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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-11-10803-2011</article-id>
<title-group>
<article-title>Chemical characteristics of inorganic ammonium salts in PM&lt;sub&gt;2.5&lt;/sub&gt;  in the atmosphere of Beijing (China)</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Ianniello</surname>
<given-names>A.</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>Spataro</surname>
<given-names>F.</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>Esposito</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>Allegrini</surname>
<given-names>I.</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>M.</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>T.</given-names>
</name>
<xref ref-type="aff" rid="aff3">
<sup>3</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>CNR – Institute of Atmospheric Pollution Research, Via Salaria Km 29.3, CP10, 00015 Monterotondo S., Rome, Italy</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>CO.R.AM – Consorzio Ricerche Ambientali, Ferrara, Italy</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>State Key Joint Laboratory for Environmental Simulation and Pollution Control, College of Environmental Sciences and Engineering, Peking University, Beijing, China</addr-line>
</aff>
<pub-date pub-type="epub">
<day>02</day>
<month>11</month>
<year>2011</year>
</pub-date>
<volume>11</volume>
<issue>21</issue>
<fpage>10803</fpage>
<lpage>10822</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/11/10803/2011/acp-11-10803-2011.html">This article is available from http://www.atmos-chem-phys.net/11/10803/2011/acp-11-10803-2011.html</self-uri>
<self-uri xlink:href="http://www.atmos-chem-phys.net/11/10803/2011/acp-11-10803-2011.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys.net/11/10803/2011/acp-11-10803-2011.pdf</self-uri>
<abstract>
<p>The atmospheric concentrations of gaseous HNO&lt;sub&gt;3&lt;/sub&gt;, HCl and NH&lt;sub&gt;3&lt;/sub&gt; and
their relative salts have been measured during two field campaigns in the
winter and in the summer of 2007 at Beijing (China), as part of CAREBEIJING
(Campaigns of Air Quality Research in Beijing and Surrounding Region). In
this study, annular denuder technique used with integration times of 2 and
24h to collect inorganic and soluble PM&lt;sub&gt;2.5&lt;/sub&gt; without interferences from
gas–particle and particle–particle interactions. The results were
discussed from the standpoint of temporal and diurnal variations and
meteorological effects. Fine particulate Cl&lt;sup&gt;&amp;minus;&lt;/sup&gt;, NH&lt;sub&gt;4&lt;/sub&gt;&lt;sup&gt;+&lt;/sup&gt; and
SO&lt;sub&gt;4&lt;/sub&gt;&lt;sup&gt;2&amp;minus;&lt;/sup&gt; exhibited distinct temporal variations, while fine
particulate NO&lt;sub&gt;3&lt;/sub&gt;&lt;sup&gt;&amp;minus;&lt;/sup&gt; did not show much variation with respect to
season. Daily mean concentrations of fine particulate NH&lt;sub&gt;4&lt;/sub&gt;&lt;sup&gt;+&lt;/sup&gt; and
SO&lt;sub&gt;4&lt;/sub&gt;&lt;sup&gt;2&amp;minus;&lt;/sup&gt; were higher during summer (12.30 μg m&lt;sup&gt;−3&lt;/sup&gt; and
18.24 μg m&lt;sup&gt;−3&lt;/sup&gt;, respectively) than during winter (6.51 μg m&lt;sup&gt;−3&lt;/sup&gt; and
7.50 μg m&lt;sup&gt;−3&lt;/sup&gt;, respectively). Daily mean concentrations of fine
particulate Cl&lt;sup&gt;&amp;minus;&lt;/sup&gt; were higher during winter (2.94 μg m&lt;sup&gt;&amp;minus;3&lt;/sup&gt;) than
during summer (0.79 μg m&lt;sup&gt;&amp;minus;3&lt;/sup&gt;), while fine particulate
NO&lt;sub&gt;3&lt;/sub&gt;&lt;sup&gt;&amp;minus;&lt;/sup&gt; showed similar both in winter (8.38 μg m&lt;sup&gt;&amp;minus;3&lt;/sup&gt;)
and in summer (9.62 μg m&lt;sup&gt;&amp;minus;3&lt;/sup&gt;) periods. The presence of large amounts of fine particulate
NO&lt;sub&gt;3&lt;/sub&gt;&lt;sup&gt;&amp;minus;&lt;/sup&gt; even in summer are due to higher local and regional
concentrations of NH&lt;sub&gt;3&lt;/sub&gt; in the atmosphere available to neutralize
H&lt;sub&gt;2&lt;/sub&gt;SO&lt;sub&gt;4&lt;/sub&gt; and HNO&lt;sub&gt;3&lt;/sub&gt;, which is consistent with the observation that
the measured particulate species were neutralized. The composition of fine
particulate matter indicated the domination of (NH&lt;sub&gt;4&lt;/sub&gt;)&lt;sub&gt;2&lt;/sub&gt;SO&lt;sub&gt;4&lt;/sub&gt;
during winter and summer periods. In addition, the high relative humidity
conditions in summer period seemed to dissolve a significant fraction of
HNO&lt;sub&gt;3&lt;/sub&gt; and NH&lt;sub&gt;3&lt;/sub&gt; enhancing fine particulate NO&lt;sub&gt;3&lt;/sub&gt;&lt;sup&gt;&amp;minus;&lt;/sup&gt; and
NH&lt;sub&gt;4&lt;/sub&gt;&lt;sup&gt;+&lt;/sup&gt; in the atmosphere. All measured particulate species showed
diurnal similar patterns during the winter and summer periods with higher
peaks in the early morning, especially in summer, when humid and stable
atmospheric conditions occurred. These diurnal variations were affected by
wind direction suggesting regional and local source influences. The fine
particulate species were correlated with NO&lt;sub&gt;x&lt;/sub&gt; and PM&lt;sub&gt;2.5&lt;/sub&gt;, supporting
the hypothesis that traffic may be also an important source of secondary
particles.</p>
</abstract>
<counts><page-count count="20"/></counts>
</article-meta>
</front>
<body/>
<back>
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