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<front>
<journal-meta>
<journal-id journal-id-type="publisher">ACP</journal-id>
<journal-title-group>
<journal-title>Atmospheric Chemistry and Physics</journal-title>
<abbrev-journal-title abbrev-type="publisher">ACP</abbrev-journal-title>
</journal-title-group>
<issn pub-type="epub">1680-7324</issn>
<publisher><publisher-name>Copernicus GmbH</publisher-name>
<publisher-loc>Göttingen, Germany</publisher-loc>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.5194/acp-10-4467-2010</article-id>
<title-group>
<article-title>Patterns of mercury dispersion from local and regional emission sources, rural Central Wisconsin, USA</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Kolker</surname>
<given-names>A.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Olson</surname>
<given-names>M. L.</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Krabbenhoft</surname>
<given-names>D. P.</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Tate</surname>
<given-names>M. T.</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Engle</surname>
<given-names>M. A.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>US Geological Survey, Eastern Energy Resources Science Center, Reston, VA, 20192 USA</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>US Geological Survey, Wisconsin Water Science Center, Middleton, WI, 53562 USA</addr-line>
</aff>
<pub-date pub-type="epub">
<day>17</day>
<month>05</month>
<year>2010</year>
</pub-date>
<volume>10</volume>
<issue>10</issue>
<fpage>4467</fpage>
<lpage>4476</lpage>
<permissions>
<license xlink:type="simple">
<license-p>This is an open-access article ditributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited.</license-p>
</license>
</permissions>
<self-uri xlink:href="http://www.atmos-chem-phys.net/10/4467/2010/acp-10-4467-2010.html">This article is available from http://www.atmos-chem-phys.net/10/4467/2010/acp-10-4467-2010.html</self-uri>
<self-uri xlink:href="http://www.atmos-chem-phys.net/10/4467/2010/acp-10-4467-2010.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys.net/10/4467/2010/acp-10-4467-2010.pdf</self-uri>
<abstract>
<p>Simultaneous real-time changes in mercury (Hg) speciation- reactive gaseous
Hg (RGM), elemental Hg (Hg°), and fine particulate Hg (Hg-PM&lt;sub&gt;2.5&lt;/sub&gt;),
were determined from June to November, 2007, in ambient air at three
locations in rural Central Wisconsin. Known Hg emission sources within the
airshed of the monitoring sites include: 1) a 1114 megawatt (MW) coal-fired
electric utility generating station; 2) a Hg-bed chlor-alkali plant; and 3) a
smaller (465 MW) coal-burning electric utility. Monitoring sites, showing
sporadic elevation of Hg°, Hg-PM&lt;sub&gt;2.5&lt;/sub&gt;, and RGM were positioned at
distances of 25, 50 and 100 km northward of the larger electric utility.
Median concentrations of Hg°, Hg-PM&lt;sub&gt;2.5&lt;/sub&gt;, and RGM were
1.3–1.4 ng m&lt;sup&gt;−3&lt;/sup&gt;, 2.6–5.0 pg m&lt;sup&gt;−3&lt;/sup&gt;, and 0.6–0.8 pg m&lt;sup&gt;−3&lt;/sup&gt;,
respectively. A series of RGM events were recorded at each site. The largest,
on 23 September, occurred under prevailing southerly winds, with a maximum
RGM value (56.8 pg m&lt;sup&gt;-3&lt;/sup&gt;) measured at the 100 km site, and
corresponding elevated SO&lt;sub&gt;2&lt;/sub&gt; (10.4 ppbv; measured at 50 km site). The
finding that RGM, Hg°, and Hg-PM&lt;sub&gt;2.5&lt;/sub&gt; are not always highest at the
25 km site, closest to the large generating station, contradicts the idea
that RGM decreases with distance from a large point source. This may be
explained if: 1) the 100 km site was influenced by emissions from the
chlor-alkali facility or by RGM from regional urban sources; 2) the emission
stack height of the larger power plant promoted plume transport at an
elevation where the Hg is carried over the closest site; or 3) RGM was being
generated in the plume through oxidation of Hg°. Operational changes
at each emitter since 2007 should reduce their Hg output, potentially
allowing quantification of the environmental benefit in future studies.</p>
</abstract>
<counts><page-count count="10"/></counts>
</article-meta>
</front>
<body/>
<back>
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</article>