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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>9</volume_number>
		<issue_number>4</issue_number>
		<publication_year>2009</publication_year>
	</journal>
	<doi>10.5194/acpd-9-15181-2009</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/9/15181/2009/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/9/15181/2009/acpd-9-15181-2009.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/9/15181/2009/acpd-9-15181-2009.pdf</fulltext_pdf>
	<start_page>15181</start_page>
	<end_page>15214</end_page>
	<publication_date>2009-07-14</publication_date>
	<article_title content_type="html">Toward a general parameterization of N&lt;sub&gt;2&lt;/sub&gt;O&lt;sub&gt;5&lt;/sub&gt;  reactivity on aqueous particles: the competing effects of particle liquid water, nitrate and chloride</article_title>
	<authors>
		<author numeration="1" affiliations="1,2">
			<name>T. H. Bertram</name>
		</author>
		<author numeration="2" affiliations="1">
			<name>J. A. Thornton</name>
			<email>thornton@atmos.washington.edu</email>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Department of Atmospheric Sciences, University of Washington, Seattle, WA, USA</affiliation>
		<affiliation numeration="2" content_type="html">now at: Department of Chemistry; University of California San Diego, La Jolla, CA, USA</affiliation>
	</affiliations>
	<abstract content_type="html">The heterogeneous reaction of N&lt;sub&gt;2&lt;/sub&gt;O&lt;sub&gt;5&lt;/sub&gt; on mixed organic-inorganic aerosol particles
      was investigated using an entrained aerosol flow tube coupled to a custom-built chemical
      ionization mass spectrometer. Laboratory results on aqueous particles confirm a strong
      dependence of the reactive uptake coefficient (γ) on particle liquid water, for
      particle water concentrations below 15 M, and the molar ratio of particle water to
      nitrate. Measurements of &amp;gamma;(N&lt;sub&gt;2&lt;/sub&gt;O&lt;sub&gt;5&lt;/sub&gt;) on mixed chloride-nitrate particles
      indicate that the presence of trace chloride can negate the suppression of
      &amp;gamma;(N&lt;sub&gt;2&lt;/sub&gt;O&lt;sub&gt;5&lt;/sub&gt;) at high nitrate loadings with implications for polluted coastal
      regions. These results are used to construct a new parameterization for &amp;gamma;(N&lt;sub&gt;2&lt;/sub&gt;O&lt;sub&gt;5&lt;/sub&gt;), that when coupled to an aerosol thermodynamics model, can be used
      within regional and/or global chemical transport models.</abstract>
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</article>

