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<!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>5</volume_number>
		<issue_number>5</issue_number>
		<publication_year>2005</publication_year>
	</journal>
	<doi>10.5194/acpd-5-8027-2005</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/5/8027/2005/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/5/8027/2005/acpd-5-8027-2005.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/5/8027/2005/acpd-5-8027-2005.pdf</fulltext_pdf>
	<start_page>8027</start_page>
	<end_page>8054</end_page>
	<publication_date>2005-09-05</publication_date>
	<article_title content_type="html">Chemical transformations in organic aerosol from biomass burning</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>A. Hoffer</name>
		</author>
		<author numeration="2" affiliations="2">
			<name>A. Gelencsér</name>
		</author>
		<author numeration="3" affiliations="3">
			<name>M. Blazsó</name>
		</author>
		<author numeration="4" affiliations="1">
			<name>P. Guyon</name>
		</author>
		<author numeration="5" affiliations="4">
			<name>P. Artaxo</name>
		</author>
		<author numeration="6" affiliations="1">
			<name>M. O. Andreae</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Max Planck Institute for Chemistry, Mainz, Germany</affiliation>
		<affiliation numeration="2" content_type="html">Air Chemistry Group of the Hungarian Academy of Sciences, Veszprém, Hungary</affiliation>
		<affiliation numeration="3" content_type="html">Institute of Materials and Environmental Chemistry CRC, Hungarian Academy of Sciences, Budapest, Hungary</affiliation>
		<affiliation numeration="4" content_type="html">Instituto de Fisica, Universidade de Sao Paulo, Sao Paulo, Brazil</affiliation>
	</affiliations>
	<abstract content_type="html">Fine aerosol particles were collected separately during daytime and
nighttime at a tropical pasture site in Rond&amp;#244;nia, Brazil, during the
burning and dry-to-wet transition period in 2002. Total carbon (TC) and
water-soluble organic carbon (WSOC) were measured by evolved gas analysis
(EGA). Based on the thermochemical properties of the fine aerosol, the
relative amounts of the low and higher molecular weight compounds were
estimated. It was found that the thermally refractory (possibly higher
molecular weight) compounds dominated the TC composition. Their contribution
to TC was higher in the daytime samples than in the nighttime ones. The
relative share of WSOC also showed a statistically significant diel
variation and so did its refractory fraction. Anhydrosugars and phenolic
acids were determined by GC-MS and their diel variation was studied. Based
on the decrease of their relative concentrations between the biomass burning
and transition periods and their distinctly different diel variations, we
suggest that the phenolic acids may undergo chemical transformations in the
aerosol phase, possibly towards more refractory compounds (humic-like
substances, HULIS), as has been suggested previously. These conclusions are
supported by the results of the thermally assisted hydrolysis and
methylation gas chromatography-mass spectrometry of the same filter samples.</abstract>
	<references>
	</references>
</article>

