Wintertime PM2.5 and PM10 carbonaceous and inorganic constituents from urban site in western India

Daily variability in the chemical composition of atmospheric PM2.5and PM10has been studied from an urban site (Ahmedabad) in western India over a span of 30days during winter. The PM2.5and PM10mass concentrations ranged from 32 to 106 mu gm-3 and 121 to 327 mu gm-3, respectively. On average, PM2.5 c...

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Veröffentlicht in:Atmospheric research 2011-12, Vol.102 (4), p.420-431
Hauptverfasser: RENGARAJAN, R, SUDHEER, A. K, SARIN, M. M
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Sprache:eng
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Zusammenfassung:Daily variability in the chemical composition of atmospheric PM2.5and PM10has been studied from an urban site (Ahmedabad) in western India over a span of 30days during winter. The PM2.5and PM10mass concentrations ranged from 32 to 106 mu gm-3 and 121 to 327 mu gm-3, respectively. On average, PM2.5 constitutes ~33% of PM10, indicating dominance of coarse mode aerosols in the urban atmosphere. The particulate EC and OC show higher abundances in PM2.5 (average: 3.0+/-0.9 and 18.3+/-5.9 mu gm-3 respectively) whereas those in PM10 are 4.4+/-2.4 and 29.8+/-11.2 mu gm-3 respectively. A linear increasing trend and representative OC/EC ratio of 6.2 indicate their primary source from biomass burning emissions. The water-soluble organic carbon (WSOC: 4.0-14.7 mu gm-3) and its linear relationship with K+ (0.6-1.7 mu gm-3) in PM2.5 further support biomass burning emissions as a dominant source for carbonaceous aerosol. Among water-soluble inorganic species, SO4|>2- is the most abundant (range: 3.2-22.5 mu gm-3); almost all of it occurs in fine mode (PM2.5) and exhibits near-quantitative neutralization with NH4|>+ (r=0.98, slope: 1.3). The water-soluble Ca2+ and Mg2+ mainly abundant in the coarse mode, suggest significant contribution from mineral dust. Documenting large temporal variability in the chemical composition of coarse and fine mode aerosol is essential in order to assess the changing regional emission scenario over mega-cities and their down-wind transport.
ISSN:0169-8095
1873-2895
DOI:10.1016/j.atmosres.2011.09.005