Characterisation of water-soluble organic aerosols at a site on the southwest coast of India

被引:17
|
作者
Hegde, Prashant [1 ]
Kawamura, Kimitaka [2 ]
Girach, I. A. [1 ]
Nair, Prabha R. [1 ]
机构
[1] Vikram Sarabhai Space Ctr, Space Phys Lab, Thiruvananthapuram, Kerala, India
[2] Hokkaido Univ, Inst Low Temp Sci, Sapporo, Hokkaido 060, Japan
基金
日本学术振兴会;
关键词
Organic aerosols; Dicarboxylic acid; Biomass burning; Anthropogenic sources; Seasonal variation; BIOMASS BURNING AEROSOLS; WEIGHT DICARBOXYLIC-ACIDS; OMEGA-OXOCARBOXYLIC ACIDS; CLOUD CONDENSATION NUCLEI; LONG-RANGE TRANSPORT; CHEMICAL-COMPOSITION; ATMOSPHERIC AEROSOLS; KETOCARBOXYLIC ACIDS; ALPHA-DICARBONYLS; SIZE DISTRIBUTIONS;
D O I
10.1007/s10874-015-9322-4
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Aerosol samples collected over a tropical location, Thumba, southernmost West Coast of India were analyzed for the abundance of homologous dicarboxylic acids (C-2 to C-12), oxocarboxylic acids (omega C-2 to omega C-9, pyruvic acid), alpha-dicarbonyls (glyoxal and methylglyoxal), organic and elemental carbon. Among the measured organics, oxalic acid was found to be the most abundant species followed by succinic and/or malonic acids. As oxoacid and alpha-carbonyl groups, glyoxylic acid and glyoxal, respectively, were observed to be dominant. On average, dicarboxylic acids accounted almost 2.1 +/- 0.7 % of the aerosol total organic carbon. Among the aerosols over Thumba, two types of formation pathways were noticed for oxalic acid. During the post-monsoon and winter periods, the photo-oxidation of biogenic and anthropogenic volatile organic compounds lead to the formation of oxalic acid through a chain reaction involving glyoxal, methylglyoxal, pyruvic and glyoxylic acids. In contrast, during the pre-monsoon, the oxidative degradation of the biogenic unsaturated fatty acids give rise to succinic acid, which can be decomposed to malonic acid and then to oxalic acid. The observed seasonal variations in acid concentrations are consistent with photochemical production and the subsequent accumulation under favourable meteorological conditions prevailing over the region.
引用
收藏
页码:181 / 205
页数:25
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