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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>R. L. Smith</dc:contributor>
  <dc:creator>S.H. Harris</dc:creator>
  <dc:date>2009</dc:date>
  <dc:description>&lt;div id="abstracts" class="Abstracts"&gt;&lt;div id="aep-abstract-id11" class="abstract author"&gt;&lt;div id="aep-abstract-sec-id12"&gt;&lt;p id="simple-para.0040"&gt;Nitrification and nitrate reduction were examined in an ephemeral drainage channel receiving discharge from coalbed natural gas (CBNG) production wells in the Powder River Basin, Wyoming. CBNG co-produced water typically contains dissolved inorganic nitrogen (DIN), primarily as ammonium. In this study, a substantial portion of discharged ammonium was oxidized within 50&amp;nbsp;m of downstream transport, but speciation was markedly influenced by diel fluctuations in dissolved oxygen (&amp;gt;&amp;nbsp;300&amp;nbsp;µM). After 300&amp;nbsp;m of transport, 60% of the initial DIN load had been removed. The effect of benthic nitrogen-cycling processes on stream water chemistry was assessed at 2 locations within the stream channel using acrylic chambers to conduct short-term (2–6&amp;nbsp;h), in-stream incubations. The highest ambient DIN removal rates (2103&amp;nbsp;µmol N m&lt;sup&gt;−&amp;nbsp;2&lt;/sup&gt;h&lt;sup&gt;−&amp;nbsp;1&lt;/sup&gt;) were found at a location where ammonium concentrations &amp;gt;&amp;nbsp;350&amp;nbsp;µM. This occurred during light incubations when oxygen concentrations were highest. Nitrification was occurring at the site, however, net accumulation of nitrate and nitrite accounted for &amp;lt;&amp;nbsp;12% of the ammonium consumed, indicating that other ammonium-consuming processes were also occurring. In dark incubations, nitrite and nitrate consumption were dominant processes, while ammonium was produced rather than consumed. At a downstream location nitrification was not a factor and changes in DIN removal rates were controlled by nitrate reduction, diel fluctuations in oxygen concentration, and availability of electron donor. This study indicates that short-term adaptation of stream channel processes can be effective for removing CBNG DIN loads given sufficient travel distances, but the long-term potential for nitrogen remobilization and nitrogen saturation remain to be determined.&lt;/p&gt;&lt;/div&gt;&lt;/div&gt;&lt;/div&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1016/j.chemgeo.2009.01.028</dc:identifier>
  <dc:language>en</dc:language>
  <dc:title>In situ measurements of microbially-catalyzed nitrification and nitrate reduction rates in an ephemeral drainage channel receiving water from coalbed natural gas discharge, Powder River Basin, Wyoming, USA</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>