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	<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>7</volume_number>
		<issue_number>4</issue_number>
		<publication_year>2007</publication_year>
	</journal>
	<doi>10.5194/acpd-7-11257-2007</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/7/11257/2007/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/7/11257/2007/acpd-7-11257-2007.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/7/11257/2007/acpd-7-11257-2007.pdf</fulltext_pdf>
	<start_page>11257</start_page>
	<end_page>11294</end_page>
	<publication_date>2007-08-02</publication_date>
	<article_title content_type="html">Predicting diurnal variability of fine inorganic aerosols and their gas-phase precursors near downtown Mexico City</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>M. Moya</name>
			<email>mmoya@servidor.unam.mx</email>
		</author>
		<author numeration="2" affiliations="2">
			<name>C. Fountoukis</name>
		</author>
		<author numeration="3" affiliations="2,3">
			<name>A. Nenes</name>
		</author>
		<author numeration="4" affiliations="4">
			<name>E. Matías</name>
		</author>
		<author numeration="5" affiliations="1">
			<name>M. Grutter</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Centro de Ciencias de la Atmósfera, Universidad Nacional Autónoma de México, Ciudad Universitaria, 04510, Mexico City, Mexico</affiliation>
		<affiliation numeration="2" content_type="html">School of Chemical and Biomolecular Engineering, Georgia Institute of Technology, 311 Ferst Drive, Atlanta, GA 30332-0100, USA</affiliation>
		<affiliation numeration="3" content_type="html">School of Earth and Atmospheric Sciences Georgia Institute of Technology, 311 Ferst Drive, Atlanta, GA 30332-0100, USA</affiliation>
		<affiliation numeration="4" content_type="html">Posgrado en Ciencias Químicas, Universidad Nacional Autónoma de México, Ciudad Universitaria, 04510, Mexico City, Mexico</affiliation>
	</affiliations>
	<abstract content_type="html">Partitioning of semi-volatile nitrate and ammonium between the gas and
particulate phases is studied combining two thermodynamic models that
explicitly include crustal elements and simulate both branches
(deliquescence, efflorescence) of aerosol behavior and measurements taken
near downtown Mexico City during a field campaign conducted in
February&amp;ndash;March, 2005. Overall, no significant differences between model
predictions (within 30% of error) are observed for particulate ammonium
(PM&lt;sub&gt;2.5&lt;/sub&gt;, PM&lt;sub&gt;1&lt;/sub&gt;). In cases of moderate to high RH (40&amp;ndash;70%), mostly
occurring during the 1st and 2nd daily sampling periods
(06:00&amp;ndash;10:00 h, 10:00&amp;ndash;14:00 h, LST), 4 h PM&lt;sub&gt;2.5&lt;/sub&gt; nitrate measurements are
predicted within 30%. When RH drops below 30%, characteristic of the
afternoon sampling periods (14:00-18:00 h), the efflorescence branch is most
consistent with observed PM nitrate. Residual error analysis of these low RH
cases suggest that aerosol nitrate loading or sulfate-to-nitrate molar ratio
control phase behavior, hence the partitioning of semi-volatile PM&lt;sub&gt;2.5&lt;/sub&gt;
nitrate in gas and particulate phases. Finally, inclusion of crustal
elements in the modeling framework reduces the error in predicted PM&lt;sub&gt;2.5&lt;/sub&gt;
ammonium by 25%. These findings, if generally applicable, can help
improve air quality modeling in nitrate deficient environments.</abstract>
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</article>

