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<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>
<abbrev-journal-title abbrev-type="nlm-ta">Atmos. Chem. Phys.</abbrev-journal-title>
</journal-title-group>
<issn pub-type="epub">1680-7324</issn>
<publisher><publisher-name>Copernicus Publications</publisher-name>
<publisher-loc>Göttingen, Germany</publisher-loc>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.5194/acp-13-10095-2013</article-id>
<title-group>
<article-title>Insights on organic aerosol aging and the influence of coal combustion at a regional receptor site of central eastern China</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Hu</surname>
<given-names>W. W.</given-names>
</name>
<xref ref-type="aff" rid="aff4">
<sup>4</sup>
</xref>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Hu</surname>
<given-names>M.</given-names>
<ext-link>https://orcid.org/0000-0003-4816-9123</ext-link>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Yuan</surname>
<given-names>B.</given-names>
</name>
<xref ref-type="aff" rid="aff5">
<sup>5</sup>
</xref>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Jimenez</surname>
<given-names>J. L.</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>Tang</surname>
<given-names>Q.</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>Peng</surname>
<given-names>J. F.</given-names>
<ext-link>https://orcid.org/0000-0003-4753-087X</ext-link>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Hu</surname>
<given-names>W.</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>Shao</surname>
<given-names>M.</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>Wang</surname>
<given-names>M.</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>Zeng</surname>
<given-names>L. M.</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>Y. 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>Gong</surname>
<given-names>Z. H.</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Huang</surname>
<given-names>X. F.</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>He</surname>
<given-names>L. Y.</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>State Key Joint Laboratory of Environmental Simulation and Pollution Control, College of Environmental Sciences and Engineering, Peking University, Beijing 100871, China</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Key Laboratory for Urban Habitat Environmental Science and Technology, School of Environment and Energy, Peking University Shenzhen Graduate School, Shenzhen 518055, China</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>Cooperative Institute for Research in the Environmental Sciences (CIRES) and Department of Chemistry and Biochemistry, Univ. of Colorado, Boulder, CO, USA</addr-line>
</aff>
<aff id="aff4">
<label>4</label>
<addr-line>now at: Cooperative Institute for Research in Environmental Sciences, University of Colorado, Boulder, CO 80309, USA</addr-line>
</aff>
<aff id="aff5">
<label>5</label>
<addr-line>now at: Earth System Research Laboratory, Chemical Sciences Division, NOAA, 325 Broadway, Boulder, Colorado 80305, USA</addr-line>
</aff>
<pub-date pub-type="epub">
<day>15</day>
<month>10</month>
<year>2013</year>
</pub-date>
<volume>13</volume>
<issue>19</issue>
<fpage>10095</fpage>
<lpage>10112</lpage>
<permissions>
<copyright-statement>Copyright: &#x000a9; 2013 W. W. Hu et al.</copyright-statement>
<copyright-year>2013</copyright-year>
<license license-type="open-access">
<license-p>This work is licensed under the Creative Commons Attribution 3.0 Unported License. To view a copy of this licence, visit <ext-link ext-link-type="uri"  xlink:href="https://creativecommons.org/licenses/by/3.0/">https://creativecommons.org/licenses/by/3.0/</ext-link></license-p>
</license>
</permissions>
<self-uri xlink:href="https://acp.copernicus.org/articles/13/10095/2013/acp-13-10095-2013.html">This article is available from https://acp.copernicus.org/articles/13/10095/2013/acp-13-10095-2013.html</self-uri>
<self-uri xlink:href="https://acp.copernicus.org/articles/13/10095/2013/acp-13-10095-2013.pdf">The full text article is available as a PDF file from https://acp.copernicus.org/articles/13/10095/2013/acp-13-10095-2013.pdf</self-uri>
<abstract>
<p>In order to understand the aging and processing of organic aerosols (OA), an
intensive field campaign (&lt;b&gt;C&lt;/b&gt;ampaign of &lt;b&gt;A&lt;/b&gt;ir
&lt;b&gt;P&lt;/b&gt;ollution at &lt;b&gt;T&lt;/b&gt;ypical &lt;b&gt;C&lt;/b&gt;oastal
&lt;b&gt;A&lt;/b&gt;reas &lt;b&gt;IN&lt;/b&gt; Eastern China, CAPTAIN) was conducted
March–April at a receptor site (a Changdao island) in central eastern China.
Multiple fast aerosol and gas measurement instruments were used during the
campaign, including a high resolution time-of-flight aerosol mass
spectrometer (HR-ToF-AMS) that was applied to measure mass concentrations and
non-refractory chemical components of submicron particles (PM&lt;sub&gt;1&lt;/sub&gt;&lt;sup&gt;nr&lt;/sup&gt;).
The average mass concentration of PM&lt;sub&gt;1&lt;/sub&gt;(PM&lt;sub&gt;1&lt;/sub&gt;&lt;sup&gt;nr&lt;/sup&gt;+black
carbon) was 47 ± 36 μg m&lt;sup&gt;−3&lt;/sup&gt; during the campaign and showed
distinct variation, depending on back trajectories and their overlap with
source regions. Organic aerosol (OA) is the largest component of PM&lt;sub&gt;1&lt;/sub&gt;
(30%), followed by nitrate (28%), sulfate (19%), ammonium (15%),
black carbon (6%), and chloride (3%). Four OA components were resolved
by positive matrix factorization (PMF) of the high-resolution spectra,
including low-volatility oxygenated organic aerosol (LV-OOA), semi-volatile
oxygenated OA (SV-OOA), hydrocarbon-like OA (HOA) and a coal combustion OA
(CCOA). The mass spectrum of CCOA had high abundance of fragments from
polycyclic aromatic hydrocarbons (PAHs) (&lt;i&gt;m/z&lt;/i&gt; 128, 152, 178, etc.). The average
atomic ratio of oxygen to carbon in OA (O / C) at Changdao was 0.59, which is
comparable to other field studies reported at locations downwind of large
pollution sources, indicating the oxidized nature of most OA during the
campaign. The evolution of OA elemental composition in the van Krevelen
diagram (H / C vs. O / C) showed a slope of −0.63; however, the OA influenced by
coal combustion exhibits a completely different evolution that appears
dominated by physical mixing. The aging of organic aerosols vs.
photochemical age was investigated. It was shown that OA / ΔCO, as well
as LV-OOA / ΔCO and SV-OOA / ΔCO, positively correlated with
photochemical age. LV-OOA accounted for 73% of the OA secondary formation
(SOA) in the oldest plumes (photochemical age of 25 h). The &lt;i&gt;k&lt;/i&gt;&lt;sub&gt;OH&lt;/sub&gt; at
Changdao, by assuming SOA formation and aging as a first-order process
proportional to OH, was calculated to be 5.2 &amp;times; 10&lt;sup&gt;&amp;minus;12&lt;/sup&gt; cm&lt;sup&gt;3&lt;/sup&gt; molec.&lt;sup&gt;−1&lt;/sup&gt; s&lt;sup&gt;−1&lt;/sup&gt;, which is similar to those determined
in recent studies of polluted air in other continents.</p>
</abstract>
<counts><page-count count="18"/></counts>
</article-meta>
</front>
<body/>
<back>
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