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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>6</issue_number>
		<publication_year>2008</publication_year>
	</journal>
	<doi>10.5194/acpd-8-20311-2008</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/8/20311/2008/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/8/20311/2008/acpd-8-20311-2008.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/8/20311/2008/acpd-8-20311-2008.pdf</fulltext_pdf>
	<start_page>20311</start_page>
	<end_page>20348</end_page>
	<publication_date>2008-12-04</publication_date>
	<article_title content_type="html">Sensitivities of the absorptive partitioning model of secondary organic aerosol formation to the inclusion of water</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>M. Barley</name>
		</author>
		<author numeration="2" affiliations="2">
			<name>D. O. Topping</name>
		</author>
		<author numeration="3" affiliations="1">
			<name>G. McFiggans</name>
			<email>g.mcfiggans@manchester.ac.uk</email>
		</author>
		<author numeration="4" affiliations="3">
			<name>M. E. Jenkin</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Centre for Atmospheric Sciences, School of Earth, Atmospheric and Environmental Sciences, University of Manchester, Manchester, M13 9PL, UK</affiliation>
		<affiliation numeration="2" content_type="html">National Centre for Atmospheric Sciences, Univ. of Manchester, Manchester, M13 9PL, UK</affiliation>
		<affiliation numeration="3" content_type="html">Atmospheric Chemistry Services, Yelverton, Devon, PL20 6EN, UK</affiliation>
	</affiliations>
	<abstract content_type="html">Depending on the assumptions about the participation of water in absorptive
partitioning, the prediction of the distribution of semi-volatile organic
component between the gaseous and condensed phases is shown to be highly
sensitive to the ambient relative humidity and the formulation of the
partitioning model used. Further sensitivities to the assumed pre-existing
particulate loading and to parameterised organic component non-ideality are
explored and shown to contribute significantly to the variation in predicted
secondary organic particulate loading.</abstract>
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</article>

