Impact of Biomass Burning Plumes on the Size-Segregated Aerosol Chemistry over an Urban Atmosphere at Indo-Gangetic Plain

被引:24
|
作者
Ghosh, Abhinandan [1 ]
Roy, Arindam [1 ]
Chatterjee, Abhijit [1 ,2 ]
Das, Sanat K. [1 ]
Ghosh, Sanjay K. [2 ,3 ]
Raha, Sibaji [1 ,2 ,3 ]
机构
[1] Bose Inst, Environm Sci Sect, Kolkata 700054, India
[2] Bose Inst, Natl Facil Astroparticale Phys & Space Sci, Darjeeling 734101, India
[3] Bose Inst, Ctr Astroparticle Phys & Space Sci, Kolkata 700091, India
关键词
Shifting cultivation; Size-segregated aerosols; Biomass burning; Eastern Ghats; LARGE-SCALE WILDFIRES; CHEMICAL-COMPOSITION; SOUTHERN AFRICA; ORGANIC AEROSOL; PHYSICOCHEMICAL CHARACTERIZATION; SOURCE APPORTIONMENT; INDUSTRIAL SITES; BROWN CARBON; EMISSIONS; SMOKE;
D O I
10.4209/aaqr.2017.12.0590
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
A study was conducted on the impact of biomass burning plumes transported from the Eastern Ghats region on the chemical characteristics of size-segregated aerosols over Kolkata, a tropical megacity situated in the eastern part of the Indo-Gangetic Plain. A Micro Orifice Uniform Deposit Impactor (MOUDI) was used to collect size-segregated aerosols affected and unaffected by the influence of transported biomass burning plumes during the pre-monsoon season (March-May) in 2016. Satellite observations revealed the presence of a thick polluted aerosol layer over Kolkata during the fire episodes, whereas a clean marine aerosol layer was observed during the normal episodes. Transported plumes enhanced the fine-mode aerosols, whereas the coarse-mode aerosols remained unaffected. PM1.0-0.1 and PM0.1 were greatly affected by the transported plumes, with a threefold increase during the fire episodes. K+, NH4+ and SO42- showed significant increases in the accumulation-mode (PM1.0-0.1) under the influence of biomass burning plumes, whereas NO3- showed an increase in the coarse-mode aerosols. The transported plumes did not change the mass-size distribution patterns of K+, NH4+ and SO42- (in which the unimodal fine-mode was dominant), but NO3- showed a change from a bimodal to a unimodal coarse-mode distribution under the influence of the plumes. It was observed that the biomass burning plumes interacted strongly with the accumulation- and superfine-mode (PM0.1) sea-salt particles, leading to the depletion of chloride. The maximum chloride depletion (similar to 80%) was observed in the size range of 0.560.32 mu m. It was observed that non-sea-SO42- was the key constituent responsible for the chloride loss from sea-salt particles. The biomass burning plume was found to have the potential to shift the dominance from coarse- to fine-mode particles in the mass-size distribution pattern of the total aerosols.
引用
收藏
页码:163 / 180
页数:18
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