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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>Brian J. Andraski</dc:contributor>
  <dc:contributor>C.A. Cooper</dc:contributor>
  <dc:contributor>S.W. Wheatcraft</dc:contributor>
  <dc:contributor>David A. Stonestrom</dc:contributor>
  <dc:contributor>R. L. Michel</dc:contributor>
  <dc:creator>C.J. Mayers</dc:creator>
  <dc:date>2005</dc:date>
  <dc:description>&lt;p&gt;&lt;span&gt;Understanding transport of tritium (&lt;/span&gt;&lt;sup&gt;3&lt;/sup&gt;&lt;span&gt;H) in unsaturated zones is critical to evaluating options for waste isolation. Tritium typically is a large component of low-level radioactive waste (LLRW). Studies at the U.S. Geological Survey's Amargosa Desert Research Site (ADRS) in Nevada investigate &lt;/span&gt;&lt;sup&gt;3&lt;/sup&gt;&lt;span&gt;H transport from a closed LLRW facility. Two boreholes are 100 and 160 m from the nearest waste trench and extend to the water table at 110 m. Soil-water vapor samples from the deep boreholes show elevated levels of &lt;/span&gt;&lt;sup&gt;3&lt;/sup&gt;&lt;span&gt;H at all depths. The objectives of this study were to (i) test source thermal and gas-advection mechanisms driving &lt;/span&gt;&lt;sup&gt;3&lt;/sup&gt;&lt;span&gt;H transport and (ii) evaluate model sensitivity to these mechanisms and to selected physical and hydraulic properties including porosity, tortuosity, and anisotropy. A two-dimensional numerical model incorporated a non-isothermal, heterogeneous domain of the unsaturated zone and instantaneous isotopic equilibrium. The TOUGH2 code was used; however, it required modification to account for temperature dependence of both the Henry's law equilibrium constant and isotopic fractionation with respect to tritiated water. Increases in source temperature, pressure, and porosity enhanced &lt;/span&gt;&lt;sup&gt;3&lt;/sup&gt;&lt;span&gt;H migration, but failed to match measured &lt;/span&gt;&lt;sup&gt;3&lt;/sup&gt;&lt;span&gt;H distributions. All anisotropic simulations with a source pressure component resembled, in shape, the upper portion of the &lt;/span&gt;&lt;sup&gt;3&lt;/sup&gt;&lt;span&gt;H distribution of the nearest borehole. Isotopic equilibrium limited migration of &lt;/span&gt;&lt;sup&gt;3&lt;/sup&gt;&lt;span&gt;H, while effects of radioactive decay were negligible. A 500 Pa pressure increase above ambient pressure in conjunction with a high degree of anisotropy (1:100) was necessary for simulated &lt;/span&gt;&lt;sup&gt;3&lt;/sup&gt;&lt;span&gt;H transport to reach the nearest borehole.&lt;/span&gt;&lt;/p&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.2136/vzj2004.0179</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>Soil Science Society of America</dc:publisher>
  <dc:title>Modeling tritium transport through a deep unsaturated zone in an arid environment</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>