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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-10-6087-2010</article-id>
<title-group>
<article-title>Dicarboxylic acids, metals and isotopic compositions of C and N in atmospheric aerosols from inland China: implications for dust and coal burning emission and secondary aerosol formation</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Wang</surname>
<given-names>G.</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>Xie</surname>
<given-names>M.</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Hu</surname>
<given-names>S.</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Gao</surname>
<given-names>S.</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Tachibana</surname>
<given-names>E.</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>Kawamura</surname>
<given-names>K.</given-names>
</name>
<xref ref-type="aff" rid="aff3">
<sup>3</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences, Xi&apos;an 710075, China</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>State Key Laboratory of Pollution Control and Resources Reuse, Nanjing University, Nanjing 210093, China</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>Institute of Low Temperature Science, Hokkaido Unversity, Sapporo 060-0819, Japan</addr-line>
</aff>
<pub-date pub-type="epub">
<day>06</day>
<month>07</month>
<year>2010</year>
</pub-date>
<volume>10</volume>
<issue>13</issue>
<fpage>6087</fpage>
<lpage>6096</lpage>
<permissions>
<copyright-statement>Copyright: &#x000a9; 2010 G. Wang et al.</copyright-statement>
<copyright-year>2010</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/10/6087/2010/acp-10-6087-2010.html">This article is available from https://acp.copernicus.org/articles/10/6087/2010/acp-10-6087-2010.html</self-uri>
<self-uri xlink:href="https://acp.copernicus.org/articles/10/6087/2010/acp-10-6087-2010.pdf">The full text article is available as a PDF file from https://acp.copernicus.org/articles/10/6087/2010/acp-10-6087-2010.pdf</self-uri>
<abstract>
<p>Dicarboxylic acids (C&lt;sub&gt;2&lt;/sub&gt;–C&lt;sub&gt;10&lt;/sub&gt;), metals, elemental
carbon (EC), organic carbon (OC), and stable isotopic compositions of total
carbon (TC) and total nitrogen (TN) were determined for PM&lt;sub&gt;10&lt;/sub&gt; samples
collected at three urban and one suburban sites of Baoji, an inland city of
China, during winter and spring 2008. Oxalic acid (C&lt;sub&gt;2&lt;/sub&gt;) was the dominant
diacid, followed by succinic (C&lt;sub&gt;4&lt;/sub&gt;) and malonic (C&lt;sub&gt;3&lt;/sub&gt;) acids. Total
diacids in the urban and suburban areas were 1546&amp;plusmn;203 and 1728&amp;plusmn;495 ng m&lt;sup&gt;−3&lt;/sup&gt; during winter
and 1236&amp;plusmn;335 and 1028&amp;plusmn;193 ng m&lt;sup&gt;−3&lt;/sup&gt; during spring. EC in the urban and the suburban atmospheres were
17&amp;plusmn;3.8 and 8.0&amp;plusmn;2.1 μg m&lt;sup&gt;−3&lt;/sup&gt; during winter and 20&amp;plusmn;5.9
and 7.1&amp;plusmn;2.7 μg m&lt;sup&gt;−3&lt;/sup&gt; during spring, while OC at the urban
and suburban sites were 74&amp;plusmn;14 and 51&amp;plusmn;7.9 μg m&lt;sup&gt;−3&lt;/sup&gt; in
winter and 51&amp;plusmn;20 and 23&amp;plusmn;6.1 μg m&lt;sup&gt;−3&lt;/sup&gt; in spring.
Secondary organic carbon (SOC) accounted for 38&amp;plusmn;16% of OC in
winter and 28&amp;plusmn;18% of OC in spring, suggesting an enhanced
photochemical production of secondary organic aerosols in winter under an
inversion layer development. Total metal elements in winter and spring were
34&amp;plusmn;10 and 61&amp;plusmn;27 μg m&lt;sup&gt;−3&lt;/sup&gt; in the urban air and 18&amp;plusmn;7
and 32&amp;plusmn;23 μg m&lt;sup&gt;−3&lt;/sup&gt; in the suburban air. A linear
correlation (&lt;i&gt;r&lt;/i&gt;&lt;sup&gt;2&lt;/sup&gt;&gt;0.8 in winter and &lt;i&gt;r&lt;/i&gt;&lt;sup&gt;2&lt;/sup&gt;&gt;0.6 in spring) was
found between primary organic carbon (POC) and Ca&lt;sup&gt;2+&lt;/sup&gt;/Fe, together with a
strong dependence of pH value of sample extracts on water-soluble inorganic
carbon, suggesting fugitive dust as an important source of the airborne
particles. Polycyclic aromatic hydrocarbons (PAHs), sulfate, and Pb in the
samples well correlated each other (&lt;i&gt;r&lt;/i&gt;&lt;sup&gt;2&lt;/sup&gt;&gt;0.6) in winter, indicating
an importance of emissions from coal burning for house heating. Stable
carbon isotope compositions of TC (&amp;delta;&lt;sup&gt;13&lt;/sup&gt;C) became higher
with an increase in the concentration ratios of C&lt;sub&gt;2&lt;/sub&gt;/OC due to aerosol
aging. In contrast, nitrogen isotope compositions of TN (&amp;delta;&lt;sup&gt;15&lt;/sup&gt;N) became lower with an increases in the mass ratios of
NH&lt;sub&gt;4&lt;/sub&gt;&lt;sup&gt;+&lt;/sup&gt;/PM&lt;sub&gt;10&lt;/sub&gt; and NO&lt;sub&gt;3&lt;/sub&gt;&lt;sup&gt;&amp;minus;&lt;/sup&gt;/PM&lt;sub&gt;10&lt;/sub&gt;, which is possibly
caused by an enhanced adsorption and/or condensation of gaseous NH&lt;sub&gt;3&lt;/sub&gt; and
HNO&lt;sub&gt;3&lt;/sub&gt; onto particles.</p>
</abstract>
<counts><page-count count="10"/></counts>
</article-meta>
</front>
<body/>
<back>
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