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<article language="en">
	<journal>
		<journal_title>Atmospheric Chemistry and Physics Discussions</journal_title>
		<journal_url>www.atmos-chem-phys-discuss.net</journal_url>
		<issn>1680-7367</issn>
		<eissn>1680-7375</eissn>
		<volume_number>8</volume_number>
		<issue_number>1</issue_number>
		<publication_year>2008</publication_year>
	</journal>
	<doi>10.5194/acpd-8-1069-2008</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/8/1069/2008/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/8/1069/2008/acpd-8-1069-2008.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/8/1069/2008/acpd-8-1069-2008.pdf</fulltext_pdf>
	<start_page>1069</start_page>
	<end_page>1088</end_page>
	<publication_date>2008-01-23</publication_date>
	<article_title content_type="html">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>
	<authors>
		<author numeration="1" affiliations="1">
			<name>M. S. Javadi</name>
		</author>
		<author numeration="2" affiliations="1">
			<name>R. Søndergaard</name>
		</author>
		<author numeration="3" affiliations="1">
			<name>O. J. Nielsen</name>
		</author>
		<author numeration="4" affiliations="2">
			<name>M. D. Hurley</name>
		</author>
		<author numeration="5" affiliations="2">
			<name>T. J. Wallington</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Department of Chemistry, University of Copenhagen, Universitetsparken 5, 2100 Copenhagen, Denmark</affiliation>
		<affiliation numeration="2" content_type="html">System Analytics and Environmental Sciences Department, Ford Motor Company, Mail Drop RIC-2122, Dearborn, MI 48121-2053, USA</affiliation>
	</affiliations>
	<abstract content_type="html">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&amp;ndash;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.</abstract>
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</article>

