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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-11-6593-2011</article-id>
<title-group>
<article-title>Effects of temperature on the heterogeneous oxidation of sulfur dioxide by ozone on calcium carbonate</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Wu</surname>
<given-names>L. 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>Tong</surname>
<given-names>S. R.</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>W. 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>Ge</surname>
<given-names>M. F.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Beijing National Laboratory for Molecular Sciences (BNLMS), State Key Laboratory for Structural Chemistry of Unstable and Stable Species, Institute of Chemistry, Chinese Academy of Sciences, 100190, Beijing, China</addr-line>
</aff>
<pub-date pub-type="epub">
<day>12</day>
<month>07</month>
<year>2011</year>
</pub-date>
<volume>11</volume>
<issue>13</issue>
<fpage>6593</fpage>
<lpage>6605</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/11/6593/2011/acp-11-6593-2011.html">This article is available from http://www.atmos-chem-phys.net/11/6593/2011/acp-11-6593-2011.html</self-uri>
<self-uri xlink:href="http://www.atmos-chem-phys.net/11/6593/2011/acp-11-6593-2011.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys.net/11/6593/2011/acp-11-6593-2011.pdf</self-uri>
<abstract>
<p>The heterogeneous oxidation of sulfur dioxide by ozone on CaCO&lt;sub&gt;3&lt;/sub&gt; was
studied as a function of temperature (230 to 298 K) at ambient
pressure. Oxidation reactions were followed in real time using diffuse
reflectance infrared Fourier transform spectrometry (DRIFTS) to obtain
kinetic and mechanistic data. From the analysis of the spectral features,
the formation of sulfate was identified on the surface in the presence of
O&lt;sub&gt;3&lt;/sub&gt; and SO&lt;sub&gt;2&lt;/sub&gt; at different temperatures from 230 to 298 K. The
results showed that the heterogeneous oxidation and the rate of sulfate
formation were sensitive to temperature. An interesting stage-transition
region was observed at temperatures ranging from 230 to 257 K, but it became
ambiguous gradually above 257 K. The reactive uptake coefficients at
different temperatures from 230 to 298 K were acquired for the first time,
which can be used directly in atmospheric chemistry modeling studies to
predict the formation of secondary sulfate aerosol in the troposphere.
Furthermore, the rate of sulfate formation had a turning point at about 250 K.
The sulfate concentration at 250 K was about twice as large as that at
298 K. The rate of sulfate formation increased with decreasing temperature
at temperatures above 250 K, while there is a contrary temperature effect at
temperatures below 250 K. The activation energy for heterogeneous oxidation
at temperatures from 245 K to 230 K was determined to be 14.63 &amp;plusmn; 0.20 kJ mol&lt;sup&gt;−1&lt;/sup&gt;.
A mechanism for the temperature dependence was proposed and the
atmospheric implications were discussed.</p>
</abstract>
<counts><page-count count="13"/></counts>
</article-meta>
</front>
<body/>
<back>
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