<?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:contributor>G.C. Bent</dc:contributor>
  <dc:contributor>G.E. Hart</dc:contributor>
  <dc:creator>B.F. Goff</dc:creator>
  <dc:date>1992</dc:date>
  <dc:description>A kinematic wave model of overland flow was used to calculate hydraulic roughness coefficients for earth covers and native hillslope surfaces at a waste burial site. Manning's n roughness coefficients were greater on earth cover plots planted to crested wheatgrass (n = 0.076) than on those planted to streambank wheatgrass (n = 0.030). Mound and intermound microtopography strongly influenced overland flow geometry on the bare native hillslope plots resulting in low apparent roughness values (n = 0.013). Time-related changes in hydraulic roughness appeared to be caused by development of a rain-induced crust on exposed soil surfaces that reduced infiltration and increased plot smoothness. -from Authors</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1080/15324989209381327</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>Taylor and Francis</dc:publisher>
  <dc:title>Hydraulic roughness of earth covers at a cold-desert waste burial site</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>