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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>Olivia L. Miller</dc:contributor>
  <dc:contributor>Scott Ator</dc:contributor>
  <dc:contributor>Matthew P. Miller</dc:contributor>
  <dc:contributor>Gregory E. Schwarz</dc:contributor>
  <dc:contributor>Dale M. Robertson</dc:contributor>
  <dc:contributor>Andrew J. Sekellick</dc:contributor>
  <dc:contributor>Kenneth D. Skinner</dc:contributor>
  <dc:contributor>David A. Saad</dc:contributor>
  <dc:creator>Noah M. Schmadel</dc:creator>
  <dc:date>2024</dc:date>
  <dc:description>&lt;div id="ab0005" class="abstract author" lang="en"&gt;&lt;div id="as0005"&gt;&lt;div id="sp0035" class="u-margin-s-bottom"&gt;Quantifying nutrient sources in streams, their temporal and spatial variability, and drivers of that variability can support effective water resources management. Yet a lack of data and modeling capabilities has previously prevented comprehensive quantification across both space and time. Here a dynamic SPARROW (Spatially Referenced Regressions on Watershed attributes) model that accounts for a lagged delivery of nutrients to streams was developed and applied to simulate seasonal and source-specific total nitrogen (TN) and total phosphorus (TP) loads in streams across the Illinois River basin (IRB). Dynamic load predictions from 2000 through 2020 revealed that a third of the TN and a quarter of the TP instream load originated from non-point sources that were lagged in their delivery from land-application to streams by more than a season. This lagged mass was the largest overall TN source—which was estimated as a lagged expression of previous seasonal non-point sources including fertilizer, manure, atmospheric deposition and fixation, and urban land use. Treated wastewater effluent was the largest TP source exported from the basin, contributing 39&amp;nbsp;% of the TP load and 15&amp;nbsp;% of the TN load, and dominated the load in the upper Illinois River near Chicago. Loads in the lower river during this period, conversely, were attributed primarily to a mix of agricultural sources and their lagged fractions from headwater tributaries. Instream processes removed 10&amp;nbsp;% of the TN load while only 4&amp;nbsp;% of the TP load was removed during instream transport. With appropriate datasets, the models could be extended to other basins or time periods and used to forecast future seasonal nutrient loads.&lt;/div&gt;&lt;/div&gt;&lt;/div&gt;&lt;div id="ab0010" class="abstract graphical" lang="en"&gt;&lt;br&gt;&lt;/div&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1016/j.scitotenv.2024.176816</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>Elsevier</dc:publisher>
  <dc:title>Seasonally varying contributions of contemporaneous and lagged sources of instream total nitrogen and phosphorus load across the Illinois River basin</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>