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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>10</volume_number>
		<issue_number>3</issue_number>
		<publication_year>2010</publication_year>
	</journal>
	<doi>10.5194/acpd-10-6567-2010</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/10/6567/2010/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/10/6567/2010/acpd-10-6567-2010.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/10/6567/2010/acpd-10-6567-2010.pdf</fulltext_pdf>
	<start_page>6567</start_page>
	<end_page>6639</end_page>
	<publication_date>2010-03-09</publication_date>
	<article_title content_type="html">Major components of atmospheric organic aerosol in southern California as determined by hourly measurements of source marker compounds</article_title>
	<authors>
		<author numeration="1" affiliations="1,2,3">
			<name>B. J. Williams</name>
			<email>brentw@me.umn.edu</email>
		</author>
		<author numeration="2" affiliations="1,4">
			<name>A. H. Goldstein</name>
		</author>
		<author numeration="3" affiliations="5">
			<name>N. M. Kreisberg</name>
		</author>
		<author numeration="4" affiliations="5">
			<name>S. V. Hering</name>
		</author>
		<author numeration="5" affiliations="2,6,7,8">
			<name>D. R. Worsnop</name>
		</author>
		<author numeration="6" affiliations="9,10">
			<name>I. M. Ulbrich</name>
		</author>
		<author numeration="7" affiliations="11">
			<name>K. S. Docherty</name>
		</author>
		<author numeration="8" affiliations="9,10">
			<name>J. L. Jimenez</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Dept. of Environmental Science, Policy, and Management, University of California, 147 Mulford Hall, Berkeley, CA, USA</affiliation>
		<affiliation numeration="2" content_type="html">Center for Aerosol and Cloud Chemistry, Aerodyne Research Inc., 45 Manning Rd., Billerica, MA, USA</affiliation>
		<affiliation numeration="3" content_type="html">Dept. of Mechanical Engineering, University of Minnesota, 271 Mechanical Engineering, 111 Church Street S.E., Minneapolis, MN, USA</affiliation>
		<affiliation numeration="4" content_type="html">Dept. of Civil and Environmental Engineering, University of California, 147 Mulford Hall, Berkeley, CA, USA</affiliation>
		<affiliation numeration="5" content_type="html">Aerosol Dynamics Inc., 935 Grayson St., Berkeley, CA, USA</affiliation>
		<affiliation numeration="6" content_type="html">Department of Physics, University of Kuopio, Kuopio, Finland</affiliation>
		<affiliation numeration="7" content_type="html">Finnish Meteorological Institute, Helsinki, Finland</affiliation>
		<affiliation numeration="8" content_type="html">Department of Physics, University of Helsinki, Helsinki, Finland</affiliation>
		<affiliation numeration="9" content_type="html">Department of Chemistry and Biochemistry, University of Colorado, Boulder, CO, USA</affiliation>
		<affiliation numeration="10" content_type="html">Cooperative Institute for Research in the Environmental Sciences, Boulder, CO, USA</affiliation>
		<affiliation numeration="11" content_type="html">now at: Alion Science and Technology, EPA Office of Research and Development, EPA Research and Development, Research Triangle Park, NC, USA</affiliation>
	</affiliations>
	<abstract content_type="html">We report the first hourly in-situ measurements of speciated organic aerosol
(OA) composition in an urban environment. Field measurements were made in
southern California at the University of Californiaâ€“Riverside during the
2005 Study of Organic Aerosol at Riverside (SOAR), which included two
separate measurement periods: a summer study (15 Julyâ€“15 August) and a
fall study (31 Octoberâ€“28 November). Hourly measurements of over 300
semivolatile and nonvolatile organic compounds were made using the thermal
desorption aerosol gas chromatograph (TAG). Positive matrix factorization
(PMF) was performed on a subset of these compounds to identify major
components contributing to submicron (i.e., PM&lt;sub&gt;1&lt;/sub&gt;) OA at the site, as
measured by an aerosol mass spectrometer (AMS). PMF analysis was performed
on an 11-day focus period in each season, representing average seasonal
conditions during the summer and a period of urban influence during the
fall. As a result of this analysis, we identify multiple types of primary
and secondary OA (POA and SOA). Secondary sources contribute substantially
to fine OA mass at Riverside, which commonly receives regional air masses
that pass through metropolitan Los Angeles during the summer. Four
individual summertime SOA components are defined, and when combined, they
contribute an average 88% of the total fine OA mass during summer
afternoons. These sources appear to be mostly from the oxidation of
anthropogenic precursor gases, with one SOA component having contributions
from oxygenated biogenics. During the fall, three out of four aerosol
components which contain SOA are inseparable from covarying primary
emissions, and therefore we can not estimate the fraction of total OA that
is secondary in nature during the fall study. Identified primary OA
components are attributed to vehicle emissions, food cooking, primary
biogenics, and biomass burning aerosol. While a distinction between local
and regional vehicle emissions is made, a combination of these two factors
accounted for approximately 11% of observed submicron OA during both
sampling periods. Food cooking operations contributed ~10% of
submicron OA mass during the summer, but was not separable from SOA during
the fall due to high covariance of sources. Biomass burning aerosol
contributed a larger fraction of fine OA mass during the fall (~11%) than compared to summer (~7%). Primary biogenic aerosol
was also identified during the summer, contributing ~1% of the OA,
but not during the fall. While the contribution of both local and regional
primary vehicle OA accounts for only ~11% of total OA during both
seasons, gas-phase vehicle emissions likely create a substantial fraction of
the observed SOA as a result of atmospheric processing.</abstract>
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