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<!DOCTYPE article SYSTEM "http://www.atmos-chem-phys-discuss.net/inc/acpd/copernicus.dtd">
<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>6</volume_number>
		<issue_number>1</issue_number>
		<publication_year>2006</publication_year>
	</journal>
	<doi>10.5194/acpd-6-1275-2006</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/6/1275/2006/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/6/1275/2006/acpd-6-1275-2006.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/6/1275/2006/acpd-6-1275-2006.pdf</fulltext_pdf>
	<start_page>1275</start_page>
	<end_page>1299</end_page>
	<publication_date>2006-02-17</publication_date>
	<article_title content_type="html">The quantitative infrared and NIR spectrum of CH&lt;sub&gt;2&lt;/sub&gt;I&lt;sub&gt;2&lt;/sub&gt; vapor: vibrational assignments and potential for atmospheric monitoring</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>T. J. Johnson</name>
		</author>
		<author numeration="2" affiliations="1">
			<name>T. Masiello</name>
		</author>
		<author numeration="3" affiliations="1">
			<name>S. W. Sharpe</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Pacific Northwest National Laboratory, Richland, WA 99354, USA</affiliation>
	</affiliations>
	<abstract content_type="html">Diiodomethane (CH&lt;sub&gt;2&lt;/sub&gt;I&lt;sub&gt;2&lt;/sub&gt;) photolysis in the presence of ozone is a
suggested precursor to new particle aerosol formation, particularly in
coastal areas. As part of the PNNL database of gas-phase infrared spectra,
the quantitative absorption spectrum of CH&lt;sub&gt;2&lt;/sub&gt;I&lt;sub&gt;2&lt;/sub&gt; has been acquired at
0.1 cm&lt;sup&gt;&amp;minus;1&lt;/sup&gt; resolution. Two strong b&lt;sub&gt;2&lt;/sub&gt; symmetry A-type bands at 584
and 1114 cm&lt;sup&gt;&amp;minus;1&lt;/sup&gt; are observed, but are not resolved at 760 Torr and appear
as B-type. In contrast, the b&lt;sub&gt;1&lt;/sub&gt; symmetry C-type bands near 5953, 4426
and 3073 cm&lt;sup&gt;&amp;minus;1&lt;/sup&gt; are resolved with rotational structure, including
Q-branches with widths &amp;#x2264;1 cm&lt;sup&gt;&amp;minus;1&lt;/sup&gt;. The quantitative infrared and
near-infrared vapor-phase spectra (600&amp;ndash;10&amp;nbsp;000 cm&lt;sup&gt;&amp;minus;1&lt;/sup&gt;) are reported for
the first time and discussed in terms of atmospheric monitoring. FT-Raman
spectra and ab initio calculations are used to complete vibrational assignments in the
C&lt;sub&gt;2v&lt;/sub&gt; point group.</abstract>
	<references>
	</references>
</article>

