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<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>9</volume_number>
		<issue_number>1</issue_number>
		<publication_year>2009</publication_year>
	</journal>
	<doi>10.5194/acpd-9-4567-2009</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/9/4567/2009/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/9/4567/2009/acpd-9-4567-2009.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/9/4567/2009/acpd-9-4567-2009.pdf</fulltext_pdf>
	<start_page>4567</start_page>
	<end_page>4607</end_page>
	<publication_date>2009-02-23</publication_date>
	<article_title content_type="html">Oxygenated organic functional groups and their sources in single and submicron organic particles in MILAGRO 2006 campaign</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>S. Liu</name>
		</author>
		<author numeration="2" affiliations="1">
			<name>S. Takahama</name>
		</author>
		<author numeration="3" affiliations="1">
			<name>L. M. Russell</name>
			<email>lmrussell@ucsd.edu</email>
		</author>
		<author numeration="4" affiliations="1,2">
			<name>S. Gilardoni</name>
		</author>
		<author numeration="5" affiliations="3">
			<name>D. Baumgardner</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Scripps Institution of Oceanography, Univ. of California, San  Diego, La Jolla, California, USA</affiliation>
		<affiliation numeration="2" content_type="html">Joint Research Centre, European  Commission, Ispra, Italy</affiliation>
		<affiliation numeration="3" content_type="html">Centro de Ciencias de la  Atmósfera, Univ. Nacional Autónoma de México, México City, México</affiliation>
	</affiliations>
	<abstract content_type="html">Fourier Transform Infrared (FTIR) and X-ray Fluorescence (XRF) were used to
measure organic functional groups and elements of submicron particles
collected during MILAGRO in March 2006 on three platforms: the Mexico City
urban area (SIMAT), the high altitude site at 4010 m (Altzomoni), and the
NCAR C130 aircraft. Scanning transmission X-ray Microscopy (STXM) and
Near-Edge X-ray Absorption Fine Structure (NEXAFS) were applied to single
particle organic functional group abundance analysis of particles
simultaneously collected at SIMAT and C130. Correlations of elemental
concentrations showed different groups of source related elements at SIMAT,
Altzomoni, and C130, suggesting different processes affecting the air masses
sampled at the three platforms. Cluster analysis resulted in seven distinct
Clusters of FTIR spectra, with the last three clusters consisting of spectra
collected almost exclusively on the C130 platform, reflecting the variety of
sources contributing to C130 samples. Positive Matrix Factorization (PMF) of
NEXAFS-STXM spectra identified three main factors representing soot,
secondary, and biomass burning type spectra. PMF of FTIR spectra resulted in
three fossil fuel combustion type factors, one biomass burning factor, and
one mixed or processed factor. The fossil fuel combustion type factors were
found to have the largest contributions to OM, while the processed factor has
the largest O/C among all factors. Alkane, carboxylic acid, and amine
functional groups were mainly associated with combustion related sources,
while alcohol groups were likely from atmospheric processing of mixed
sources. While the processed factor has the highest O/C, half of the OM and
O/C measured could be attributed directly to fossil fuel combustion sources.
Both PMF of NEXAFS-STXM spectra and PMF of FTIR spectra indicate that the
combustion type factors are more affected by fluctuations in local sources,
while the processed factors are more consistent during the sampling period.</abstract>
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</article>

