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...


Q2: A (50 cm) well fully penetrates an unconfined aquifer of saturated depth 80 m. When a<br>discharge of (50 m3/min) was being pumped for a long time, observed wells at radial<br>distances of 100 and 300 m indicated drawdown of 1 and 0.5 m respectively. Estimate the<br>coefficient of permeability (K) and transmissibility (T) of the aquifer, drawdown at the<br>pumping well and the slop of water table?<br>

Extracted 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?

Jun 11, 2022
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