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I <br /> Feasibility Study Report <br /> 1140 W Hammer Lane, Stockton, CA <br /> The testing program consisted of three separate elements designed to provide complimentary <br /> information The first element consisted of static groundwater monitoring to establish initial conditions <br /> and to help in the evaluation of water level changes observed during pumping The second element of <br /> the test program consisted of a step-drawdown test of well MW-4, designed to provide data on well <br /> efficiency and to select an appropriate pumping rate for the longer term tests The third element of the <br /> program consisted of conducting a constant rate pumping test on well MW-4 to estimate aquifer <br /> formation transmissivity by two methods 1) the Jacob time-drawdown method and 2) the relationship <br /> Ibetween specific capacity and transmissivity <br />' Using the test data, RESNA calculated the estimated value of formation transn-ussivity, based on the <br />' pumping test, at approximately 11,300 gpd/ft The log for pumping well MW-4 indicates an aquifer <br /> thickness of approximately 10 feet RESNA calculated the hydraulic conductivity to be approximately <br /> 1,130 gpd/ft2 This value corresponds to the upper to middle range of expected values for sandy <br /> aquifers <br /> RESNA calculated the radius of plume capture for a hypothetical extraction well constructed similar <br /> to the existing monitoring wells using Darcy's law Using the data obtained from the pumping tests <br /> and a natural groundwater gradient of approximately 0 003 ft/ft, the estimated radius of influence <br /> was calculated to be approximately 20 feet RESNA concluded that the radius of influence would <br /> not be acceptable, either in terms of hydraulic control or effective remediation RESNA concluded <br /> that a capture zone radius of approximately 100 feet would be necessary to capture the plume using <br /> a dedicated extraction well with a diameter of 4 to 6 inches optimally located near MW5 (the well <br /> impacted to the greatest extent) The estimated pumping rate required to achieve the capture zone <br /> radius is approximately 21,300 gpd or 15 gpm It is unclear, based upon the pumping test, if the <br /> shallow aquifer beneath the site would yield 15 gpm over an extended period <br /> 1 45 Additional Subsurface Investigation <br /> Pursuant to a request by PHS/EHD, Ground Zero advanced additional soil borings at the site to <br />' investigate the vertical extent of soil contamination in the vicinity of the former USTs and to investigate <br /> .� the lateral extent of groundwater contamination north of the former USTs Ground Zero supervised <br /> G 11h%taV.ROUNDZE1KNOWLES HAMIREMRT51FemN1ityRLpart dog <br />' 5 <br />