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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>5</volume_number>
		<issue_number>2</issue_number>
		<publication_year>2005</publication_year>
	</journal>
	<doi>10.5194/acpd-5-1115-2005</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/5/1115/2005/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/5/1115/2005/acpd-5-1115-2005.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/5/1115/2005/acpd-5-1115-2005.pdf</fulltext_pdf>
	<start_page>1115</start_page>
	<end_page>1164</end_page>
	<publication_date>2005-03-01</publication_date>
	<article_title content_type="html">Evaluation of the pathways of tropospheric nitrophenol formation using a multiphase model</article_title>
	<authors>
		<author numeration="1" affiliations="1,3">
			<name>M. A. J. Harrison</name>
		</author>
		<author numeration="2" affiliations="1">
			<name>M. R. Heal</name>
		</author>
		<author numeration="3" affiliations="2">
			<name>J. N. Cape</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">School of Chemistry, University of Edinburgh, West Mains Road, Edinburgh EH9 3JJ, UK</affiliation>
		<affiliation numeration="2" content_type="html">Edinburgh Research Station, Centre for Ecology and Hydrology, Bush Estate, Penicuik, Midlothian, EH26 0QB, UK</affiliation>
		<affiliation numeration="3" content_type="html">current address: Hadley Centre, Met Office, FitzRoy Road, Exeter, EX1 3PB, UK</affiliation>
	</affiliations>
	<abstract content_type="html">Phenols are a major class of volatile organic compounds (VOC) whose reaction
within, and partitioning between, the gas and liquid phases affects their
lifetime within the atmosphere, the local oxidising capacity, and the extent
of production of nitrophenols, which are toxic chemicals. In this work, a
zero-dimension box model was constructed to quantify the relative nitration
pathways, and partitioning into the liquid phase, of mono-aromatic compounds
in order to help elucidate the formation pathways of 2- and 4-nitrophenol in
the troposphere. The liquid phase contributed significantly to the
production of nitrophenols for liquid water content (&lt;i&gt;L&lt;sub&gt;c&lt;/sub&gt;&lt;/i&gt;) values
exceeding 3&amp;times;10&lt;sup&gt;-9&lt;/sup&gt;, and for a range of assumed liquid droplet diameter,
even though the resultant equilibrium partitioning to the liquid phase was
much lower. For example, in a &apos;&apos;typical&apos;&apos; model scenario, with &lt;i&gt;L&lt;sub&gt;c&lt;/sub&gt;&lt;/i&gt;=3&amp;times;10&lt;sup&gt;-7&lt;/sup&gt;,
58% of nitrophenol production occurred in the liquid phase
but only 2% of nitrophenol remained there, i.e. a significant proportion
of nitrophenol observed in the gas phase may actually be produced via the
liquid phase. The importance of the liquid phase was enhanced at lower
temperatures, by a factor ~1.5&amp;ndash;2 at 278 K cf. 298 K. The model showed
that nitrophenol production was particularly sensitive to the values of the
rate coefficients for the liquid phase reactions between phenol and OH or
NO&lt;sub&gt;3&lt;/sub&gt; reactions, but insensitive to the rate coefficient for the reaction
between benzene and OH, thus identifying where further experimental data are
required.</abstract>
	<references>
	</references>
</article>

