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<front>
<journal-meta>
<journal-id journal-id-type="publisher">ACPD</journal-id>
<journal-title-group>
<journal-title>Atmospheric Chemistry and Physics Discussions</journal-title>
<abbrev-journal-title abbrev-type="publisher">ACPD</abbrev-journal-title>
</journal-title-group>
<issn pub-type="epub">1680-7375</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/acpd-3-1477-2003</article-id>
<title-group>
<article-title>GC&amp;times&amp;GC measurements of C&lt;sub&gt;7&lt;/sub&gt;&amp;ndash;C&lt;sub&gt;11&lt;/sub&gt; aromatic and n-alkane hydrocarbons on Crete, in air from Eastern Europe during the MINOS campaign</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Xu</surname>
<given-names>X.</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>Williams</surname>
<given-names>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>Plass-Dülmer</surname>
<given-names>C.</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>Berresheim</surname>
<given-names>H.</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>Salisbury</surname>
<given-names>G.</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>Lange</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>Lelieveld</surname>
<given-names>J.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Max Planck Institute for Chemistry, Mainz, Germany</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>German Weather Service, Meteorological Observatory Hohenpeissenberg, Germany</addr-line>
</aff>
<pub-date pub-type="epub">
<day>17</day>
<month>03</month>
<year>2003</year>
</pub-date>
<volume>3</volume>
<issue>2</issue>
<fpage>1477</fpage>
<lpage>1513</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>
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<self-uri xlink:href="http://www.atmos-chem-phys-discuss.net/3/1477/2003/acpd-3-1477-2003.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys-discuss.net/3/1477/2003/acpd-3-1477-2003.pdf</self-uri>
<abstract>
<p>During the Mediterranean Intensive Oxidant Study (MINOS) campaign
      in August 2001 gas-phase organic compounds were measured using comprehensive two-dimensional gas chromatography
      (GC&amp;times;GC) at the Finokalia ground station, Crete. In this paper, C&lt;sub&gt;7&lt;/sub&gt;&amp;ndash;C&lt;sub&gt;11&lt;/sub&gt; aromatic and n-alkane measurements are
      presented and interpreted. The mean mixing ratios of the hydrocarbons varied from
      1+/&amp;minus;1 pptv (i-propylbenzene) to 43+/&amp;minus;36 pptv (toluene). The observed mixing ratios showed strong
      day-to-day variations and generally higher levels during the first half of the campaign. Mean diel profiles showed maxima at local
      midnight and late morning, and minima in the early morning and evening. Results from analysis using a simplified box model
      suggest that both the chemical sink (i.e. reaction with OH) and the variability of source strengths were the causes of the
      observed variations in hydrocarbon mixing ratios. The logarithms of hydrocarbon concentrations were negatively correlated with the
      OH concentrations integral over a day prior to the hydrocarbon measurements. Slopes of the regression lines derived from these
      correlations for different compounds are compared with literature rate constants for their reactions with OH. The slopes for most
      compounds agree reasonably well with the literature rate constants. A sequential reaction model has been applied to the
      interpretation of the relationship between ethylbenzene and two of its potential products, i.e. acetophenone and benzeneacetaldehyde.
      The model can explain the good correlation observed between [acetophenone]/[ethylbenzene] and
      [benzeneacetaldehyde]/[ethylbenzene]. The model results and field measurements suggest that the reactivity of
      benzeneacetaldehyde may lie between those of acetophenone and ethylbenzene and that the ratio between yields of acetophenone and
      benzeneacetaldehyde may be up to 28:1. Photochemical ages of trace gases sampled at Finokalia during the campaign are estimated using
      the sequential reaction model and related data. They lie in the range of about 0.5&amp;ndash;2.5 days.</p>
</abstract>
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