲜发射的局部气溶胶的优势。生物质和生物燃料燃烧的影响也通过生物质燃烧K〜_(BB)示踪剂证实,表明主要农业残留物燃烧主要在夜间期间发生。 C_3植物在整个采样持续时间内衍生在采样位置的气溶胶,在季风季节期间显着贡献。化石燃料和C_3植物燃烧均导致季风和季风季节的碳质气溶胶总量。

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    Department of Civil Engineering and APTL at Center for Environmental Science and Engineering (CESE) Indian Institute of Technology Kanpur Kanpur 208 016 India;

    Department of Civil Engineering and APTL at Center for Environmental Science and Engineering (CESE) Indian Institute of Technology Kanpur Kanpur 208 016 India;

    Department of Civil Engineering and APTL at Center for Environmental Science and Engineering (CESE) Indian Institute of Technology Kanpur Kanpur 208 016 India;

    Department of Civil Engineering and APTL at Center for Environmental Science and Engineering (CESE) Indian Institute of Technology Kanpur Kanpur 208 016 India;

    Department of Civil Engineering and APTL at Center for Environmental Science and Engineering (CESE) Indian Institute of Technology Kanpur Kanpur 208 016 India;

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