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• where: <br />0 =flow (ft3 day-1) <br />K = Hydraulic conductivity (ft day_1) <br />2 <br />A = Cross sectional area of the aquifer perpendicular to the flow direction (ft ) <br />1 = Average hydraulic gradient of the aquifer (ft/ft) <br />The hydraulic conductivities (K) were calculated based on the saturated thicknesses <br />determined from the potentiometric maps (Exhibits 7-2 through 7-4 ). The following <br />assumptions were considered when determining K values for the overburden. Inf lorv (ground <br />water discharge) equals outflow (baseflow stream discharge). The ground water discharge <br />to streamflow occurs primarily in the upper portions of the overburden aquifer. Based on <br />lithol ogy the upper portions of the overburden aquifer have a higher transmissi vi ty than <br />the deeper portions of the aquifer. Consequently, tra nsmissi vity values have been <br />adjusted to account for the difference. <br /> Cross sectional areas for the three aquifers were calculated by multiplying the width of <br /> each unit normal to the flow direction by the mean saturated thickness of each respective <br /> unit (see Exhibits 7-2 through 7-4 ). The average hydraulic grad Tents ~we re determined at <br />• the vicinity of each cross section. <br />K = 3.7 ft/day (Overburden at Cross Section A) <br />K = 5.4 ft/day (Overburden at Cross Section B) <br />K = 5.4 ft/day (Overburden at Cross Section C) <br />K = 0.16 ft/day (Dakota Coal at Cross Section A and B) <br />K = 0.46 ft/day (Underburden) <br />I = .031 ft/ft (Overburden at Cross Section A) <br />I = .0342 ft/ft (Overburden at Cross Section B) <br />I = .043 ft/ft (Overburden at Cross Section C) <br />I = .0297 ft/ft (Dakota Coal at Cross Section A) <br />I = .043 ft/ft (Dakota Coal at Cross Section B) <br />I = .0301 ft/ft (Underburden) <br />A = 133,000 ft2 (Overburden at Cross Section A) <br />A = 253,500 ft2 (Overburden at Cross Section B) <br />• A = 40,000 ft2 (Overburden at Cross Section C) <br />7-15 Revised 04/11/BB <br />