<?xml version="1.0" encoding="utf-8" standalone="no"?>
<!DOCTYPE article SYSTEM "http://www.atmos-chem-phys.net/inc/acp/copernicus.dtd">
<article language="en">
	<journal>
		<journal_title>Atmospheric Chemistry and Physics</journal_title>
		<journal_url>www.atmos-chem-phys.net</journal_url>
		<issn>1680-7316</issn>
		<eissn>1680-7324</eissn>
		<volume_number>4</volume_number>
		<issue_number>8</issue_number>
		<publication_year>2004</publication_year>
	</journal>
	<doi>10.5194/acp-4-2083-2004</doi>
	<article_url>http://www.atmos-chem-phys.net/4/2083/2004/</article_url>
	<abstract_html>http://www.atmos-chem-phys.net/4/2083/2004/acp-4-2083-2004.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys.net/4/2083/2004/acp-4-2083-2004.pdf</fulltext_pdf>
	<start_page>2083</start_page>
	<end_page>2089</end_page>
	<publication_date>2005-10-19</publication_date>
	<article_title content_type="html">Enhanced uptake of water by oxidatively processed oleic acid</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>A. Asad</name>
		</author>
		<author numeration="2" affiliations="1">
			<name>B. T. Mmereki</name>
		</author>
		<author numeration="3" affiliations="1">
			<name>D. J. Donaldson</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Department of Chemistry and Department of Physical and Environmental Sciences, University of Toronto, 80 St. George St., Toronto, Ont. M5S 3H6, Canada</affiliation>
	</affiliations>
	<abstract content_type="html">A quartz crystal microbalance apparatus has been used to measure the room
temperature uptake of water vapour by thin films of oleic acid as a function
of relative humidity, both before and following exposure of the films to
various partial pressures of gas phase ozone. A rapid increase in the
water-sorbing ability of the film is observed as its exposure to ozone is
increased, followed by a plateau region in which additional water is taken
up more gradually. In this fully-processed region the mass of water taken up
by the film is about 4 times that of the unprocessed film. Infrared spectra
of the films, measured after variable exposures to ozone, show dramatic
increases in both the &quot;free&quot; and hydrogen-bonded O-H stretching regions,
and a decrease in the intensity of olefinic features. These results are
consistent with the formation of an oxygenated polymeric product or
products, as well as the gas phase products previously identified.</abstract>
	<references>
	</references>
</article>

