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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>10</volume_number>
		<issue_number>1</issue_number>
		<publication_year>2010</publication_year>
	</journal>
	<doi>10.5194/acpd-10-1823-2010</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/10/1823/2010/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/10/1823/2010/acpd-10-1823-2010.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/10/1823/2010/acpd-10-1823-2010.pdf</fulltext_pdf>
	<start_page>1823</start_page>
	<end_page>1846</end_page>
	<publication_date>2010-01-21</publication_date>
	<article_title content_type="html">Patterns of mercury dispersion from local and regional emission sources, rural Central Wisconsin, USA</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>A. Kolker</name>
			<email>akolker@usgs.gov</email>
		</author>
		<author numeration="2" affiliations="2">
			<name>M. L. Olson</name>
		</author>
		<author numeration="3" affiliations="2">
			<name>D. P. Krabbenhoft</name>
		</author>
		<author numeration="4" affiliations="2">
			<name>M. T. Tate</name>
		</author>
		<author numeration="5" affiliations="1">
			<name>M. A. Engle</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">US Geological Survey, Eastern Energy Resources Science Center, Reston,  VA, 20192, USA</affiliation>
		<affiliation numeration="2" content_type="html">US Geological Survey, Wisconsin Water Science Center, Middleton, WI,  53562, USA</affiliation>
	</affiliations>
	<abstract content_type="html">Simultaneous real-time changes in mercury (Hg) speciation –
      reactive gaseous Hg (RGM), elemental Hg (Hg&amp;deg;), 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 RGM, Hg&amp;deg; and Hg-PM&lt;sub&gt;2.5&lt;/sub&gt;, were
      positioned at distances of 25, 50 and 100 km northward of the
      larger electric utility. 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;&amp;minus;3&lt;/sup&gt;) measured at the 100 km site, and
      corresponding elevated SO&lt;sub&gt;2&lt;/sub&gt; (10.41 ppbv; measured at
      50 km site). The finding that RGM, Hg&amp;deg;, 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&amp;deg;. Operational changes at each emitter since 2007
      should reduce their Hg output, potentially allowing
      quantification of the environmental benefit in future studies.</abstract>
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</article>

