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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-4-1771-2004</article-id>
<title-group>
<article-title>Carbonyl compounds in boreal coniferous forest air in Hyytiälä, Southern Finland</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Hellén</surname>
<given-names>H.</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>Hakola</surname>
<given-names>H.</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>Reissell</surname>
<given-names>A.</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
<xref ref-type="aff" rid="aff3">
<sup>3</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Ruuskanen</surname>
<given-names>T. M.</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Finnish Meteorological Institute, Sahaajankatu 20 E, 00880 Helsinki, Finland</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>University of Helsinki, Department of Physical Sciences, Finland</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>University of Helsinki, Department of Chemistry, Finland</addr-line>
</aff>
<pub-date pub-type="epub">
<day>08</day>
<month>09</month>
<year>2004</year>
</pub-date>
<volume>4</volume>
<issue>7</issue>
<fpage>1771</fpage>
<lpage>1780</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/4/1771/2004/acp-4-1771-2004.html">This article is available from http://www.atmos-chem-phys.net/4/1771/2004/acp-4-1771-2004.html</self-uri>
<self-uri xlink:href="http://www.atmos-chem-phys.net/4/1771/2004/acp-4-1771-2004.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys.net/4/1771/2004/acp-4-1771-2004.pdf</self-uri>
<abstract>
<p>A variety of C&lt;sub&gt;1&lt;/sub&gt;-C&lt;sub&gt;12&lt;/sub&gt; carbonyl compounds were measured in the air of
a boreal coniferous forest located in Hyyti&amp;#228;l&amp;#228;, Southern Finland.
24-hour samples were collected during March and April in 2003 using DNPH
(2,4-dinitrophenyl hydrazine) coated C&lt;sub&gt;18&lt;/sub&gt;-cartridges and analyzed by
liquid chromatography-mass spectrometry (LC-MS).

&lt;P  style=&quot;line-height: 20px;&quot;&gt;
Altogether 22 carbonyl compounds were quantified. The most abundant
carbonyls were acetone (24-hour average 1340ng/m&lt;sup&gt;3&lt;/sup&gt;), formaldehyde
(480ng/m&lt;sup&gt;3&lt;/sup&gt;) and acetaldehyde (360ng/m&lt;sup&gt;3&lt;/sup&gt;). Concentrations of monoterpene
reaction products nopinone (9ng/m&lt;sup&gt;3&lt;/sup&gt;) and limona ketone (5ng/m&lt;sup&gt;3&lt;/sup&gt;)
were low compared to the most abundant low molecular weight carbonyls.
Trajectory analysis showed that highest concentrations of carbonyls were
measured in the air masses coming from the East and the lowest in the air
masses cycled long time over Scandinavia. The total concentration of
carbonyl compounds in Hyyti&amp;#228;l&amp;#228; in March/April 2003 was much higher
than the concentration of aromatic hydrocarbons and monoterpenes in April
2002.

&lt;P  style=&quot;line-height: 20px;&quot;&gt;
Scaling the concentrations against reactivity with the OH-radical showed,
that in spite of relatively low ambient concentrations higher molecular
weight aldehydes contribute significantly to the total OH-reactive mass of
carbonyls. The impact of carbonyl compounds on OH-radical chemistry is
important. Contribution of carbonyls as an OH sink is comparable to that of
NO&lt;sub&gt;2&lt;/sub&gt; and higher than monoterpenes and aromatic hydrocarbons.

&lt;P  style=&quot;line-height: 20px;&quot;&gt;
Lifetimes of the measured carbonyls with respect to reactions with OH
radicals, ozone (O&lt;sub&gt;3&lt;/sub&gt;), and nitrate (NO&lt;sub&gt;3&lt;/sub&gt;) radicals as well as
photolysis were estimated. The main sink reactions for most of the carbonyl
compounds in Hyyti&amp;#228;l&amp;#228; in springtime are expected to be reactions
with the OH radical and photolysis. For 6-methyl-5-hepten-2-one and limona
ketone also reactions with ozone are important. The sources of carbonyl
compounds are presently highly uncertain. Based on the comparisons with
urban concentrations the direct anthropogenic emissions are not as important
as secondary biogenic and anthropogenic sources or primary biogenic sources
in Hyyti&amp;#228;l&amp;#228;.</p>
</abstract>
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