Q10. From the pumping of a semiconfined aquifer of thickness 31 m and permeability 22 m/d, it is estimated that the recharge rate from an overlaying unconfined aquifer through an aquitard of thickness 2.5 m, is 55 mm/year. The average piezometric surface in the semiconfined aquifer is 15 m below the water table in the unconfined aquifer. Determine the hydraulic characteristics of the aquitard (semi-confining layer) and the aquifer. If a well drilled in the aquifer in is pumped at the rate of 4,000 m³/day, how many square kilometers of recharge area are required to sustain the flow at the estimated recharge rate?

Structural Analysis
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Author:KASSIMALI, Aslam.
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Q10. From the pumping of a semiconfined aquifer of thickness 31 m and
permeability 22 m/d, it is estimated that the recharge rate from an overlaying
unconfined aquifer through an aquitard of thickness 2.5 m, is 55 mm/year. The
average piezometric surface in the semiconfined aquifer is 15 m below the
water table in the unconfined aquifer. Determine the hydraulic characteristics
of the aquitard (semi-confining layer) and the aquifer. If a well drilled in the
aquifer in is pumped at the rate of 4,000 m³/day, how many square kilometers
of recharge area are required to sustain the flow at the estimated recharge
rate?
Transcribed Image Text:Q10. From the pumping of a semiconfined aquifer of thickness 31 m and permeability 22 m/d, it is estimated that the recharge rate from an overlaying unconfined aquifer through an aquitard of thickness 2.5 m, is 55 mm/year. The average piezometric surface in the semiconfined aquifer is 15 m below the water table in the unconfined aquifer. Determine the hydraulic characteristics of the aquitard (semi-confining layer) and the aquifer. If a well drilled in the aquifer in is pumped at the rate of 4,000 m³/day, how many square kilometers of recharge area are required to sustain the flow at the estimated recharge rate?
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