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<oai_dc:dc xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:oai_dc="http://www.openarchives.org/OAI/2.0/oai_dc/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/oai_dc/ http://www.openarchives.org/OAI/2.0/oai_dc.xsd">
  <dc:contributor>Douglas A. Burns</dc:contributor>
  <dc:contributor>Peter S. Murdoch</dc:contributor>
  <dc:contributor>Rene H. Germain</dc:contributor>
  <dc:creator>Jason Siemion</dc:creator>
  <dc:date>2011</dc:date>
  <dc:description>Previous studies have shown that clearcutting of northern hardwood forests mobilizes base cations, inorganic monomeric aluminum (Al&lt;sub&gt;im&lt;/sub&gt;), and nitrate (NO&lt;sub&gt;3&lt;/sub&gt;&lt;sup&gt;-&lt;/sup&gt;&lt;sub&gt;-&lt;/sub&gt;N) from soils to surface waters, but the effects of partial harvests on NO&lt;sub&gt;3&lt;/sub&gt;&lt;sup&gt;-&lt;/sup&gt;&lt;sub&gt;-&lt;/sub&gt;N have been less frequently studied. In this study we describe the effects of a series of partial harvests of varying proportions of basal area removal (22%, 28% and 68%) on Al&lt;sub&gt;im&lt;/sub&gt;, calcium (Ca&lt;sup&gt;2+&lt;/sup&gt;), and NO&lt;sub&gt;3&lt;/sub&gt;&lt;sup&gt;-&lt;/sup&gt;&lt;sub&gt;-&lt;/sub&gt;N concentrations in soil extracts, soil water, and surface water in the Catskill Mountains of New York, USA. Increases in NO&lt;sub&gt;3&lt;/sub&gt;&lt;sup&gt;-&lt;/sup&gt;&lt;sub&gt;-&lt;/sub&gt;N concentrations relative to pre-harvest values were observed within a few months after harvest in soils, soil water, and stream water for all three harvests. Increases in Al&lt;sub&gt;im&lt;/sub&gt; and Ca&lt;sup&gt;2+&lt;/sup&gt; concentrations were also evident in soil water and stream water over the same time period for all three harvests. The increases in Al&lt;sub&gt;im&lt;/sub&gt;, Ca&lt;sup&gt;2+&lt;/sup&gt;, and NO&lt;sub&gt;3&lt;/sub&gt;&lt;sup&gt;-&lt;/sup&gt;&lt;sub&gt;-&lt;/sub&gt;N concentrations in the 68% harvest were statistically significant as measured by comparing the 18-month pre-harvest period with the 18-month post-harvest period, with fewer significant responses in the two harvests of lowest intensity. All three solutes returned to pre-harvest concentrations in soil water and stream water in the two lowest intensity harvests in 2&amp;ndash;3 years compared to a full 3 years in the 68% harvest. When the results of this study were combined with those of a previous nearby clearcut and 40% harvest, the post-harvest increases in NO&lt;sub&gt;3&lt;/sub&gt;&lt;sup&gt;-&lt;/sup&gt;&lt;sub&gt;-&lt;/sub&gt;N concentrations in stream water and soil water suggest a harvesting level above which the relation between concentration and harvest intensity changes; there was a greater change in concentration per unit change in harvest intensity when basal area removal was greater than 40%. These results indicate that the deleterious effects on aquatic ecosystems previously demonstrated for intensive harvests in northern hardwood forests of northeastern North America that receive high levels of atmospheric N deposition can be greatly diminished as harvesting intensity decreases below 40?8%. These results await confirmation through additional incremental forest harvest studies at other locations throughout the world that receive high levels of atmospheric N deposition.</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1016/j.foreco.2011.01.036</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>Elsevier</dc:publisher>
  <dc:title>The relation of harvesting intensity to changes in soil, soil water, and stream chemistry in a northern hardwood forest, Catskill Mountains, USA</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>