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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>9</volume_number>
		<issue_number>1</issue_number>
		<publication_year>2009</publication_year>
	</journal>
	<doi>10.5194/acpd-9-4231-2009</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/9/4231/2009/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/9/4231/2009/acpd-9-4231-2009.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/9/4231/2009/acpd-9-4231-2009.pdf</fulltext_pdf>
	<start_page>4231</start_page>
	<end_page>4249</end_page>
	<publication_date>2009-02-09</publication_date>
	<article_title content_type="html">Ammonia in positively charged pre-nucleation clusters: a quantum-chemical  study and atmospheric implications</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>A. B. Nadykto</name>
		</author>
		<author numeration="2" affiliations="1">
			<name>F. Yu</name>
			<email>yfq@asrc.cestm.albany.edu</email>
		</author>
		<author numeration="3" affiliations="1">
			<name>J. Herb</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Atmospheric Sciences Research Center, State University of New York at Albany,  251 Fuller Rd., Albany, NY 12203, USA</affiliation>
	</affiliations>
	<abstract content_type="html">The quantum-chemical treatment of pre-nucleation clusters consisting
      of atmospheric nucleation precursors is critically important for the
      understanding of the molecular nature of atmospheric nucleation. In
      the present study, the influence of ammonia on the thermochemical
      stability of positively charged pre-nucleation clusters has been
      studied using the Density Functional Theory (DFT). The formation of
      binary (NH&lt;sub&gt;4&lt;/sub&gt;&lt;sup&gt;+&lt;/sup&gt;)(H&lt;sub&gt;2&lt;/sub&gt;O)&lt;sub&gt;n&lt;/sub&gt; and ternary
      (NH&lt;sub&gt;4&lt;/sub&gt;&lt;sup&gt;+&lt;/sup&gt;)(H&lt;sub&gt;2&lt;/sub&gt;OSO&lt;sub&gt;4&lt;/sub&gt;)(H&lt;sub&gt;2&lt;/sub&gt;O)&lt;sub&gt;n&lt;/sub&gt; ionic clusters and the
      conversion of (H&lt;sub&gt;3&lt;/sub&gt;O&lt;sup&gt;+&lt;/sup&gt;)(H&lt;sub&gt;2&lt;/sub&gt;O)&lt;sub&gt;n&amp;minus;1&lt;/sub&gt; into
      (NH&lt;sub&gt;4&lt;/sub&gt;&lt;sup&gt;+&lt;/sup&gt;)(H&lt;sub&gt;2&lt;/sub&gt;O)&lt;sub&gt;n&lt;/sub&gt; and
      (H&lt;sub&gt;3&lt;/sub&gt;O&lt;sup&gt;+&lt;/sup&gt;)(H&lt;sub&gt;2&lt;/sub&gt;SO&lt;sub&gt;4&lt;/sub&gt;)(H&lt;sub&gt;2&lt;/sub&gt;O)&lt;sub&gt;n&amp;minus;1&lt;/sub&gt; into
      (NH&lt;sub&gt;4&lt;/sub&gt;&lt;sup&gt;+&lt;/sup&gt;)(H&lt;sub&gt;2&lt;/sub&gt;SO&lt;sub&gt;4&lt;/sub&gt;)(H&lt;sub&gt;2&lt;/sub&gt;O)&lt;sub&gt;n&lt;/sub&gt; have been
      investigated. The thermochemical analysis carried out in the present
      study shows both (H&lt;sub&gt;3&lt;/sub&gt;O&lt;sup&gt;+&lt;/sup&gt;)(H&lt;sub&gt;2&lt;/sub&gt;O)&lt;sub&gt;n&amp;minus;1&lt;/sub&gt;&amp;rarr;
      (NH&lt;sub&gt;4&lt;/sub&gt;&lt;sup&gt;+&lt;/sup&gt;)(H&lt;sub&gt;2&lt;/sub&gt;O)&lt;sub&gt;n&lt;/sub&gt; and
      (H&lt;sub&gt;2&lt;/sub&gt;SO&lt;sub&gt;4&lt;/sub&gt;)(H&lt;sub&gt;3&lt;/sub&gt;O&lt;sup&gt;+&lt;/sup&gt;)(H&lt;sub&gt;2&lt;/sub&gt;O)&lt;sub&gt;n&amp;minus;1&lt;/sub&gt;&amp;rarr;
      (NH&lt;sub&gt;4&lt;/sub&gt;&lt;sup&gt;+&lt;/sup&gt;)(H&lt;sub&gt;2&lt;/sub&gt;SO&lt;sub&gt;4&lt;/sub&gt;)(H&lt;sub&gt;2&lt;/sub&gt;O)&lt;sub&gt;n&lt;/sub&gt; transformations to be
      favorable thermodynamically and gives us a clear indication of the
      important role of ammonia in the conversion of positively charged
      clusters containing hydronium (H&lt;sub&gt;3&lt;/sub&gt;O&lt;sup&gt;+&lt;/sup&gt;) into those containing
      protonated ammonia. Under typical continental boundary layer
      condition, a large fraction of positive sulfuric acid monomer ions may
      contain ammonia. The ratio of
      NH&lt;sub&gt;4&lt;/sub&gt;&lt;sup&gt;+&lt;/sup&gt;(H&lt;sub&gt;2&lt;/sub&gt;SO&lt;sub&gt;4&lt;/sub&gt;)(H&lt;sub&gt;2&lt;/sub&gt;O)&lt;sub&gt;n+1&lt;/sub&gt; to
      (H&lt;sub&gt;3&lt;/sub&gt;O)&lt;sup&gt;+&lt;/sup&gt;(H&lt;sub&gt;2&lt;/sub&gt;SO&lt;sub&gt;4&lt;/sub&gt;)(H&lt;sub&gt;2&lt;/sub&gt;O)&lt;sub&gt;n&lt;/sub&gt; decreases
      significantly with the hydration number but is still above ~10
      when &lt;i&gt;n&lt;/i&gt;=5. In contrast, most of neutral and negative hydrated
      sulfuric acid monomers do not contain ammonia. The atmospheric
      implications of the obtained results are discussed.</abstract>
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</article>

