<?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>Timothy J. Durbin</dc:contributor>
  <dc:creator>Freddy E. Arteaga</dc:creator>
  <dc:date>1978</dc:date>
  <dc:description>&lt;p&gt;Eagle Valley is a topographic and ground-water basin in the west-central area of Nevada. The demand for water in the valley is approaching the limits of the locally available resource, which is the water yield of 9,000 acre-feet per year from the adjacent mountain areas.&lt;/p&gt;&lt;p&gt;The steady-state pumping rate from the ground-water basin is defined as the rate that just balances ground-water recharge and discharge. The recharge of water after agricultural or municipal use is a contribution toward overall ground-water recharge and, therefore, to the steady-state pumping rate. However, because the recharge factors are different for municipal and agricultural use, the total quantity of ground-water recharge from the beneficial use of water depends on the type of water use. Consequently, the steady-state pumping rate depends on the type of water use.&lt;/p&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.3133/ofr79261</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>U.S. Geological Survey</dc:publisher>
  <dc:title>Development of a relation for steady-state pumping rate for Eagle Valley ground-water basin, Nevada</dc:title>
  <dc:type>reports</dc:type>
</oai_dc:dc>