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<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>3</issue_number>
		<publication_year>2006</publication_year>
	</journal>
	<doi>10.5194/acpd-6-3845-2006</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/6/3845/2006/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/6/3845/2006/acpd-6-3845-2006.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/6/3845/2006/acpd-6-3845-2006.pdf</fulltext_pdf>
	<start_page>3845</start_page>
	<end_page>3882</end_page>
	<publication_date>2006-05-15</publication_date>
	<article_title content_type="html">Atmospheric sulphuric acid and aerosol formation: implications from atmospheric measurements for nucleation and early growth mechanisms</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>S.-L. Sihto</name>
		</author>
		<author numeration="2" affiliations="1">
			<name>M. Kulmala</name>
		</author>
		<author numeration="3" affiliations="2">
			<name>V.-M. Kerminen</name>
		</author>
		<author numeration="4" affiliations="1">
			<name>M. Dal Maso</name>
		</author>
		<author numeration="5" affiliations="1">
			<name>T. Petäjä</name>
		</author>
		<author numeration="6" affiliations="1">
			<name>I. Riipinen</name>
		</author>
		<author numeration="7" affiliations="2">
			<name>H. Korhonen</name>
		</author>
		<author numeration="8" affiliations="3">
			<name>F. Arnold</name>
		</author>
		<author numeration="9" affiliations="4">
			<name>R. Janson</name>
		</author>
		<author numeration="10" affiliations="1">
			<name>M. Boy</name>
		</author>
		<author numeration="11" affiliations="5">
			<name>A. Laaksonen</name>
		</author>
		<author numeration="12" affiliations="6">
			<name>K. E. J. Lehtinen</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">University of Helsinki, Department of Physical Sciences, P.O. Box 64, 00014 University of Helsinki, Finland</affiliation>
		<affiliation numeration="2" content_type="html">Finnish Meteorological Institute, Climate and Global Change, Erik Palmenin Aukio 1, P.O. Box 503, 00101 Helsinki, Finland</affiliation>
		<affiliation numeration="3" content_type="html">Atmospheric Physics Division, Max-Planck Institute for Nuclear Physics (MPIK), P.O. Box 103980, 69029 Heidelberg, Germany</affiliation>
		<affiliation numeration="4" content_type="html">University of Stockholm, Department of Applied Environmental Science, Air Pollution Laboratory, Frescativ&amp;auml;gen 54, 10691 Stockholm, Sweden</affiliation>
		<affiliation numeration="5" content_type="html">University of Kuopio, Department of Applied Physics, P.O. Box 1627, 70211 Kuopio, Finland</affiliation>
		<affiliation numeration="6" content_type="html">Finnish Meteorological Institute and University of Kuopio, Department of Applied Physics, P.O. Box 1627, 70211 Kuopio, Finland</affiliation>
	</affiliations>
	<abstract content_type="html">We have investigated the formation and early growth of atmospheric secondary
aerosol particles building on atmospheric measurements. The measurements
were part of the QUEST 2 campaign which took place in spring 2003 in
Hyyti&amp;#228;l&amp;#228; (Finland). During the campaign numerous new aerosol
particle formation events occurred of which 15 were accompanied by gaseous
sulphuric acid measurements. Our detailed analysis of these 15 events is
focussed on nucleation and early growth (to a diameter of 3 nm) of fresh
particles. It revealed that new particle formation seems to be a function of
the gaseous sulphuric acid concentration to the power from one to two. The
former would be consistent with the recently developed activation theory
while the latter would be consistent with the kinetic nucleation theory. We
find that some events are dominated by the activation mechanism and some are
dominated by the kinetic mechanism. Inferred coefficients for the two
nucleation mechanisms are correlated with the product of gaseous sulphuric
acid and ammonia concentrations. This indicates that besides gaseous
sulphuric acid also ammonia has a role in nucleation. Early growth of fresh
particles to a diameter of 3 nm has a mean rate of 1.2 nm/h and is clearly
correlated with the gaseous sulphuric acid concentration.</abstract>
	<references>
	</references>
</article>

