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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>Darwin J. Ockerman</dc:contributor>
  <dc:creator>J. Ryan Banta</dc:creator>
  <dc:date>2014</dc:date>
  <dc:description>&lt;p&gt;Suspended sediment in rivers and streams can play an&amp;nbsp;important role in ecological health of rivers and estuaries&amp;nbsp;and consequently is an important issue for water-resource managers. To better understand suspended-sediment loads and transport in a watershed, the U.S. Geological Survey (USGS), in cooperation with the San Antonio River Authority, developed a Hydrological Simulation Program&amp;mdash;FORTRAN model to simulate hydrologic conditions and suspended-sediment loads during&amp;nbsp;2000&amp;ndash;12 for four watersheds, which comprise the overall study area in the San Antonio River Basin (hereinafter referred to as the &amp;ldquo;USGS&amp;ndash;2014 model&amp;rdquo;). The study area consists of approximately 2,150 square miles encompassing parts of Bexar, Guadalupe, Wilson, Karnes, DeWitt, Goliad, Victoria, and Refugio Counties. The USGS&amp;ndash;2014 model was calibrated for hydrology and suspended sediment for 2006&amp;ndash;12. Overall, model-fit statistics and graphic evaluations from the calibration and testing periods provided multiple lines of evidence indicating that the USGS&amp;ndash;2014 model simulations of hydrologic and suspended-sediment conditions were mostly&amp;nbsp;&amp;ldquo;good&amp;rdquo; to &amp;ldquo;very good.&amp;rdquo; Model simulation results indicated that approximately 1,230&amp;nbsp;tons per day of suspended sediment exited the study area and were delivered to the Guadalupe River during 2006&amp;ndash;12, of which approximately 62 percent originated upstream from the study area. Sample data and simulated model results indicate that most of the suspended-sediment load in the study area consisted of silt- and clay-sized particles (less than 0.0625&amp;nbsp;millimeters). The Cibolo Creek watershed was the largest contributor of suspended sediment from the study area. For the entire study area, open/developed land and cropland exhibited the highest simulated soil erosion rates; however, the largest contributions of sediment (by land-cover type) were pasture and forest/rangeland/shrubland, which together composed approximately 80&amp;nbsp;percent of the land cover of the study area and generated about 70 percent of the suspended-sediment load from the study area.&lt;/p&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.3133/sir20145182</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>U.S. Geological Survey</dc:publisher>
  <dc:title>Simulation of hydrologic conditions and suspended-sediment loads in the San Antonio River Basin downstream from San Antonio, Texas, 2000-12</dc:title>
  <dc:type>reports</dc:type>
</oai_dc:dc>