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<br />88 GROUNDWATER PUMPING TESTS <br /> <br />T = 1.146 X 10'(62)1.0/1.45 T = 4900 gpdlft <br />S = 4.9 X 103(0.01)5.6/[2.693 X 103(20)'] S = 0.00025 <br /> <br />SiI = 3.6 min, <br /> <br />t" = 180 min <br /> <br />W(u,,) = 4.9 X 103(3.6)/[1.146 X 10'(62)) <br />W(Ull) = 2.4827 <br /> <br />un = 4.92 X 10-' <br /> <br />rn = {[4,9 X 103(180)4.92 X 10-']1 <br />[2.693 X 103(2.5 X 1O-')j} If' <br /> <br />r" = 253 ft <br /> <br />Si' = 3.0 ft t12 = 1000 min <br /> <br />W(ud = 4.9 X 103(3)/[1.146 X 10'(62)] W(ud = 2.0689 <br /> <br />\1;, = 7.72 X 10-' <br /> <br />r12 '" {[4.9 X 1()3(1.0 X 103)7.72 X 10-']1 <br />[2.693 X 103(2.5 X 1O-')j} 112 <br /> <br />r12 = 750 ft <br /> <br />..... <br />Ll.. <br />C <br />~ <br />o <br />-0 <br />~ <br />C <br />L <br />Cl <br /> <br />Time-drawdown graphs for the observation wells are pre- <br />sented in Figure 5.3. <br />The average values of aquifer transmissivity and <br />storativity are 4900 gpd/ft and 0.0002, respectively. Based <br />on an average aquifer thickness of 8 ft, the hydraulic con- <br />ductivity is 613 gpdlsq ft. Available data indicate that the <br />aquifer is a t.hin strip of fine sand and some gravel approxi- <br />.mately 600. ft wide which trends northeast to southwest <br />through the pumping test area. Well storage capacity <br />impacts were appreciable until about 11 minutes after <br />pumping started. <br />A pumping test was conducted in Case Study 5.3 in <br />November 1979 using a small-diameter production well <br />located in southwestern Indiana (see Davis and Walton, <br />1982, pp. 841-848). The production well encountered 93 ft <br />of unconsolidated deposits, 207 ft of sandstone, 30 ft of <br />limestone, 126 ft of shale, and 4 ft of coal. The casing with a <br />radius of 0.25 ft extended from land surface 97 ft through <br />the unconsolidated deposits and into bedrock. <br /> <br />1 <br />2 <br />3 <br />5 <br />7 <br />9 <br />11 <br />16 <br /> <br />100.0 <br /> <br />CASE STUDIES 89 <br /> <br />10.0 <br /> <br /> <br />O. I <br /> <br />0.1 I 10 100 <br /> <br />Timg Aftgr Pumping Stortgd <br /> <br />Figure 5.3. Time-drawdown graphs for Case Study 5.2. <br /> <br />The pump in the production well was discharged at a <br />constant rate of9 gpm for a period of 6 hours, and water <br />levels in the production well were measured at frequent <br />intervals. Recovery was also observed for a period of 6 <br />hours. Time-recovery data for the production well are pre- <br />sented in Table 5.3. <br /> <br />Table 5.3. Database for Case Study 5.3 <br /> <br />Time After <br />Pumping <br />Stopped <br />(min) <br /> <br />1.0 <br /> <br />Adjusted <br />ReCovery <br />(ft) <br />5.91 <br />16.36 <br />18.98 <br />33.55 <br />.46.11 <br />57.02 <br />65.23 <br />84.87 <br /> <br />Time After <br />Pumping <br />Stopped <br />(min) <br />23 <br />35 <br />56 <br />79 <br />110 <br />170 <br />240 <br />300 <br /> <br />1000 <br />(Min) <br /> <br />Adjusted <br />Recovery <br />(ft) <br />107.32 <br />126.77 <br />150.01 <br />163.37 <br />179.86 <br />191.02 <br />201.13 <br />203.74 <br />