<?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.L. Locke</dc:contributor>
  <dc:creator>G.M. Russell</dc:creator>
  <dc:date>1997</dc:date>
  <dc:description>Analysis of water collected during August and September 1993  from well PM-2, on Pahute Mesa at\x11the Nevada Test Site, indicated  tritium concentrations of\x1121,000 Bq/L at 610 m below land surface. The  Schooner event (U-20u) was detonated in 1968 approximately 270 meterssoutheast of well PM-2 at a working depth of 108.2 meters. The crater  created by the Schooner event was about 129.8 meters in radius  and\x1163.4 meters in depth. Geologic and hydrologic properties of the stratigraphic units are  summarized from historical data. The soil around the well and water in  the well were analyzed for radionuclides and water in the well was also  analyzed for inorganic constituents and organic (volatile and  semivolatile) substances.  Close agreement between tritium analyses of water from well PM-2, at  different times and at the same depths, confirms the elevated levels of  tritium. The highest tritium values in the borehole were at 610 meters  below land surface-above the shallowest perforations at 765 meters below  land surface. These values were only slightly higher than values found at  greater depth in the well.</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.3133/ofr96599</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>U.S. Geological Survey ;&#13;
Branch of Information Services [distributor],</dc:publisher>
  <dc:title>Summary of data concerning radiological contamination at well PM-2, Nevada Test Site, Nye County, Nevada</dc:title>
  <dc:type>reports</dc:type>
</oai_dc:dc>