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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>Alexander Berner</dc:contributor>
  <dc:contributor>Gregory A. Wetherbee</dc:contributor>
  <dc:contributor>Sheila F. Murphy</dc:contributor>
  <dc:contributor>Ruth C. Heindel</dc:contributor>
  <dc:creator>J. David Felix</dc:creator>
  <dc:date>2023</dc:date>
  <dc:description>&lt;div id="abs0010" class="abstract author" lang="en"&gt;&lt;div id="abssec0010"&gt;&lt;p id="abspara0010"&gt;Urban ammonia (NH&lt;sub&gt;3&lt;/sub&gt;) emissions contribute to poor local air quality and can be transported to rural landscapes, impacting sensitive ecosystems. The Colorado Front Range urban corridor encompasses the Denver Metropolitan Area, rural farmland/rangeland and montane forest between the city and the Rocky Mountains. Reactive nitrogen emissions from the corridor are partly responsible for increased N deposition to the wildland-urban interface (WUI) in this region. To determine the significance of individual NH&lt;sub&gt;3&lt;/sub&gt;&lt;span&gt;&amp;nbsp;&lt;/span&gt;sources to WUI ecosystems, we measured the concentration and isotopic composition (δ&lt;sup&gt;15&lt;/sup&gt;N–NH&lt;sub&gt;3&lt;/sub&gt;) of ambient NH&lt;sub&gt;3(g)&lt;/sub&gt;&lt;span&gt;&amp;nbsp;&lt;/span&gt;from April to October 2018 across a five-site urban to rural gradient in the corridor. The urban sites had higher NH&lt;sub&gt;3&lt;/sub&gt;&lt;span&gt;&amp;nbsp;&lt;/span&gt;concentrations and δ&lt;sup&gt;15&lt;/sup&gt;N–NH&lt;sub&gt;3&lt;/sub&gt;&lt;span&gt;&amp;nbsp;&lt;/span&gt;values than the rural/suburban sites. Based on isotope mixing models, NH&lt;sub&gt;3&lt;/sub&gt;&lt;span&gt;&amp;nbsp;&lt;/span&gt;emission source contributions for all sites were fertilizer (12&amp;nbsp;±&amp;nbsp;5.7%), livestock waste (18&amp;nbsp;±&amp;nbsp;12%), vehicles (37&amp;nbsp;±&amp;nbsp;23%), and biomass burning (34&amp;nbsp;±&amp;nbsp;20%). Vehicle contributions were consistent across all months with an average of 35% and summer months showed a peak in biomass burning contributions (40%). As wildfires are projected to increase due to climate change, we stress a need for constraints on the isotopic signature of NH&lt;sub&gt;3&lt;/sub&gt;&lt;span&gt;&amp;nbsp;&lt;/span&gt;emitted from wildfires. Vehicle emissions contributed the greatest amount of NH&lt;sub&gt;3&lt;/sub&gt;&lt;span&gt;&amp;nbsp;&lt;/span&gt;(40%) at the urban sites while rural/suburban sites had higher agricultural contributions (41%). Had 2018 not had an anomalously high wildfire season, 46% and 60% of the NH&lt;sub&gt;3&lt;/sub&gt;&lt;span&gt;&amp;nbsp;&lt;/span&gt;would have been attributed to vehicle emissions at the WUI site and urban sites, respectively. NH&lt;sub&gt;3&lt;/sub&gt;&lt;span&gt;&amp;nbsp;&lt;/span&gt;emissions have historically been ascribed to agricultural activities but these findings illustrate the universal significance of vehicle emissions and the potential for sustained wildfire activity to be a primary contributor to NH&lt;sub&gt;3&lt;/sub&gt;. Air quality (e.g., particulate matter) and nitrogen deposition reduction plans may benefit by including management practices that address vehicle NH&lt;sub&gt;3&lt;/sub&gt;&lt;span&gt;&amp;nbsp;&lt;/span&gt;emissions.&lt;/p&gt;&lt;/div&gt;&lt;/div&gt;&lt;div id="abs0015" class="abstract graphical"&gt;&lt;br&gt;&lt;/div&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1016/j.envpol.2022.120537</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>Elsevier</dc:publisher>
  <dc:title>Nitrogen isotopes indicate vehicle emissions and biomass burning dominate ambient ammonia across Colorado's Front Range urban corridor</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>