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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>2</issue_number>
		<publication_year>2009</publication_year>
	</journal>
	<doi>10.5194/acpd-9-7115-2009</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/9/7115/2009/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/9/7115/2009/acpd-9-7115-2009.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/9/7115/2009/acpd-9-7115-2009.pdf</fulltext_pdf>
	<start_page>7115</start_page>
	<end_page>7154</end_page>
	<publication_date>2009-03-17</publication_date>
	<article_title content_type="html">Kinetics and mechanisms of heterogeneous reaction of NO&lt;sub&gt;2&lt;/sub&gt; on CaCO&lt;sub&gt;3&lt;/sub&gt; surfaces under dry and wet conditions</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>H. J. Li</name>
		</author>
		<author numeration="2" affiliations="1">
			<name>T. Zhu</name>
			<email>tzhu@pku.edu.cn</email>
		</author>
		<author numeration="3" affiliations="1">
			<name>D. F. Zhao</name>
		</author>
		<author numeration="4" affiliations="1">
			<name>Z. F. Zhang</name>
		</author>
		<author numeration="5" affiliations="1">
			<name>Z. M. Chen</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">State Key Joint Laboratory of Environmental Simulation and Pollution Control, College of Environmental Sciences and Engineering, Peking University, Beijing, 100871, China</affiliation>
	</affiliations>
	<abstract content_type="html">Calcium nitrate (Ca(NO&lt;sub&gt;3&lt;/sub&gt;)&lt;sub&gt;2&lt;/sub&gt;) was observed in mineral dust and could
change the hygroscopic and optical properties of mineral dust significantly
due to its strong water solubility. The reaction of calcium carbonate
(CaCO&lt;sub&gt;3&lt;/sub&gt;) with nitric acid (HNO&lt;sub&gt;3&lt;/sub&gt;) is believed the main reason for
the observed Ca(NO&lt;sub&gt;3&lt;/sub&gt;)&lt;sub&gt;2&lt;/sub&gt; in the mineral dust. In the atmosphere, the
concentration of nitrogen dioxide (NO&lt;sub&gt;2&lt;/sub&gt;) is orders of magnitude higher
than that of HNO&lt;sub&gt;3&lt;/sub&gt;; however, little is known about the reaction of
NO&lt;sub&gt;2&lt;/sub&gt; with CaCO&lt;sub&gt;3&lt;/sub&gt;. In this study, the heterogeneous reaction of
NO&lt;sub&gt;2&lt;/sub&gt; on the surface of CaCO&lt;sub&gt;3&lt;/sub&gt; particles was investigated using
diffuse reflectance infrared Fourier transform spectroscopy (DRIFTS)
combined with X-ray photoelectron spectroscopy (XPS) and scanning electron
microscopy (SEM) under wet and dry conditions. Nitrate formation was
observed in both conditions, and nitrite was observed under wet conditions,
indicating the reaction of NO&lt;sub&gt;2&lt;/sub&gt; on the CaCO&lt;sub&gt;3&lt;/sub&gt; surface produced
nitrate and probably nitrous acid (HONO). Relative humidity (RH) influenced
both the initial uptake coefficient and the reaction mechanism. With RH&lt;52%, surface –OH was formed through dissociation of the surface adsorbed
water via oxygen vacancy, thus determining the reaction order. With RH&gt;52%, a monolayer of water formed on the surface of the CaCO&lt;sub&gt;3&lt;/sub&gt;
particles, which reacted with NO&lt;sub&gt;2&lt;/sub&gt; as a first order reaction, forming
HNO&lt;sub&gt;3&lt;/sub&gt; and HONO. The initial uptake coefficient γ&lt;sub&gt;0&lt;/sub&gt; was
determined to be (1.66&amp;plusmn;0.38)&amp;times;10&lt;sup&gt;&amp;minus;7&lt;/sup&gt; under dry
conditions and up to (0.84&amp;plusmn;0.44)&amp;times;10&lt;sup&gt;&amp;minus;6&lt;/sup&gt; under wet
conditions. Considering that NO&lt;sub&gt;2&lt;/sub&gt; concentrations in the atmosphere are
orders of magnitude higher than those of HNO&lt;sub&gt;3&lt;/sub&gt;, the reaction of NO&lt;sub&gt;2&lt;/sub&gt;
on CaCO&lt;sub&gt;3&lt;/sub&gt; particle should have similar importance as that of HNO&lt;sub&gt;3&lt;/sub&gt;
in the atmosphere and could also be an important source of HONO in the
atmosphere.</abstract>
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</article>

