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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-6-579-2006</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/6/579/2006/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/6/579/2006/acpd-6-579-2006.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/6/579/2006/acpd-6-579-2006.pdf</fulltext_pdf>
	<start_page>579</start_page>
	<end_page>613</end_page>
	<publication_date>2006-01-17</publication_date>
	<article_title content_type="html">Kinetics and mechanism of heterogeneous oxidation of sulfur dioxide by ozone on surface of calcium carbonate</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>L. Li</name>
		</author>
		<author numeration="2" affiliations="1">
			<name>Z. M. Chen</name>
		</author>
		<author numeration="3" affiliations="1">
			<name>Y. H. Zhang</name>
		</author>
		<author numeration="4" affiliations="1">
			<name>T. Zhu</name>
		</author>
		<author numeration="5" affiliations="1">
			<name>J. L. Li</name>
		</author>
		<author numeration="6" affiliations="1">
			<name>J. Ding</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">State Key Joint Laboratory of Environment Simulation and Pollution Control, College of Environmental Sciences, Peking University, Beijing 100871, China</affiliation>
	</affiliations>
	<abstract content_type="html">Sulfate particles play a key role in the air quality and the global climate,
but the heterogeneous formation mechanism of sulfates on surfaces of
atmospheric particles is not well established. Carbonates, which act as a
reactive component in mineral dust due to their special chemical properties,
may contribute significantly to the sulfate formation by heterogeneous
processes. This paper presents a study on the oxidation of SO&lt;sub&gt;2&lt;/sub&gt; by
O&lt;sub&gt;3&lt;/sub&gt; on CaCO&lt;sub&gt;3&lt;/sub&gt; particles. Using Diffuse Reflectance Infrared Fourier
Transform Spectroscopy (DRIFTS), the formation of sulfite and sulfate on the
surface was identified, and the roles of O&lt;sub&gt;3&lt;/sub&gt; and water in oxidation
processes were determined. The results showed that in the presence of
O&lt;sub&gt;3&lt;/sub&gt;, SO&lt;sub&gt;2&lt;/sub&gt; can be oxidized to sulfate on the surface of CaCO&lt;sub&gt;3&lt;/sub&gt;
particles. The reaction is first order in SO&lt;sub&gt;2&lt;/sub&gt; and zero order in
O&lt;sub&gt;3&lt;/sub&gt;. The reactive uptake coefficient for SO&lt;sub&gt;2&lt;/sub&gt; oxidation by O&lt;sub&gt;3&lt;/sub&gt;
was determined to be (1.4&amp;plusmn;0.3)&amp;times;10&lt;sup&gt;&amp;minus;7&lt;/sup&gt; using the BET area
as the reactive area and (7.7&amp;plusmn;1.6)&amp;times;10&lt;sup&gt;&amp;minus;4&lt;/sup&gt; using the
geometric area. A two-stage mechanism that involves adsorption of SO&lt;sub&gt;2&lt;/sub&gt;
followed by O&lt;sub&gt;3&lt;/sub&gt; oxidation is proposed and the adsorption of SO&lt;sub&gt;2&lt;/sub&gt; on
the CaCO&lt;sub&gt;3&lt;/sub&gt; surface is the rate-determining step. The proposed mechanism
can well explain the experiment results. The atmospheric implications were
explored based on a box model calculation. It was found that the
heterogeneous reaction might be an important pathway for sulfate formation
in the atmosphere.</abstract>
	<references>
	</references>
</article>

