<?xml version='1.0' encoding='utf-8'?>
<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:creator>C.D. Albert</dc:creator>
  <dc:date>1973</dc:date>
  <dc:description>&lt;p&gt;Fluvial-sediment samples have been collected from the Kansas River at Wamego from 1957-70 by the U.S. Geological Survey in cooperation with the Kansas Water Resources Board. During this period. the stream-runoff pattern of the basin has been altered by constructions of Tuttle Creek and Milford Reservoirs.&lt;/p&gt;
&lt;p&gt;An analysis of data shows that the reduction of suspended sediment discharge has been significant as a result of reservoir storage. However. the particle-size distribution of fluvial sediment has not been appreciably altered.&lt;/p&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.3133/ofr732</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>U.S. Geological Survey</dc:publisher>
  <dc:title>Fluvial sediment characteristics of the Kansas River at Wamego, Kansas, 1957-70</dc:title>
  <dc:type>reports</dc:type>
</oai_dc:dc>