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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-8-3141-2008</article-id>
<title-group>
<article-title>Atmospheric chemistry of trans-CF&lt;sub&gt;3&lt;/sub&gt;CH=CHF: products and mechanisms of hydroxyl radical and chlorine atom initiated oxidation</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Javadi</surname>
<given-names>M. S.</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>Søndergaard</surname>
<given-names>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>Nielsen</surname>
<given-names>O. J.</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>Hurley</surname>
<given-names>M. D.</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>Wallington</surname>
<given-names>T. J.</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Department of Chemistry, University of Copenhagen, Universitetsparken 5, 2100 Copenhagen, Denmark</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>System Analytics and Environmental Sciences Department, Ford Motor Company, Mail Drop RIC-2122, Dearborn, Michigan 48121-2053, USA</addr-line>
</aff>
<pub-date pub-type="epub">
<day>24</day>
<month>06</month>
<year>2008</year>
</pub-date>
<volume>8</volume>
<issue>12</issue>
<fpage>3141</fpage>
<lpage>3147</lpage>
<permissions>
<copyright-statement>Copyright: &#x000a9; 2008 M. S. Javadi et al.</copyright-statement>
<copyright-year>2008</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/8/3141/2008/acp-8-3141-2008.html">This article is available from https://acp.copernicus.org/articles/8/3141/2008/acp-8-3141-2008.html</self-uri>
<self-uri xlink:href="https://acp.copernicus.org/articles/8/3141/2008/acp-8-3141-2008.pdf">The full text article is available as a PDF file from https://acp.copernicus.org/articles/8/3141/2008/acp-8-3141-2008.pdf</self-uri>
<abstract>
<p>Smog chamber/FTIR techniques were used to study the products and mechanisms
of OH radical and Cl atom initiated oxidation of trans-CF&lt;sub&gt;3&lt;/sub&gt;CH=CHF in 700 Torr
of N&lt;sub&gt;2&lt;/sub&gt;/O&lt;sub&gt;2&lt;/sub&gt; diluent at 295&amp;plusmn;1 K. Hydroxyl radical initiated
oxidation leads to the formation of CF&lt;sub&gt;3&lt;/sub&gt;CHO and HC(O)F in yields which
were indistinguishable from 100% and were not dependent on the O&lt;sub&gt;2&lt;/sub&gt;
partial pressure. Chlorine atom initiated oxidation gives HC(O)F,
CF&lt;sub&gt;3&lt;/sub&gt;CHO, CF&lt;sub&gt;3&lt;/sub&gt;C(O)Cl, and CF&lt;sub&gt;3&lt;/sub&gt;C(O)CHFCl. The yields of
CF&lt;sub&gt;3&lt;/sub&gt;C(O)Cl and CF&lt;sub&gt;3&lt;/sub&gt;C(O)CHFCl increased at the expense of HC(O)F and
CF&lt;sub&gt;3&lt;/sub&gt;CHO as the O&lt;sub&gt;2&lt;/sub&gt; partial pressure was increased over the range
5–700 Torr. The results are discussed with respect to the atmospheric
chemistry and environmental impact of trans-CF&lt;sub&gt;3&lt;/sub&gt;CH=CHF.</p>
</abstract>
<counts><page-count count="7"/></counts>
</article-meta>
</front>
<body/>
<back>
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</article>