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<article xmlns:mml="http://www.w3.org/1998/Math/MathML" xmlns:xlink="http://www.w3.org/1999/xlink" article-type="research-article" dtd-version="3.0" xml:lang="en">
<front>
<journal-meta>
<journal-id journal-id-type="publisher">ACP</journal-id>
<journal-title-group>
<journal-title>Atmospheric Chemistry and Physics</journal-title>
<abbrev-journal-title abbrev-type="publisher">ACP</abbrev-journal-title>
</journal-title-group>
<issn pub-type="epub">1680-7324</issn>
<publisher><publisher-name>Copernicus GmbH</publisher-name>
<publisher-loc>Göttingen, Germany</publisher-loc>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.5194/acp-5-3127-2005</article-id>
<title-group>
<article-title>Characterization and source apportionment of atmospheric organic and elemental carbon during fall and winter of 2003 in Xi&apos;an, China</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Cao</surname>
<given-names>J. J.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Wu</surname>
<given-names>F.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Chow</surname>
<given-names>J. C.</given-names>
</name>
<xref ref-type="aff" rid="aff3">
<sup>3</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Lee</surname>
<given-names>S. C.</given-names>
</name>
<xref ref-type="aff" rid="aff4">
<sup>4</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Li</surname>
<given-names>Y.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Chen</surname>
<given-names>S. W.</given-names>
</name>
<xref ref-type="aff" rid="aff5">
<sup>5</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>An</surname>
<given-names>Z. S.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Fung</surname>
<given-names>K. K.</given-names>
</name>
<xref ref-type="aff" rid="aff6">
<sup>6</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Watson</surname>
<given-names>J. G.</given-names>
</name>
<xref ref-type="aff" rid="aff3">
<sup>3</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Zhu</surname>
<given-names>C. S.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Liu</surname>
<given-names>S. X.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>SKLLQG, Institute of Earth Environment, Chinese Academy of Sciences, Xi’an 710075, China</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>The Graduate School of Chinese academy of Sciences, Beijing 100049, China</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>Desert Research Institute, Reno, Nevada, USA</addr-line>
</aff>
<aff id="aff4">
<label>4</label>
<addr-line>The Hong Kong Polytechnic University, Hong Kong, China</addr-line>
</aff>
<aff id="aff5">
<label>5</label>
<addr-line>Tongji University, Shanghai 200092, China</addr-line>
</aff>
<aff id="aff6">
<label>6</label>
<addr-line>Atmoslytic, Inc., Calabasas, CA, USA</addr-line>
</aff>
<pub-date pub-type="epub">
<day>22</day>
<month>11</month>
<year>2005</year>
</pub-date>
<volume>5</volume>
<issue>11</issue>
<fpage>3127</fpage>
<lpage>3137</lpage>
<permissions>
<license xlink:type="simple">
<license-p>This is an open-access article ditributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited.</license-p>
</license>
</permissions>
<self-uri xlink:href="http://www.atmos-chem-phys.net/5/3127/2005/acp-5-3127-2005.html">This article is available from http://www.atmos-chem-phys.net/5/3127/2005/acp-5-3127-2005.html</self-uri>
<self-uri xlink:href="http://www.atmos-chem-phys.net/5/3127/2005/acp-5-3127-2005.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys.net/5/3127/2005/acp-5-3127-2005.pdf</self-uri>
<abstract>
<p>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.</p>
</abstract>
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