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<!DOCTYPE article SYSTEM "http://www.atmos-chem-phys.net/inc/acp/copernicus.dtd">
<article language="en">
	<journal>
		<journal_title>Atmospheric Chemistry and Physics</journal_title>
		<journal_url>www.atmos-chem-phys.net</journal_url>
		<issn>1680-7316</issn>
		<eissn>1680-7324</eissn>
		<volume_number>5</volume_number>
		<issue_number>11</issue_number>
		<publication_year>2005</publication_year>
	</journal>
	<doi>10.5194/acp-5-3127-2005</doi>
	<article_url>http://www.atmos-chem-phys.net/5/3127/2005/</article_url>
	<abstract_html>http://www.atmos-chem-phys.net/5/3127/2005/acp-5-3127-2005.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys.net/5/3127/2005/acp-5-3127-2005.pdf</fulltext_pdf>
	<start_page>3127</start_page>
	<end_page>3137</end_page>
	<publication_date>2005-11-22</publication_date>
	<article_title content_type="html">Characterization and source apportionment of atmospheric organic and elemental carbon during fall and winter of 2003 in Xi&apos;an, China</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>J. J. Cao</name>
		</author>
		<author numeration="2" affiliations="1,2">
			<name>F. Wu</name>
		</author>
		<author numeration="3" affiliations="3">
			<name>J. C. Chow</name>
		</author>
		<author numeration="4" affiliations="4">
			<name>S. C. Lee</name>
		</author>
		<author numeration="5" affiliations="1">
			<name>Y. Li</name>
		</author>
		<author numeration="6" affiliations="5">
			<name>S. W. Chen</name>
		</author>
		<author numeration="7" affiliations="1">
			<name>Z. S. An</name>
		</author>
		<author numeration="8" affiliations="6">
			<name>K. K. Fung</name>
		</author>
		<author numeration="9" affiliations="3">
			<name>J. G. Watson</name>
		</author>
		<author numeration="10" affiliations="1">
			<name>C. S. Zhu</name>
		</author>
		<author numeration="11" affiliations="1">
			<name>S. X. Liu</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">SKLLQG, Institute of Earth Environment, Chinese Academy of Sciences, Xi’an 710075, China</affiliation>
		<affiliation numeration="2" content_type="html">The Graduate School of Chinese academy of Sciences, Beijing 100049, China</affiliation>
		<affiliation numeration="3" content_type="html">Desert Research Institute, Reno, Nevada, USA</affiliation>
		<affiliation numeration="4" content_type="html">The Hong Kong Polytechnic University, Hong Kong, China</affiliation>
		<affiliation numeration="5" content_type="html">Tongji University, Shanghai 200092, China</affiliation>
		<affiliation numeration="6" content_type="html">Atmoslytic, Inc., Calabasas, CA, USA</affiliation>
	</affiliations>
	<abstract content_type="html">Continuous measurements of atmospheric organic and elemental carbon (OC and
EC) were taken during the high-pollution fall and winter seasons at Xi&apos;an,
Shaanxi Province, China from September 2003 through February 2004.
Battery-powered mini-volume samplers collected PM&lt;sub&gt;2.5&lt;/sub&gt; samples daily and
PM&lt;sub&gt;10&lt;/sub&gt; samples every third day. Samples were also obtained from the
plumes of residential coal combustion, motor-vehicle exhaust, and biomass
burning sources. These samples were analyzed for OC/EC by thermal/optical
reflectance (TOR) following the Interagency Monitoring of Protected Visual
Environments (IMPROVE) protocol. OC and EC levels at Xi&apos;an are higher than
most urban cities in Asia. Average PM&lt;sub&gt;2.5&lt;/sub&gt; OC concentrations in fall and
winter were 34.1&amp;plusmn;18.0 &amp;mu;g m&lt;sup&gt;&amp;minus;3&lt;/sup&gt; and 61.9&amp;plusmn;;33.2 &amp;mu;g m&lt;sup&gt;&amp;minus;3&lt;/sup&gt;,
respectively; while EC concentrations were 11.3&amp;plusmn;6.9 &amp;mu;g m&lt;sup&gt;&amp;minus;3&lt;/sup&gt;
and 12.3&amp;plusmn;5.3 &amp;mu;g m&lt;sup&gt;&amp;minus;3&lt;/sup&gt;, respectively. Most of the OC
and EC were in the PM&lt;sub&gt;2.5&lt;/sub&gt; fraction. OC was strongly correlated (R&amp;gt;0.95)
with EC in the autumn and moderately correlated (R=0.81) with EC
during winter. Carbonaceous aerosol (OC&amp;times;1.6+EC) accounted for
48.8%&amp;plusmn;10.1% of the PM&lt;sub&gt;2.5&lt;/sub&gt; mass during fall and 45.9&amp;plusmn;7.5%
during winter. The average OC/EC ratio was 3.3 in fall and 5.1 in
winter, with individual OC/EC ratios nearly always exceeding 2.0. The higher
wintertime OC/EC corresponded to increased residential coal combustion for
heating. Total carbon (TC) was associated with source contributions using
absolute principal component analysis (APCA) with eight thermally-derived
carbon fractions. During fall, 73% of TC was attributed to gasoline
engine exhaust, 23% to diesel exhaust, and 4% to biomass burning.
During winter, 44% of TC was attributed to gasoline engine exhaust,
44% to coal burning, 9% to biomass burning, and 3% to diesel engine
exhaust.</abstract>
	<references>
	</references>
</article>

