A well that pumps at a constant rate of 500m^3 per day has achieved equilibrium so that there is no change in the drawdown with time. The well taps a confined aquifer that is 24m thick. An observation well 20 m away has a head of 220m above sea level. Another observation well 40 m away has a head of 230 m above sea level. Compute the value of aquifer transmissivity and hydraulic conduc
A well that pumps at a constant rate of 500m^3 per day has achieved equilibrium so that there is no change in the drawdown with time. The well taps a confined aquifer that is 24m thick. An observation well 20 m away has a head of 220m above sea level. Another observation well 40 m away has a head of 230 m above sea level. Compute the value of aquifer transmissivity and hydraulic conduc
Applications and Investigations in Earth Science (9th Edition)
9th Edition
ISBN:9780134746241
Author:Edward J. Tarbuck, Frederick K. Lutgens, Dennis G. Tasa
Publisher:Edward J. Tarbuck, Frederick K. Lutgens, Dennis G. Tasa
Chapter1: The Study Of Minerals
Section: Chapter Questions
Problem 1LR
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A well that pumps at a constant rate of 500m^3 per day has achieved equilibrium so that there is no change in the drawdown with time. The well taps a confined aquifer that is 24m thick. An observation well 20 m away has a head of 220m above sea level. Another observation well 40 m away has a head of 230 m above sea level. Compute the value of aquifer transmissivity and hydraulic conduc
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