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	<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>9</volume_number>
		<issue_number>6</issue_number>
		<publication_year>2009</publication_year>
	</journal>
	<doi>10.5194/acpd-9-24783-2009</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/9/24783/2009/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/9/24783/2009/acpd-9-24783-2009.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/9/24783/2009/acpd-9-24783-2009.pdf</fulltext_pdf>
	<start_page>24783</start_page>
	<end_page>24814</end_page>
	<publication_date>2009-11-19</publication_date>
	<article_title content_type="html">Tropospheric photooxidation of CF&lt;sub&gt;3&lt;/sub&gt;CH&lt;sub&gt;2&lt;/sub&gt;CHO and CF&lt;sub&gt;3&lt;/sub&gt;(CH&lt;sub&gt;2&lt;/sub&gt;)&lt;sub&gt;2&lt;/sub&gt;CHO  initiated by Cl atoms and OH radicals</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>M. Antiñolo</name>
		</author>
		<author numeration="2" affiliations="1">
			<name>E. Jiménez</name>
		</author>
		<author numeration="3" affiliations="2">
			<name>A. Notario</name>
		</author>
		<author numeration="4" affiliations="1">
			<name>E. Martínez</name>
		</author>
		<author numeration="5" affiliations="1">
			<name>J. Albaladejo</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Departamento de Química Física, Facultad de Ciencias  Químicas. Universidad de Castilla-La Mancha. Avda. Camilo José  Cela, s/n. 13071 Ciudad Real, Spain</affiliation>
		<affiliation numeration="2" content_type="html">Instituto de Tecnologías Química y Medioambiental  (ITQUIMA). Universidad de Castilla-La Mancha, Avda. Camilo José Cela, s/n. 13071 Ciudad Real, Spain</affiliation>
	</affiliations>
	<abstract content_type="html">The absolute rate coefficients for the tropospheric reactions of chlorine (Cl) atoms
      and hydroxyl (OH) radicals with CF&lt;sub&gt;3&lt;/sub&gt;CH&lt;sub&gt;2&lt;/sub&gt;CHO and
      CF&lt;sub&gt;3&lt;/sub&gt;(CH&lt;sub&gt;2&lt;/sub&gt;)&lt;sub&gt;2&lt;/sub&gt;CHO were measured as a function of temperature (263–371 K)
      and pressure (50–215 Torr of He) by pulsed UV laser photolysis techniques. Vacuum
      UV resonance fluorescence was employed to detect and monitor the time evolution of Cl
      atoms. Laser induced fluorescence was used in this work as a detection of OH radicals
      as a function of reaction time. No pressure dependence of the bimolecular rate coefficients,
      &lt;i&gt;k&lt;/i&gt;&lt;sub&gt;Cl&lt;/sub&gt; and &lt;i&gt;k&lt;/i&gt;&lt;sub&gt;OH&lt;/sub&gt;, was found at all temperatures. At room temperature
      &lt;i&gt;k&lt;/i&gt;&lt;sub&gt;Cl&lt;/sub&gt; and &lt;i&gt;k&lt;/i&gt;&lt;sub&gt;OH&lt;/sub&gt; were (in
      10&lt;sup&gt;&amp;minus;11&lt;/sup&gt; cm&lt;sup&gt;3&lt;/sup&gt; molecule&lt;sup&gt;&amp;minus;1&lt;/sup&gt; s&lt;sup&gt;&amp;minus;1&lt;/sup&gt;):
