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<!DOCTYPE article SYSTEM "http://www.hydrol-earth-syst-sci.net/inc/hess/copernicus.dtd">
<article language="en">
	<journal>
		<journal_title>Hydrology and Earth System Sciences</journal_title>
		<journal_url>www.hydrol-earth-syst-sci.net</journal_url>
		<issn>1027-5606</issn>
		<eissn>1607-7938</eissn>
		<volume_number>7</volume_number>
		<issue_number>4</issue_number>
		<publication_year>2003</publication_year>
	</journal>
	<doi>10.5194/hess-7-561-2003</doi>
	<article_url>http://www.hydrol-earth-syst-sci.net/7/561/2003/</article_url>
	<abstract_html>http://www.hydrol-earth-syst-sci.net/7/561/2003/hess-7-561-2003.html</abstract_html>
	<fulltext_pdf>http://www.hydrol-earth-syst-sci.net/7/561/2003/hess-7-561-2003.pdf</fulltext_pdf>
	<start_page>561</start_page>
	<end_page>573</end_page>
	<publication_date>0000-00-00</publication_date>
	<article_title content_type="html">Acidification and recovery of aquatic ecosystems in south central Ontario, Canada: regional application of the MAGIC model</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>J. Aherne</name>
		</author>
		<author numeration="2" affiliations="1">
			<name>P. J. Dillon</name>
		</author>
		<author numeration="3" affiliations="2">
			<name>B. J. Cosby</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Environmental and Resource Studies, Trent University, Peterborough, ON K9J 7B8, Canada</affiliation>
		<affiliation numeration="2" content_type="html">Department of Environmental Sciences, University of Virginia, Charlottesville, USA</affiliation>
	</affiliations>
	<abstract content_type="html">The dynamic model MAGIC was applied to 25 lakes in south-central Ontario, 
        Canada using a regional modelling methodology. Soil and lake water chemistry for each 
        lake catchment was simulated for the period 1850–2050. Sulphate 
        (SO&lt;sub&gt;4&lt;/sub&gt;&lt;sup&gt;2–&lt;/sup&gt;) deposition forecasts were derived from recently proposed 
        emission reductions, which correspond roughly to a 50% reduction in 
        SO&lt;sub&gt;4&lt;/sub&gt;&lt;sup&gt;2–&lt;/sup&gt; deposition by 2010 from the 2000 baseline. Changes in 
        SO&lt;sub&gt;4&lt;/sub&gt;&lt;sup&gt;2–&lt;/sup&gt; deposition had a significant impact on lake chemistry. 
        Simulated lake water chemistry showed a recovery potential under the current deposition 
        scenario; by 2050 concentration levels recovered to values predicted for the early 1900s. 
        Moreover, simulated future lake water chemistry showed significant recovery compared to 
        1975 levels. However, although regional simulations predict that base cation losses 
        have decreased in recent years, soils in the region will continue to acidify with 
        Ca&lt;sup&gt;2+&lt;/sup&gt; losses dominating depletion of the exchangeable pool. Base cation losses 
        from the exchangeable pool are currently buffering lakes against the impacts of acid 
        deposition; ultimately base cation inputs into the lakes will decrease as exchangeable 
        base cation pools become depleted. Further emission reductions are necessary to ensure 
        continued recovery from acidification.&lt;/p&gt;
&lt;p  style=&quot;line-height: 20px;&quot;&gt;&lt;b&gt;Keywords: &lt;/b&gt;regional dynamic model, sulphate, acid neutralising capacity, critical loads, 
      lake chemistry, soil base saturation</abstract>
	<references>
	</references>
</article>

