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u= well function parameter , determined from tables <br /> of u vs W(u) ( e.g. Freeze and Cherry, 1979, Table <br /> 8 . 1 } <br /> t= time (duration) of pumping ( s ) <br /> S= specific yield (dimensionless ) <br /> At the radius of influence "R" , the value of (ho-h) is , by <br /> definition, very small . To determine "R" , w( u) is first <br />' determined, "K" is used from the Hvorslev Method, (h -h) is <br /> set at 0 . 01 m, and "Q" is set to the rate of water extraction <br /> needed for the bioreactor proposed for use on site ( 3-4 <br /> gallons/hr) . After calculating W(u) , "u" is determined from <br /> �� <br /> tables of W(u) vs u, and the equation is solved for R t <br /> is set at 2 weeks ( for example) , and "S" is estimated from tables <br /> showing ranges of specific yield for sediments of various grain <br /> sizes ( e .g. Fetter, 1988 , Table 4 . 2 ) . <br /> The hydraulic conductivities as calculated, porosities , aquifer <br /> thickness , the contamination levels as described in well logs <br /> and reports of laboratory analyses , and the calculated gradient <br /> will be introduced into the SUTRA software program. <br /> r SUTRA ( Saturated-Unsaturated Transport ) Is a computer program <br /> created by the U.S . Geological Survey in cooperation with the <br /> U . S . Air Force that simulates fluid movement and the transport <br /> of either energy or dissolved substances in a subsurface <br /> environment. The model employs a two-dimensional hybrid <br /> finite-element and integrated finite-difference method to <br />' approximate the governing equations that describe the processes <br /> that are simulated. <br /> SUTRA provides fluid pressures and solute concentrations as <br /> they vary with time, everywhere in the simulated subsurface <br /> system. SUTRA flow simulation may be employed for areal and <br /> cross-sectional modeling of saturated groundwater flow systems, <br /> and for cross-sectional modeling of unsaturated zone flow. <br /> Solute transport simulations using SUTRA may be employed to <br /> model natural of man-induced chemical species transport including <br /> processes of solute sorption, production and decay, and may <br /> r be applied to analyze groundwater contaminant transport problems <br /> and aquifer restoration design. Solute transport simulation <br /> with SUTRA may be used for modeling of variable density leachate <br /> ' movement . <br /> Using SUTRA, a pumping simulation will be developed to predict <br /> ' the time necessary to remediate the site. The final remediation <br /> design will depend upon the results obtained from these <br /> calculations . <br /> ' It is proposed that upon its extraction, groundwater be delivered <br /> to a surface storage tank. This water would then be delivered <br /> II . <br />