      &lt;i&gt;k&lt;/i&gt;&lt;sub&gt;Cl&lt;/sub&gt;(CF&lt;sub&gt;3&lt;/sub&gt;CH&lt;sub&gt;2&lt;/sub&gt;CHO) = (1.55&amp;plusmn;0.53); &lt;i&gt;k&lt;/i&gt;&lt;sub&gt;Cl&lt;/sub&gt;(CF&lt;sub&gt;3&lt;/sub&gt;(CH&lt;sub&gt;2&lt;/sub&gt;)&lt;sub&gt;2&lt;/sub&gt;CHO) = (3.39&amp;plusmn;1.38);
      &lt;i&gt;k&lt;/i&gt;&lt;sub&gt;OH&lt;/sub&gt;(CF&lt;sub&gt;3&lt;/sub&gt;CH&lt;sub&gt;2&lt;/sub&gt;CHO) = (0.259&amp;plusmn;0.050);
      &lt;i&gt;k&lt;/i&gt;&lt;sub&gt;OH&lt;/sub&gt;(CF&lt;sub&gt;3&lt;/sub&gt;(CH&lt;sub&gt;2&lt;/sub&gt;)&lt;sub&gt;2&lt;/sub&gt;CHO) = (1.28&amp;plusmn;0.24). A slightly negative
      temperature dependence of &lt;i&gt;k&lt;/i&gt;&lt;sub&gt;Cl&lt;/sub&gt; was observed for CF&lt;sub&gt;3&lt;/sub&gt;CH&lt;sub&gt;2&lt;/sub&gt;CHO and
      CF&lt;sub&gt;3&lt;/sub&gt;(CH&lt;sub&gt;2&lt;/sub&gt;)&lt;sub&gt;2&lt;/sub&gt;CHO, and &lt;i&gt;k&lt;/i&gt;&lt;sub&gt;OH&lt;/sub&gt;(CF&lt;sub&gt;3&lt;/sub&gt;CH&lt;sub&gt;2&lt;/sub&gt;CHO). In contrast,
      &lt;i&gt;k&lt;/i&gt;&lt;sub&gt;OH&lt;/sub&gt;(CF&lt;sub&gt;3&lt;/sub&gt;(CH&lt;sub&gt;2&lt;/sub&gt;)&lt;sub&gt;2&lt;/sub&gt;CHO) did not exhibit a temperature dependence in
      the studied ranged. Arrhenius expressions for these reactions were:
&lt;br&gt;&lt;br&gt;
&lt;i&gt;k&lt;/i&gt;&lt;sub&gt;Cl&lt;/sub&gt;(CF&lt;sub&gt;3&lt;/sub&gt;CH&lt;sub&gt;2&lt;/sub&gt;CHO) =(4.4&amp;plusmn;1.0) &amp;times; 10&lt;sup&gt;&amp;minus;11&lt;/sup&gt; exp{&amp;minus;(316&amp;plusmn;68)/T} cm&lt;sup&gt;3&lt;/sup&gt; molecule&lt;sup&gt;&amp;minus;1&lt;/sup&gt; s&lt;sup&gt;&amp;minus;1&lt;/sup&gt;,
&lt;br&gt;&lt;br&gt;
&lt;i&gt;k&lt;/i&gt;&lt;sub&gt;Cl&lt;/sub&gt;(CF&lt;sub&gt;3&lt;/sub&gt;(CH&lt;sub&gt;2&lt;/sub&gt;)&lt;sub&gt;2&lt;/sub&gt;CHO) = (2.9&amp;plusmn;0.7) &amp;times; 10&lt;sup&gt;&amp;minus;10&lt;/sup&gt; exp{&amp;minus;625&amp;plusmn;80)/T} cm&lt;sup&gt;3&lt;/sup&gt; molecule&lt;sup&gt;&amp;minus;1&lt;/sup&gt; s&lt;sup&gt;&amp;minus;1&lt;/sup&gt;,
&lt;br&gt;&lt;br&gt;
&lt;i&gt;k&lt;/i&gt;&lt;sub&gt;OH&lt;/sub&gt;(CF&lt;sub&gt;3&lt;/sub&gt;CH&lt;sub&gt;2&lt;/sub&gt;CHO) = (7.8&amp;plusmn;2.2) &amp;times; 10&lt;sup&gt;&amp;minus;12&lt;/sup&gt; exp{&amp;minus;(314&amp;plusmn;90)/T} cm&lt;sup&gt;3&lt;/sup&gt; molecule&lt;sup&gt;&amp;minus;1&lt;/sup&gt; s&lt;sup&gt;&amp;minus;1&lt;/sup&gt;.
&lt;br&gt;&lt;br&gt;
      The atmospheric impact of the homogeneous removal by OH radicals and Cl atoms
      of these fluorinated aldehydes is discussed in terms of the global atmospheric lifetimes,
      taking into account different degradation pathways. The calculated lifetimes show that
      atmospheric oxidation of CF&lt;sub&gt;3&lt;/sub&gt;(CH&lt;sub&gt;2&lt;/sub&gt;)&lt;sub&gt;x&lt;/sub&gt;CHO are globally dominated by OH
      radicals, however reactions initiated by Cl atoms can act as a source of free
      radicals at dawn in the troposphere.</abstract>
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</article>

