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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>8</volume_number>
		<issue_number>3</issue_number>
		<publication_year>2008</publication_year>
	</journal>
	<doi>10.5194/acpd-8-9761-2008</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/8/9761/2008/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/8/9761/2008/acpd-8-9761-2008.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/8/9761/2008/acpd-8-9761-2008.pdf</fulltext_pdf>
	<start_page>9761</start_page>
	<end_page>9782</end_page>
	<publication_date>2008-05-28</publication_date>
	<article_title content_type="html">SO&lt;sub&gt;2&lt;/sub&gt; oxidation products other than H&lt;sub&gt;2&lt;/sub&gt;SO&lt;sub&gt;4&lt;/sub&gt; as a trigger of new particle formation &amp;ndash; Part 1: Laboratory investigations</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>T. Berndt</name>
			<email>berndt@tropos.de</email>
		</author>
		<author numeration="2" affiliations="1">
			<name>F. Stratmann</name>
		</author>
		<author numeration="3" affiliations="1">
			<name>S. Bräsel</name>
		</author>
		<author numeration="4" affiliations="1">
			<name>J. Heintzenberg</name>
		</author>
		<author numeration="5" affiliations="2">
			<name>A. Laaksonen</name>
		</author>
		<author numeration="6" affiliations="3">
			<name>M. Kulmala</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Leibniz-Institut für Troposphärenforschung e.V., Leipzig, Germany</affiliation>
		<affiliation numeration="2" content_type="html">University of Kuopio, Kuopio, Finland</affiliation>
		<affiliation numeration="3" content_type="html">University of Helsinki, Helsinki, Finland</affiliation>
	</affiliations>
	<abstract content_type="html">Mechanistic investigations of atmospheric H&lt;sub&gt;2&lt;/sub&gt;SO&lt;sub&gt;4&lt;/sub&gt; particle formation
have been performed in a laboratory study taking either H&lt;sub&gt;2&lt;/sub&gt;SO&lt;sub&gt;4&lt;/sub&gt; from
a liquid reservoir or using the gas-phase reaction of OH radicals with
SO&lt;sub&gt;2&lt;/sub&gt;. Applying both approaches for H&lt;sub&gt;2&lt;/sub&gt;SO&lt;sub&gt;4&lt;/sub&gt; generation
simultaneously we found that H&lt;sub&gt;2&lt;/sub&gt;SO&lt;sub&gt;4&lt;/sub&gt; evaporated from the liquid
reservoir acts considerably less effective for the process of particle
formation and growth than the products originating from the reaction of OH
radicals with SO&lt;sub&gt;2&lt;/sub&gt;. Furthermore, for NO&lt;sub&gt;x&lt;/sub&gt; concentrations
&amp;gt;5&amp;times;10&lt;sup&gt;11&lt;/sup&gt; molecule cm&lt;sup&gt;&amp;minus;3&lt;/sup&gt; the formation of new particles
from the reaction of OH radicals with SO&lt;sub&gt;2&lt;/sub&gt; is inhibited. This suggests
that substances other than H&lt;sub&gt;2&lt;/sub&gt;SO&lt;sub&gt;4&lt;/sub&gt; (likely products from
sulphur-containing peroxy radicals) trigger lower tropospheric new particle
formation and growth. The currently accepted mechanism for SO&lt;sub&gt;2&lt;/sub&gt;
gas-phase oxidation does not consider the formation of such substances
making a revision necessary.</abstract>
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</article>

