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<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-9-8559-2009</article-id>
<title-group>
<article-title>Hydrogen soil deposition at an urban site in Finland</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Lallo</surname>
<given-names>M.</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>Aalto</surname>
<given-names>T.</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>Hatakka</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>Laurila</surname>
<given-names>T.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Finnish Meteorological Institute, Helsinki, Finland</addr-line>
</aff>
<pub-date pub-type="epub">
<day>11</day>
<month>11</month>
<year>2009</year>
</pub-date>
<volume>9</volume>
<issue>21</issue>
<fpage>8559</fpage>
<lpage>8571</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/9/8559/2009/acp-9-8559-2009.html">This article is available from http://www.atmos-chem-phys.net/9/8559/2009/acp-9-8559-2009.html</self-uri>
<self-uri xlink:href="http://www.atmos-chem-phys.net/9/8559/2009/acp-9-8559-2009.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys.net/9/8559/2009/acp-9-8559-2009.pdf</self-uri>
<abstract>
<p>Hydrogen deposition velocities (&lt;i&gt;v&lt;sub&gt;d&lt;/sub&gt;&lt;/i&gt;) were estimated by field chamber
measurements and model simulations. A closed-chamber method was used for
soil deposition studies in Helsinki, Finland, at an urban park inhabited by
broad-leaved trees. Radon tracer method was used to estimate the &lt;i&gt;v&lt;sub&gt;d&lt;/sub&gt;&lt;/i&gt; in
nighttime when photochemical reactions were minimal and radon gas was
concentrated in the shallow boundary layer due to exhalation from soil. A
two-dimensional atmospheric model was used for the calculation of respective
&lt;i&gt;v&lt;sub&gt;d&lt;/sub&gt;&lt;/i&gt; values and radon exhalation rates. The &lt;i&gt;v&lt;sub&gt;d&lt;/sub&gt;&lt;/i&gt; and radon exhalation
rates were lower in winter than in summer according to all methods. The
radon tracer method and the two-dimensional model results for hydrogen
deposition velocity were in the range of 0.13 mm s&lt;sup&gt;&amp;minus;1&lt;/sup&gt; to 0.93 mm s&lt;sup&gt;&amp;minus;1&lt;/sup&gt;
(radon tracer) and 0.12 mm s&lt;sup&gt;&amp;minus;1&lt;/sup&gt; to 0.61 mm s&lt;sup&gt;&amp;minus;1&lt;/sup&gt; (two-dimensional).
The soil chamber results for &lt;i&gt;v&lt;sub&gt;d&lt;/sub&gt;&lt;/i&gt; were 0.00 mm s&lt;sup&gt;&amp;minus;1&lt;/sup&gt; to 0.70 mm s&lt;sup&gt;&amp;minus;1&lt;/sup&gt;.
Both models and chamber measurements revealed a relation between
one week cumulative rain sum and deposition velocity. When precipitation
events occurred a few days before the chamber measurements, lower &lt;i&gt;v&lt;sub&gt;d&lt;/sub&gt;&lt;/i&gt;
values were observed. A snow cover also lowered &lt;i&gt;v&lt;sub&gt;d&lt;/sub&gt;&lt;/i&gt;.</p>
</abstract>
<counts><page-count count="13"/></counts>
</article-meta>
</front>
<body/>
<back>
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