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<article xmlns:mml="http://www.w3.org/1998/Math/MathML" xmlns:xlink="http://www.w3.org/1999/xlink" article-type="research-article" dtd-version="3.0" xml:lang="en">
<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-10-1545-2010</article-id>
<title-group>
<article-title>Heterogeneous ozonation kinetics of 4-phenoxyphenol in the presence of photosensitizer</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Net</surname>
<given-names>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>Nieto-Gligorovski</surname>
<given-names>L.</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>Gligorovski</surname>
<given-names>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>Wortham</surname>
<given-names>H.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Universités d&apos;Aix-Marseille I, II, III – CNRS UMR 6264: Laboratoire Chimie Provence Equipe Instrumentation et Réactivité Atmosphérique Case courrier 29, 3 place Victor Hugo, 13331 Marseille Cedex 03, France</addr-line>
</aff>
<pub-date pub-type="epub">
<day>15</day>
<month>02</month>
<year>2010</year>
</pub-date>
<volume>10</volume>
<issue>4</issue>
<fpage>1545</fpage>
<lpage>1554</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/10/1545/2010/acp-10-1545-2010.html">This article is available from http://www.atmos-chem-phys.net/10/1545/2010/acp-10-1545-2010.html</self-uri>
<self-uri xlink:href="http://www.atmos-chem-phys.net/10/1545/2010/acp-10-1545-2010.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys.net/10/1545/2010/acp-10-1545-2010.pdf</self-uri>
<abstract>
<p>In this work we have quantitatively measured the degradation of
4-phenoxyphenol adsorbed on silica particles following oxidative
processing by gas-phase ozone. This was performed under dark
conditions and in the presence of 4-carboxybenzophenone under
simulated sunlight irradiation of the particles surface.
&lt;br&gt;&lt;br&gt;
At the mixing ratio of 60 ppb which corresponds to strongly polluted
ozone areas, the first order of decay of 4-phenoxyphenol is
&lt;i&gt;k&lt;/i&gt;&lt;sub&gt;1&lt;/sub&gt;=9.95&amp;times;10&lt;sup&gt;&amp;minus;6&lt;/sup&gt; s&lt;sup&gt;&amp;minus;1&lt;/sup&gt;. At a very high ozone
mixing ratio of 6 ppm the first order rate constants for
4-phenoxyphenol degradation were the following:
&lt;i&gt;k&lt;/i&gt;&lt;sub&gt;1&lt;/sub&gt;=2.86&amp;times;10&lt;sup&gt;&amp;minus;5&lt;/sup&gt; s&lt;sup&gt;&amp;minus;1&lt;/sup&gt; under dark conditions
and &lt;i&gt;k&lt;/i&gt;&lt;sub&gt;1&lt;/sub&gt;=5.58&amp;times;10&lt;sup&gt;&amp;minus;5&lt;/sup&gt; s&lt;sup&gt;&amp;minus;1&lt;/sup&gt; in the presence of
photosensitizer (4-carboxybenzophenone) under light illumination of
the particles surface. In both cases, the experimental data follow
the modified Langmuir-Hinshelwood equation for surface reactions.
The Langmuir-Hinshelwood and Langmuir-Rideal mechanisms for
bimolecular surface reactions are also discussed along with the
experimental results.
&lt;br&gt;&lt;br&gt;
Most importantly, the quantities of the oligomers such as
2-(4-Phenoxyphenoxy)-4-phenoxyphenol and
4-[4-(4-Phenoxyphenoxy)phenoxy]phenol formed during the heterogeneous
ozonolysis of adsorbed 4-phenoxyphenol were much higher under solar light
irradiation of the surface in comparison to the dark conditions.</p>
</abstract>
<counts><page-count count="10"/></counts>
</article-meta>
</front>
<body/>
<back>
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