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Title: A two-dimensional simulation of tritium transport in the vadose zone at the Nevada Test site

Technical Report ·
DOI:https://doi.org/10.2172/10189131· OSTI ID:10189131

The site of a 0.75-kiloton underground nuclear explosion, the Cambric event, was selected for the study of radionuclide transport in the hydrologic environment. Water samples from RNM-2S, a well located 91 m from Cambric, have been analyzed for tritium and other radionuclides since the initiation of pumping. Water from RNM-2S flows to Frenchman Lake via an unlined canal. Flume data indicate canal transmission losses of approximately 2m{sup 3}/day/meter of canal. To determine if infiltrating canal water might be recirculated by RNM-2S, and therefore provide an additional radionuclide input to water samples collected at RNM-2S, a two-dimensional variably saturated solute transport computer model (SATURN, Huyakorn et al., 1983) was used to simulate the movement of tritium from the canal to the water table. Results indicate that recirculated canal water has not had a significant effect on the breakthrough of tritium at RNM-2S.

Research Organization:
Nevada Univ., Las Vegas, NV (United States). Desert Research Inst.
Sponsoring Organization:
USDOE, Washington, DC (United States)
DOE Contract Number:
AC08-81NV10162
OSTI ID:
10189131
Report Number(s):
DOE/NV/10162-21; ON: DE95001439; BR: 35AR05154/35GB01040
Resource Relation:
Other Information: DN: Publication No. 45098; PBD: Sep 1994
Country of Publication:
United States
Language:
English