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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>Robert G. Striegl</dc:contributor>
  <dc:contributor>Richard W. Healy</dc:contributor>
  <dc:contributor>Robert L. Michel</dc:contributor>
  <dc:contributor>Herbert Haas</dc:contributor>
  <dc:contributor>David W. Morganwalp</dc:contributor>
  <dc:contributor>Herbert T. Buxton</dc:contributor>
  <dc:creator>David E. Prudic</dc:creator>
  <dc:date>1999</dc:date>
  <dc:description>&lt;div&gt;&lt;p&gt;Tritium concentrations have been determined yearly since April 1994 from water-vapor samples collected at test hole UZB-2. The hole was drilled about 100 m (meters) south of the southwest corner of a commercial burial site for low-level radioactive wastes in September 1993. UZB-2 is equipped with ten 2.5-cm (centimeters) diameter air ports permanently installed in the unsaturated zone between the depths of 5.5 and 108.8 m below land surface. Depth to ground water is about 110 m. Additional sampling ports were driven by hand to depths of 0.5, 1.0 and 1.5 m in May 1997. Initial samples of water vapor collected in April 1994 showed elevated tritium concentrations of more than 100 TU (tritium units) from all 10 air ports, with a maximum concentration of 762±10 TU from an air port at a depth of 24.1 m. Subsequent tritium concentrations increased in all air ports, although tritium concentrations at depths of less than 34.1 m have remained relatively constant since July 1995. The largest observed increase in tritium has been at a depth of 47.9 m. There, tritium concentration has increased from 198±5 TU in April 1994 to 2,570±30 TU in June 1998. Large increases also have been measured in samples collected from air ports at depths of 106.4 and 108.8 m, just above the water table.&lt;/p&gt;&lt;p&gt;During September and October 1998, carbon dioxide samples were collected from all ten air ports in UZB-2 and at a depth of 1.5 m, and analyzed for radioactive carbon-14 (&lt;sup&gt;14&lt;/sup&gt;C).&lt;span&gt;&amp;nbsp;&lt;/span&gt;&lt;sup&gt;14&lt;/sup&gt;C concentrations are highest in air ports at depths less than 6 m where they exceed 2,000 pmc (percent modern carbon). Concentrations decrease rapidly in air ports at depth and are about 20 pmc below 94.2 m. However, at 47.9 meters, the&lt;span&gt;&amp;nbsp;&lt;/span&gt;&lt;sup&gt;14&lt;/sup&gt;C concentration is 205±1 pmc, which is 2 to 4 times higher than concentrations in air ports immediately above and below. This depth corresponds to the largest tritium increase in UZB-2. Concentrations of both tritium and&lt;span&gt;&amp;nbsp;&lt;/span&gt;&lt;sup&gt;14&lt;/sup&gt;C are greater than what could be expected from atmospheric fallout. The distribution of tritium and&lt;span&gt;&amp;nbsp;&lt;/span&gt;&lt;sup&gt;14&lt;/sup&gt;C likely represent a complex pattern of lateral and vertical transport through the unsaturated zone from buried wastes to UZB-2.&lt;/p&gt;&lt;/div&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:language>en</dc:language>
  <dc:publisher>U.S. Geological Survey</dc:publisher>
  <dc:title>Tritium and 14C concentrations in unsaturated-zone gases at test hole UZB-2, Amargosa Desert Research Site, 1994-98: A section in U.S. Geological Survey Toxic Substances Hydrology Program: Proceedings of the technical meeting, Charleston, South Carolina, March 8-12, 1999: Volume 3 (Part C) (WRI 99-4018C)&gt;</dc:title>
  <dc:type>reports</dc:type>
</oai_dc:dc>