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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>1</issue_number>
		<publication_year>2006</publication_year>
	</journal>
	<doi>10.5194/acpd-6-17-2006</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/6/17/2006/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/6/17/2006/acpd-6-17-2006.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/6/17/2006/acpd-6-17-2006.pdf</fulltext_pdf>
	<start_page>17</start_page>
	<end_page>43</end_page>
	<publication_date>2006-01-02</publication_date>
	<article_title content_type="html">The effect of varying levels of surfactant on the reactive uptake of N&lt;sub&gt;2&lt;/sub&gt;O&lt;sub&gt;5&lt;/sub&gt; to aqueous aerosol</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>V. F. McNeill</name>
		</author>
		<author numeration="2" affiliations="2">
			<name>J. Patterson</name>
		</author>
		<author numeration="3" affiliations="2">
			<name>G. M. Wolfe</name>
		</author>
		<author numeration="4" affiliations="1">
			<name>J. A. Thornton</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Department of Atmospheric Sciences, University of Washington, Seattle, Washington, 98195, USA</affiliation>
		<affiliation numeration="2" content_type="html">Department of Chemistry, University of Washington, Seattle, Washington, 98195, USA</affiliation>
	</affiliations>
	<abstract content_type="html">Recent observations have detected surface active organics in atmospheric
aerosols. We have studied the reaction of N&lt;sub&gt;2&lt;/sub&gt;O&lt;sub&gt;5&lt;/sub&gt; on aqueous natural
seawater and NaCl aerosol as a function of sodium dodecyl sulfate (SDS)
concentration to test the effect of varying levels of surfactant on
gas-aerosol reaction rates. SDS was chosen as a proxy for naturally
occurring long chain monocarboxylic acid molecules, such as palmitic or
stearic acid, because of its solubility in water and well-characterized
surface properties. Experiments were performed using a newly constructed
aerosol flow tube coupled to a chemical ionization mass spectrometer for
monitoring the gas phase, and a differential mobility analyzer/condensation
particle counter for determining aerosol surface area. We find that the
presence of ~3.5 wt% SDS in the aerosol, which corresponds to a
monolayer surface coverage of ~2&amp;times;10&lt;sup&gt;14&lt;/sup&gt; molecules cm&lt;sup&gt;&amp;minus;2&lt;/sup&gt;,
suppresses the N&lt;sub&gt;2&lt;/sub&gt;O&lt;sub&gt;5&lt;/sub&gt; reaction probability, &amp;gamma;&lt;sup&gt;N2O5&lt;/sup&gt;, by
approximately a factor of ten, independent of relative humidity. Consistent
with this observation is a similar reduction in the rate of ClNO&lt;sub&gt;2&lt;/sub&gt;
product generation measured simultaneously. However, the product yield
remains nearly constant under all conditions. The degree of suppression is
strongly dependent on SDS content in the aerosol, with no discernable effect
at 0.1 wt% SDS, but significant suppression at what we predict to be
submonolayer coverages with 0.3&amp;ndash;0.6 wt% SDS on NaCl and natural
seawater aerosols, respectively.</abstract>
	<references>
	</references>
</article>

