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C i ecure https://w learn blackboard.com webapps backboard/execute content file/cmd=view&content; id= 30/34121&course; id= 104//0 1 If this Item does not open automatically you can open HW#4: Darcy's Law-Flow Through Porous Media: Due October 9 here 201740-GEO-308-001 Course Home Page My Alerts My Gracs Tool Panel H Microsoft PowerPoint GE0306 HW416 [Compatibility Mode] 4. Use Darcy's Law to determine K (hydraulic conductivty () specific discharge and the average linear pore velocity ( Ifacontaminant was moving through this system how fast would it be traveling? legrty Classes The following information is known about an aquifer: Effective porosity Average thickness: 50 m Width (perpendicular to direction of flow): 2,200 m Flow Rate from Well B (Q): 20 m/s Area: Wx thickness 0.28 Q-20 m3Vs h = 170 m h=80 m Aquiclude (Granite) 5. An aquifer has three different formations each of which is isotropic and Type here to search 226 PM 1019/17

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Darcy's law is an equation that describes the flow of a fluid through a porous medium. The law was formulated by Henry Darcy based on the results of experiments on the flow of water through beds of sand, forming the basis of hydrogeology, a branch of earth sciences.

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