Sustainable Energy
2nd Edition
ISBN: 9781337551663
Author: DUNLAP, Richard A.
Publisher: Cengage,
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The steady state recharge rate from Problem 2 is q = -0.66 meters/day
An excavation is proposed for a square area near the bend of a river, as shown in Fig 5. It is expected that the flow of water into the excavation will come through the silt layer. Pumping tests reveal an average horizontalhydraulic conductivity of 2 x 10-5 cm/s in the silt layer. The excavation has to be kept dry. Determine the flow (qi) into the excavation in m3/day.
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3. In a pipeline with converging diameter, will the gradient of the total energy line be steeper or milder than the gradient of the piezometric head line? Why?
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