2: A (50 cm) well fully penetrates an unconfined aquifer of saturated depth 80 m. When a discharge of (50 m3/min) was being pumped for a long time, observed wells at radial distances of 100 and 300 m indicated drawdown of 1 and 0.5 m respectively. Estimate the coefficient of permeability (K) and transmissibility (T) of the aquifer, drawdown at the pumping well and the slop of water table?
2: A (50 cm) well fully penetrates an unconfined aquifer of saturated depth 80 m. When a discharge of (50 m3/min) was being pumped for a long time, observed wells at radial distances of 100 and 300 m indicated drawdown of 1 and 0.5 m respectively. Estimate the coefficient of permeability (K) and transmissibility (T) of the aquifer, drawdown at the pumping well and the slop of water table?
Chapter2: Loads On Structures
Section: Chapter Questions
Problem 1P
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Transcribed Image Text:Q2: A (50 cm) well fully penetrates an unconfined aquifer of saturated depth 80 m. When a
discharge of (50 m3/min) was being pumped for a long time, observed wells at radial
distances of 100 and 300 m indicated drawdown of 1 and 0.5 m respectively. Estimate the
coefficient of permeability (K) and transmissibility (T) of the aquifer, drawdown at the
pumping well and the slop of water table?
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