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<!DOCTYPE article SYSTEM "http://www.atmos-chem-phys-discuss.net/inc/acpd/copernicus.dtd">
<article language="en">
	<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>6</volume_number>
		<issue_number>2</issue_number>
		<publication_year>2006</publication_year>
	</journal>
	<doi>10.5194/acpd-6-3135-2006</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/6/3135/2006/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/6/3135/2006/acpd-6-3135-2006.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/6/3135/2006/acpd-6-3135-2006.pdf</fulltext_pdf>
	<start_page>3135</start_page>
	<end_page>3174</end_page>
	<publication_date>2006-04-18</publication_date>
	<article_title content_type="html">Factors of air ion balance in a coniferous forest according to measurements in Hyyti&amp;#228;l&amp;#228;, Finland</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>H. Tammet</name>
		</author>
		<author numeration="2" affiliations="1,2">
			<name>U. Hõrrak</name>
		</author>
		<author numeration="3" affiliations="2">
			<name>L. Laakso</name>
		</author>
		<author numeration="4" affiliations="2">
			<name>M. Kulmala</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Institute of Environmental Physics, University of Tartu, &amp;Uuml;likooli 18, 50090, Tartu, Estonia</affiliation>
		<affiliation numeration="2" content_type="html">Department of Physical Sciences, University of Helsinki, P.O. Box 64, 00014, Finland</affiliation>
	</affiliations>
	<abstract content_type="html">A new theoretical model includes dry deposition of ions onto the forest
canopy and takes into account different parameters of positive and negative
ions. Explicit algebraic solution of the air ion balance equations allows
calculating the ionization rate and the average charge of aerosol particles
according to air ion and aerosol measurements, and parameters of forest. The
transformation of direct measurements to the values of the ionization rate
does not bring along amplification of measurement errors. The model was used
to estimate the ionization rate at the Hyyti&amp;#228;l&amp;#228; forest station,
Finland, and it solved the controversy of different estimates in the earlier
study. The ionization rate during one-day measurements proved to be
5.6&amp;plusmn;0.8 cm&lt;sup&gt;&amp;minus;3&lt;/sup&gt; s&lt;sup&gt;&amp;minus;1&lt;/sup&gt; at the standard measuring height of 2 m and
3.9&amp;plusmn;0.2 cm&lt;sup&gt;&amp;minus;3&lt;/sup&gt; s&lt;sup&gt;&amp;minus;1&lt;/sup&gt; at the height of 14 m between the tops of the trees.
The height variation should be considered when the ionization rate is used
as a parameter in models of ion-induced nucleation. The recombination sink
of cluster ions on the ions of opposite polarity made up 9&amp;ndash;13%, the
sink on aerosol particles 65&amp;ndash;69%, and the sink on forest canopy
18&amp;ndash;26% of the total sink of cluster ions. The average lifetime of
cluster ions was about 130 s for positive ions and about 110 s for negative
ions. About 70% of the space charge of the air was carried by aerosol
particles at the height of 2 m and about 84% at the height of 14 m.</abstract>
	<references>
	</references>
</article>

