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By Greg Pohll; Jenny Chapman; Karl Pohlmann; Ahmed Hassan; Jeff Daniels; USDOE Office of Environmental Management (EM) (US); Desert Research Institute, Nevada University, Reno, NV (United States).; University of Nevada System. Desert Research Institute.; Uni

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The differences between including a well and not including one become more pronounced as the hydraulic conductivity and effective porosity decrease. The results suggest that contaminant boundary maps that are produced with the assumption that domestic wells have only a minor influence on radionuclide behavior may need to be modified under certain situations. No-Flow Boundary Source Location Pumping Well Constant Constant Flow Direction No-Flow Boundary Figure A1. Hypothetical groundwater flow and transport components for the two-dimensional flow model.

S. O. Box 98518 Las Vegas, NV 89193-8518 David Stahl Shaw Environmental, Inc. O. Box 93838, M/S 439 Las Vegas, NV 89193-3838 Kenneth A. S. O. S. Geological Survey Water Resources Division 6770 S. Paradise Rd. Las Vegas, NV 89119 Document Section, Library University of Nevada, Las Vegas 4505 Maryland Parkway Las Vegas, NV 89154 53 Library Shaw Environmental, Inc. Bldg. O. Box 93838, M/S 439 Las Vegas, NV 89193-3838 ATTN: Toni Miller, M/S 439 Library Southern Nevada Science Center Desert Research Institute 755 E.

W. Gelhar, 1990. Numerical simulation of solute transport in threedimensional randomly heterogeneous porous media. Water Resour. , 26(10):2541-2562. United States Department of Energy, Nevada Operations Office, 2000. United States Nuclear Tests, July 1945 through September 1992, Las Vegas, NV, DOE/NV-209-REV 15, December 2000, United States Department of Energy, Nevada Operations Office. United States Environmental Protection Agency (EPA), 1976. S. S. Department of Commerce National Technical Information Service, Springfield, VA; NTIS Accession No.

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