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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>3</issue_number>
		<publication_year>2005</publication_year>
	</journal>
	<doi>10.5194/acpd-5-3561-2005</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/5/3561/2005/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/5/3561/2005/acpd-5-3561-2005.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/5/3561/2005/acpd-5-3561-2005.pdf</fulltext_pdf>
	<start_page>3561</start_page>
	<end_page>3593</end_page>
	<publication_date>2005-06-01</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="2">
			<name>J. C. Chow</name>
		</author>
		<author numeration="3" affiliations="3">
			<name>S. C. Lee</name>
		</author>
		<author numeration="4" affiliations="1">
			<name>Y. Li</name>
		</author>
		<author numeration="5" affiliations="4">
			<name>S. W. Chen</name>
		</author>
		<author numeration="6" affiliations="1">
			<name>Z. S. An</name>
		</author>
		<author numeration="7" affiliations="5">
			<name>K. Fung</name>
		</author>
		<author numeration="8" affiliations="2">
			<name>J. G. Watson</name>
		</author>
		<author numeration="9" affiliations="1">
			<name>C. S. Zhu</name>
		</author>
		<author numeration="10" affiliations="1">
			<name>S. X. Liu</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">1State Key Laboratory of Loess &amp; Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences, Xi’an 710075, China</affiliation>
		<affiliation numeration="2" content_type="html">Desert Research Institute, Reno, USA</affiliation>
		<affiliation numeration="3" content_type="html">The Hong Kong Polytechnic University, Hong Kong, China</affiliation>
		<affiliation numeration="4" content_type="html">Tongji University, Shanghai 200 092, China</affiliation>
		<affiliation numeration="5" content_type="html">AtmAA Inc., Calabasas, CA, USA</affiliation>
	</affiliations>
	<abstract content_type="html">Continuous observation of atmospheric organic and elemental carbon (OC,
EC) were conducted at Xi&apos;an during high pollution seasons from September
2003 to February 2004. PM&lt;sub&gt;2.5&lt;/sub&gt; samples were collected on pre-fired
quartz-fiber filters with battery-powered mini-volume samplers every day and
PM&lt;sub&gt;10&lt;/sub&gt; samples were collected every third days. Three types of source
samples (i.e., coal-combustion, motor vehicle exhaust, and biomass burning)
were also collected during ambient sampling period. Ambient and source
samples were analyzed for OC and EC by thermal/optical reflectance (TOR)
following the Interagency Monitoring of Protected Visual Environments
(IMPROVE) protocol. The average PM&lt;sub&gt;2.5&lt;/sub&gt; OC concentrations in fall and
winter were 34.1&amp;plusmn;18.0 &amp;micro;g m&lt;sup&gt;-3&lt;/sup&gt; and 61.9&amp;plusmn;33.2 &amp;micro;g
m&lt;sup&gt;-3&lt;/sup&gt;, respectively, while EC were 11.3&amp;plusmn;6.9 &amp;micro;g m&lt;sup&gt;-3&lt;/sup&gt; and
12.3&amp;plusmn;5.3 &amp;micro;g m&lt;sup&gt;-3&lt;/sup&gt;, respectively. Most of OC and EC were
associated with fine particle (PM&lt;sub&gt;2.5&lt;/sub&gt;) mode. The OC and EC levels at
Xi&apos;an are higher than most urban cities in Asia. The OC and EC in fall were
found to be strongly correlated (R&lt;sup&gt;2&lt;/sup&gt;&amp;gt;0.9), with moderate correlation
in winter (R&lt;sup&gt;2&lt;/sup&gt;=0.66). The carbonaceous aerosol accounted for 48.8&amp;plusmn;10.1%
of the PM&lt;sub&gt;2.5&lt;/sub&gt; during fall and 45.9&amp;plusmn;7.5% during
winter. Average OC/EC ratio was 3.3 in fall and 5.1 in winter with
individual OC/EC ratios constantly exceeding 2.0. Elevated OC/EC ratios were
found during heating seasons with increased coal combustion. The
contribution of secondary organic carbon was not significant during winter.
The time series of OC and EC showed periodic variability. Traffic
contributes 5 and 7 day peaks in the spectrum, precipitation appears as a 10
day periodicity and biomass burning can be identified as a 24 day
periodicity. Total carbon (TC) was apportioned by absolute principal
component analysis (APCA) using the 8 carbon fraction data (OC1, OC2, OC3,
OC4, EC1, EC2, EC3, and OP [a pyrolyzed carbon fraction]). TC attributes
73% to gasoline exhaust, 23% to diesel exhaust, and 4% to biomass
burning during fall. However, TC attributes 44% each to gasoline exhaust
and coal burning, 9% to biomass burning, and 3% to diesel exhaust
during winter.</abstract>
	<references>
	</references>
</article>

