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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>
</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-11-6139-2011</article-id>
<title-group>
<article-title>Characteristics of atmospheric ammonia over Beijing, China</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Meng</surname>
<given-names>Z. 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>Lin</surname>
<given-names>W. L.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
<xref ref-type="aff" rid="aff4">
<sup>4</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Jiang</surname>
<given-names>X. 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>Yan</surname>
<given-names>P.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
<xref ref-type="aff" rid="aff4">
<sup>4</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Wang</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>Zhang</surname>
<given-names>Y. 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>Jia</surname>
<given-names>X. F.</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>Yu</surname>
<given-names>X. L.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Key Laboratory for Atmospheric Chemistry, Center for Atmospheric Watch and Services, Chinese Academy of Meteorological Sciences, Beijing, China</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Tsinghua University, Beijing, China</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>Department of Environmental Engineering, School of Civil and Environmental Engineering, University of Science and Technology Beijing, Beijing, China</addr-line>
</aff>
<aff id="aff4">
<label>4</label>
<addr-line>Meteorological Observation Centre, China Meteorological Administration, Beijing, China</addr-line>
</aff>
<pub-date pub-type="epub">
<day>29</day>
<month>06</month>
<year>2011</year>
</pub-date>
<volume>11</volume>
<issue>12</issue>
<fpage>6139</fpage>
<lpage>6151</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/11/6139/2011/acp-11-6139-2011.html">This article is available from http://www.atmos-chem-phys.net/11/6139/2011/acp-11-6139-2011.html</self-uri>
<self-uri xlink:href="http://www.atmos-chem-phys.net/11/6139/2011/acp-11-6139-2011.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys.net/11/6139/2011/acp-11-6139-2011.pdf</self-uri>
<abstract>
<p>Continuous measurements of atmospheric ammonia (NH&lt;sub&gt;3&lt;/sub&gt;) were conducted
using Ogawa passive samplers from February 2008 to July 2010 at an urban
site and from January 2007 to July 2010 at a rural site in Beijing, China.
NH&lt;sub&gt;4&lt;/sub&gt;&lt;sup&gt;+&lt;/sup&gt; in fine particles was also collected at the rural site during
2008–2009. The field comparison between the Ogawa passive samplers and an
active analyzer for NH&lt;sub&gt;3&lt;/sub&gt; conducted at the urban site assures the quality
and accuracy of the measurements. The concentrations of NH&lt;sub&gt;3&lt;/sub&gt; at the
urban site ranged from 0.7 to 85.1 ppb, with the annual average of 18.5 ± 13.8
and 23.5 &amp;plusmn;  18.0 ppb in 2008 and 2009, respectively. The 
NH&lt;sub&gt;3&lt;/sub&gt; concentrations at the rural site were lower than those at urban site, and
varied from 0.8 to 42.9 ppb, with the annual average of 4.5 &amp;plusmn; 4.6,
6.6 &amp;plusmn;  7.0 and 7.1 &amp;plusmn;  3.5 ppb in 2007, 2008 and 2009, respectively. The
data showed marked seasonal variations at both sites. The results emphasized
traffic to be a significant source of NH&lt;sub&gt;3&lt;/sub&gt; concentrations in winter in
urban areas of Beijing. This was illustrated by the strong correlations of
NH&lt;sub&gt;3&lt;/sub&gt; with the traffic related pollutants (NO&lt;sub&gt;x&lt;/sub&gt; and CO) and also by the
bimodal diurnal cycle of NH&lt;sub&gt;3&lt;/sub&gt; concentrations that was synchronized with
traffic. Similar patterns were not observed during the summer, suggesting
other non-traffic sources became more important. At the rural site, the
daily NH&lt;sub&gt;4&lt;/sub&gt;&lt;sup&gt;+&lt;/sup&gt; concentrations ranged from 0.10 to 36.53 μg m&lt;sup&gt;−3&lt;/sup&gt;,
with an average of 7.03 μg m&lt;sup&gt;−3&lt;/sup&gt; from June 2008 to
December 2009. Monthly NH&lt;sub&gt;3&lt;/sub&gt; were significantly correlated with
NH&lt;sub&gt;4&lt;/sub&gt;&lt;sup&gt;+&lt;/sup&gt; concentrations. Average monthly NH&lt;sub&gt;3&lt;/sub&gt;/NH&lt;sub&gt;4&lt;/sub&gt;&lt;sup&gt;+&lt;/sup&gt;
ratios varied from 0.13 to 2.28, with an average of 0.73. NH&lt;sub&gt;4&lt;/sub&gt;&lt;sup&gt;+&lt;/sup&gt; in PM&lt;sub&gt;2.5&lt;/sub&gt;
 was primarily associated with SO&lt;sub&gt;4&lt;/sub&gt;&lt;sup&gt;&amp;minus;2&lt;/sup&gt; at the rural site.</p>
</abstract>
<counts><page-count count="13"/></counts>
</article-meta>
</front>
<body/>
<back>
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