Two wells are located 100 m apart in a confined aquifer with a transmissivity T = 2 • 10–4 m2/s and storativity S = 7•10–5. One well to the west is pumped at a rate of 6.6 m3/hr and the other to the east at a rate of 10.0 m3/hr. Plot drawdown as a function of distance along the line joining the wells at 1 hr after the pumping starts.
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