<?xml version="1.0" encoding="utf-8" standalone="no"?>
<!DOCTYPE article SYSTEM "http://www.atmos-chem-phys-discuss.net/inc/acpd/copernicus.dtd">
<article language="en">
	<journal>
		<journal_title>Atmospheric Chemistry and Physics Discussions</journal_title>
		<journal_url>www.atmos-chem-phys-discuss.net</journal_url>
		<issn>1680-7367</issn>
		<eissn>1680-7375</eissn>
		<volume_number>4</volume_number>
		<issue_number>5</issue_number>
		<publication_year>2004</publication_year>
	</journal>
	<doi>10.5194/acpd-4-6867-2004</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/4/6867/2004/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/4/6867/2004/acpd-4-6867-2004.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/4/6867/2004/acpd-4-6867-2004.pdf</fulltext_pdf>
	<start_page>6867</start_page>
	<end_page>6907</end_page>
	<publication_date>2004-10-28</publication_date>
	<article_title content_type="html">Low molecular weight organic acids in aerosol particles from Rond&amp;ocirc;nia, Brazil, during the biomass-burning, transition and wet periods</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>A. H. Falkovich</name>
		</author>
		<author numeration="2" affiliations="1,2">
			<name>E. R. Graber</name>
		</author>
		<author numeration="3" affiliations="1">
			<name>G. Schkolnik</name>
		</author>
		<author numeration="4" affiliations="1">
			<name>Y. Rudich</name>
			<email>yinon.rudich@weizmann.ac.il</email>
		</author>
		<author numeration="5" affiliations="3">
			<name>W. Maenhaut</name>
		</author>
		<author numeration="6" affiliations="4">
			<name>P. Artaxo</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Department of Environmental Sciences, Weizmann Institute, Rehovot 76100, Israel</affiliation>
		<affiliation numeration="2" content_type="html">Permanent affiliation: Institute of Soil, Water and Environmental Sciences, The Volcani Center, ARO, Bet Dagan 50250, Israel</affiliation>
		<affiliation numeration="3" content_type="html">Department of Analytical Chemistry, Institute for Nuclear Sciences, Ghent University, Proeftuinstraat 86, B-9000 Gent, Belgium</affiliation>
		<affiliation numeration="4" content_type="html">Institute of Physics, University of S&amp;atilde;o Paulo, Rua do Mat&amp;atilde;o, Travessa R, 187, CEP 05508-900 S&amp;atilde;o Paulo, Brazil</affiliation>
	</affiliations>
	<abstract content_type="html">Particles from biomass burning and regional haze were sampled in
Rond&amp;#244;nia, 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 &amp;ndash; 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 &amp;ndash; 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&lt;sub&gt;2&lt;/sub&gt;-C&lt;sub&gt;6&lt;/sub&gt; 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&lt;sub&gt;2&lt;/sub&gt;-C&lt;sub&gt;6&lt;/sub&gt;) acids are dominated by oxalic acid followed by malonic and
succinic acids. The largest ionic species is ammonium sulfate (60&amp;ndash;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&lt;sup&gt;+&lt;/sup&gt;, a known biomass burning tracer, it is suggested
that many of the organic acids are directly emitted by vegetation fires. It
is concluded that the dicarboxylic acids are mostly confined to the
particulate phase, and no evidence for semi-volatile behavior was observed.
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.</abstract>
	<references>
	</references>
</article>

