Low molecular weight organic acids in aerosol particles from Rondonia, Brazil, during the biomass-burning, transition and wet periods

被引:174
作者
Falkovich, AH
Graber, ER
Schkolnik, G
Rudich, Y [1 ]
Maenhaut, W
Artaxo, P
机构
[1] Weizmann Inst Sci, Dept Environm Sci, IL-76100 Rehovot, Israel
[2] Univ Ghent, Inst Sci Nucl, Dept Analyt Chem, B-9000 Ghent, Belgium
[3] Univ Sao Paulo IFUSP, Inst Phys, BR-05508900 Sao Paulo, Brazil
关键词
D O I
10.5194/acp-5-781-2005
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Particles from biomass burning and regional haze were sampled in Rondonia, Brazil, during dry, transition and wet periods from September to November 2002, as part of the LBA-SMOCC (Large-Scale Biosphere-Atmosphere Experiment in Amazonia - Smoke, Aerosols, Clouds, Rainfall, and Climate) field campaign. Water soluble organic and inorganic compounds in bulk (High Volume and Stacked Filter Unit sampler) and size-resolved (Micro Orifice Uniform Deposit Impactor - MOUDI) smoke samples were determined by ion chromatography. It was found that low molecular weight polar organic acids account for a significant fraction of the water soluble organic carbon (WSOC) in biomass burning aerosols (C-2-C-6 dicarboxylic acids reached up to 3.7% and one-ring aromatic acids reached up to 2% of fine fraction WSOC during burning period). Short dicarboxylic (C-2-C-6) acids are dominated by oxalic acid followed by malonic and succinic acids. The largest ionic species is ammonium sulfate (60-70% of ionic mass). It was found that most of the ionic mass is concentrated in submicrometer-sized particles. Based on the size distribution and correlations with K+, a known biomass burning tracer, it is suggested that many of the organic acids are directly emitted by vegetation fires. Concentrations of dicarboxylic acids in the front and back filters of high volume sampler were determined. Based on these measurements, it was concluded that in the neutral or slightly basic smoke particles typical of this region, dicarboxylic acids are mostly confined to the particulate phase. Finally, it is shown that the distribution of water soluble species shifts to larger aerosols sizes as the aerosol population ages and mixes with other aerosol types in the atmosphere.
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页码:781 / 797
页数:17
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