Example 5.2 A 30 cm well penetrates 50 m below the static water table. After a long period of pumping at a rate of 1800 lpm, the drawdowns in the wells at 15 and 45 m from the pumped well were 1.7 and 0.8 m, respectively. Determine the transmissibility of the aquifer. What is the drawdown in the pumped well?

Structural Analysis
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ISBN:9781337630931
Author:KASSIMALI, Aslam.
Publisher:KASSIMALI, Aslam.
Chapter2: Loads On Structures
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Example 5.2 A 30 cm well penetrates 50 m below the static water table. After a long period of
pumping at a rate of 1800 lpm, the drawdowns in the wells at 15 and 45 m from the pumped
well were 1.7 and 0.8 m, respectively. Determine the transmissibility of the aquifer. What is
the drawdown in the pumped well?
Transcribed Image Text:Example 5.2 A 30 cm well penetrates 50 m below the static water table. After a long period of pumping at a rate of 1800 lpm, the drawdowns in the wells at 15 and 45 m from the pumped well were 1.7 and 0.8 m, respectively. Determine the transmissibility of the aquifer. What is the drawdown in the pumped well?
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