Aerosol Chemical Profile of Near-Source Biomass Burning Smoke in Sonla, Vietnam during 7-SEAS Campaigns in 2012 and 2013

This study aimed to investigate aerosol chemical characteristics and to obtain the chemical profile of near-source biomass burning (BB) aerosols at a site (675 m a.s.l.) in Sonla, Northern Vietnam. Particulate matter (PM) with an aerodynamic diameter less than or equal to 2.5 µm (PM 2.5 ) was collec...

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Veröffentlicht in:Aerosol and Air Quality Research 2016-11, Vol.16 (11), p.2603-2617
Hauptverfasser: Lee, Chung-Te, Ram, Shidharth Sankar, Nguyen, Dac Loc, Chou, Charles C. K., Chang, Shih-Yu, Lin, Neng-Huei, Chang, Shuenn-Chin, Hsiao, Ta-Chih, Sheu, Guey-Rong, Ou-Yang, Chang-Feng, Chi, Kai Hsien, Wang, Sheng-Hsiang, Wu, Xue-Chang
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Sprache:eng
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Zusammenfassung:This study aimed to investigate aerosol chemical characteristics and to obtain the chemical profile of near-source biomass burning (BB) aerosols at a site (675 m a.s.l.) in Sonla, Northern Vietnam. Particulate matter (PM) with an aerodynamic diameter less than or equal to 2.5 µm (PM 2.5 ) was collected over a 24 h sampling period as part of the Seven South East Asian Studies (7-SEAS) campaign. The studies were conducted when BB was highly active — that is, in the spring of 2012 and 2013. The collected particles were analyzed for carbonaceous fractions and water-soluble components, in addition to the mass concentration. Data obtained were further analyzed to determine the stable species profile by classifying the 5-day air-mass backward trajectories. The average PM 2.5 mass concentrations were 51 ± 19 µg m −3 and 57 ± 27 µg m −3 in 2012 and 2013, respectively. Carbonaceous contents dominated BB aerosol, with 59% ± 9% and 58% ± 9% in organic carbon (OC) and 9% ± 3% and 10% ± 3% in elemental carbon (EC) of PM 2.5 in 2012 and 2013, respectively. Of the 8 carbonaceous fractions analyzed thermo-optically for PM 2.5 , OC3 (evolution temperature at 280°C–480°C) was most abundant in OC fractions, and EC1-OP (elemental carbon evolved at 580°C minus the pyrolized OC fractions) was predominant in EC fractions in most occasions. Among the measured water-soluble inorganic ions, NH 4 + and SO 4 2− widely varied, indicating the influence of different trajectory origins. This finding was confirmed by trajectory classification of aerosol data. The trajectories were also distinguished with respect to char-EC to soot-EC ratio, and water-soluble OC. These characteristics were highest in the trajectory from the BB source area.
ISSN:1680-8584
2071-1409
DOI:10.4209/aaqr.2015.07.0465