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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>2</issue_number>
		<publication_year>2008</publication_year>
	</journal>
	<doi>10.5194/acpd-8-4811-2008</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/8/4811/2008/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/8/4811/2008/acpd-8-4811-2008.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/8/4811/2008/acpd-8-4811-2008.pdf</fulltext_pdf>
	<start_page>4811</start_page>
	<end_page>4829</end_page>
	<publication_date>2008-03-05</publication_date>
	<article_title content_type="html">On the volatility and production mechanisms of newly formed nitrate and water soluble organic aerosol in Mexico City</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>C. J. Hennigan</name>
			<email>chennigan@eas.gatech.edu</email>
		</author>
		<author numeration="2" affiliations="2,5">
			<name>A. P. Sullivan</name>
		</author>
		<author numeration="3" affiliations="3">
			<name>C. I. Fountoukis</name>
		</author>
		<author numeration="4" affiliations="2,3">
			<name>A. Nenes</name>
		</author>
		<author numeration="5" affiliations="2">
			<name>A. Hecobian</name>
		</author>
		<author numeration="6" affiliations="2">
			<name>O. Vargas</name>
		</author>
		<author numeration="7" affiliations="2">
			<name>A. T. Case Hanks</name>
		</author>
		<author numeration="8" affiliations="2">
			<name>L. G. Huey</name>
		</author>
		<author numeration="9" affiliations="4">
			<name>B. L. Lefer</name>
		</author>
		<author numeration="10" affiliations="1">
			<name>A. G. Russell</name>
		</author>
		<author numeration="11" affiliations="2">
			<name>R. J. Weber</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">School of Civil and Environmental Engineering, Georgia Institute of Technology, Atlanta, GA, 30332-0340, USA</affiliation>
		<affiliation numeration="2" content_type="html">School of Earth and Atmospheric Sciences, Georgia Institute of Technology, Atlanta, GA, 30332-0340, USA</affiliation>
		<affiliation numeration="3" content_type="html">School of Chemical and Biomolecular Engineering, Georgia Institute of Technology, Atlanta, GA, 30332-0340, USA</affiliation>
		<affiliation numeration="4" content_type="html">Geosciences Department, University of Houston, Houston, TX, 77204-5007, USA</affiliation>
		<affiliation numeration="5" content_type="html">now at: Colorado State University, Ft. Collins, CO, USA</affiliation>
	</affiliations>
	<abstract content_type="html">Measurements of atmospheric gases and fine particle chemistry were made in
the Mexico City Metropolitan Area (MCMA) at a site ~30 km down wind
of the city center. Ammonium nitrate (NH&lt;sub&gt;4&lt;/sub&gt;NO&lt;sub&gt;3&lt;/sub&gt;) dominated the
inorganic aerosol fraction and showed a distinct diurnal signature
characterized by rapid morning production and a rapid mid-day concentration
decrease. The concentration increase was due to both secondary formation and
entrainment from the free troposphere. A majority (approximately two-thirds)
of the midday concentration decrease was caused by dilution from boundary
layer expansion, however a significant fraction (approximately one-third) of
the nitrate loss was due to particle evaporation. The water-soluble organic
carbon fraction of fine particles (WSOC) and nitrate were highly correlated
(&lt;I&gt;R&lt;/I&gt;&lt;sup&gt;2&lt;/sup&gt;=0.80) for the entire three-day analysis period, however the
WSOC-nitrate correlation was highest (&lt;I&gt;R&lt;/I&gt;&lt;sup&gt;2&lt;/sup&gt;=0.88) between the hours of
08:00&amp;ndash;12:45, indicating similar sources and processing during this period.
The results show that WSOC also experienced evaporation losses and that a
significant fraction of the MCMA secondary organic aerosol (SOA) measured at
the surface was semi-volatile.</abstract>
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</article>

