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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>10</volume_number>
		<issue_number>3</issue_number>
		<publication_year>2010</publication_year>
	</journal>
	<doi>10.5194/acpd-10-6829-2010</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/10/6829/2010/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/10/6829/2010/acpd-10-6829-2010.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/10/6829/2010/acpd-10-6829-2010.pdf</fulltext_pdf>
	<start_page>6829</start_page>
	<end_page>6869</end_page>
	<publication_date>2010-03-11</publication_date>
	<article_title content_type="html">Isotope modeling of nitric acid formation in the atmosphere using ISO-RACM: testing the importance of NO oxidation, heterogeneous reactions, and trace gas chemistry</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>G. Michalski</name>
			<email>gmichals@purdue.edu</email>
		</author>
		<author numeration="2" affiliations="1">
			<name>F. Xu</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Department of Chemistry, Earth and Atmospheric Sciences, Purdue University 550 Stadium Mall Dr. West Lafayette, West Lafayette, IN, USA</affiliation>
	</affiliations>
	<abstract content_type="html">Here we present ISO-RACM, an isotope mass balance model that utilizes the Regional
Atmospheric Chemistry Mechanism to predict &amp;Delta;&lt;sup&gt;17&lt;/sup&gt;O values in atmospheric nitrate. A
large number of simulations were carried out that varied atmospheric parameters that are
important in altering the magnitude and range of &amp;Delta;&lt;sup&gt;17&lt;/sup&gt;O values generated in
photochemically produce nitrate. These parameters included temperature, relative
humidity, actinic flux, aerosol surface area and chemical speciation, and three different
N&lt;sub&gt;2&lt;/sub&gt;O&lt;sub&gt;5&lt;/sub&gt; uptake parameterizations. Trace gas mixing ratios were also varied including CH&lt;sub&gt;4&lt;/sub&gt;,
CO, NO&lt;sub&gt;x&lt;/sub&gt;, O&lt;sub&gt;3&lt;/sub&gt;, volatile organic compounds and biogenic organic compounds. The model
predicts that there are seasonal, latitudinal and diurnal variations in &amp;Delta;&lt;sup&gt;17&lt;/sup&gt;O values due to
changes in actinic flux with lower values corresponding to higher actinic fluxes. There
was also a minor positive correlation between higher &amp;Delta;&lt;sup&gt;17&lt;/sup&gt;O values and increased
temperature. There were distinct differences in &amp;Delta;&lt;sup&gt;17&lt;/sup&gt;O depending on which
N&lt;sub&gt;2&lt;/sub&gt;O&lt;sub&gt;5&lt;/sub&gt; parameterization was used, mostly the result of changing relative humidity being a factor
in two of the parameterization schemes. Changing CO and CH&lt;sub&gt;4&lt;/sub&gt; mixing ratios had
negligible impact on &amp;Delta;&lt;sup&gt;17&lt;/sup&gt;O values but significant variation in magnitude and range were
predicted with NO&lt;sub&gt;x&lt;/sub&gt;, O&lt;sub&gt;3&lt;/sub&gt;, and organic loading. High NO&lt;sub&gt;x&lt;/sub&gt; and O&lt;sub&gt;3&lt;/sub&gt; generated high &amp;Delta;&lt;sup&gt;17&lt;/sup&gt;O with
a narrow (10 &amp;permil;) range, while high organics led to low &amp;Delta;&lt;sup&gt;17&lt;/sup&gt;O values and a wider range of
possible values. Implications for using &amp;Delta;&lt;sup&gt;17&lt;/sup&gt;O to evaluate NO&lt;sub&gt;x&lt;/sub&gt;-NO&lt;sub&gt;y&lt;/sub&gt; chemistry and aerosol
formation processes are discussed, as is needed future research.</abstract>
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</article>

