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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-3-2043-2003</article-id>
<title-group>
<article-title>DRIFTS and Knudsen cell study of the heterogeneous reactivity of SO&lt;sub&gt;2&lt;/sub&gt; and NO&lt;sub&gt;2&lt;/sub&gt; on mineral dust</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Ullerstam</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>Johnson</surname>
<given-names>M. 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>Vogt</surname>
<given-names>R.</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>Ljungström</surname>
<given-names>E.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Gothenburg University, Department of Chemistry, SE-41296 Gothenburg, Sweden</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Copenhagen University, Department of Chemistry, Universitetsparken 5, DK-2100 Copenhagen, Denmark</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>Ford Forschungszentrum GmbH Aachen, Süsterfeldstrasse 200, D-52072 Aachen, Germanyhagen</addr-line>
</aff>
<pub-date pub-type="epub">
<day>25</day>
<month>11</month>
<year>2003</year>
</pub-date>
<volume>3</volume>
<issue>6</issue>
<fpage>2043</fpage>
<lpage>2051</lpage>
<permissions>
<copyright-statement>Copyright: &#x000a9; 2003 M. Ullerstam et al.</copyright-statement>
<copyright-year>2003</copyright-year>
<license license-type="open-access">
<license-p>This work is licensed under the Creative Commons Attribution-NonCommercial-ShareAlike 2.5 Generic License. To view a copy of this licence, visit <ext-link ext-link-type="uri"  xlink:href="https://creativecommons.org/licenses/by-nc-sa/2.5/">https://creativecommons.org/licenses/by-nc-sa/2.5/</ext-link></license-p>
</license>
</permissions>
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<self-uri xlink:href="https://acp.copernicus.org/articles/3/2043/2003/acp-3-2043-2003.pdf">The full text article is available as a PDF file from https://acp.copernicus.org/articles/3/2043/2003/acp-3-2043-2003.pdf</self-uri>
<abstract>
<p>The heterogeneous oxidation of
      SO&lt;sub&gt;2&lt;/sub&gt; by NO&lt;sub&gt;2&lt;/sub&gt; on mineral dust was studied using Diffuse
      Reflectance Infrared Fourier Transform Spectroscopy (DRIFTS) and a Knudsen cell. This
      made it possible to characterise, kinetically, both the formation of sulfate and nitrate as
      surface products and the gas phase loss of the reactive species. The gas phase loss rate was
      determined to be first order in both SO&lt;sub&gt;2&lt;/sub&gt; and
      NO&lt;sub&gt;2&lt;/sub&gt;. From the DRIFTS experiment the uptake
      coefficient, &lt;font face=&quot;Symbol&quot;&gt;g&lt;/font&gt;, for the formation of sulfate was determined to be of the order of
      10&lt;sup&gt;-10&lt;/sup&gt; using the BET area as the reactive surface area. No significant formation of sulfate was seen in the
      absence of NO&lt;sub&gt;2&lt;/sub&gt;. The Knudsen cell study gave uptake coefficients of the order of
      10&lt;sup&gt;-6&lt;/sup&gt; and 10&lt;sup&gt;-7&lt;/sup&gt; for SO&lt;sub&gt;2&lt;/sub&gt; and
      NO&lt;sub&gt;2&lt;/sub&gt; respectively. There was no significant difference in uptake when
      SO&lt;sub&gt;2&lt;/sub&gt; or
      NO&lt;sub&gt;2&lt;/sub&gt; were introduced individually compared to experiments in which
      SO&lt;sub&gt;2&lt;/sub&gt; and
      NO&lt;sub&gt;2&lt;/sub&gt; were
      present at the same time.</p>
</abstract>
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