Two fully penetrating wells are dug 1.4 km apart in a confined aquifer. The difference in their piezometric levels is 4.0 m. The aquifer has a hydraulic conductivity of 3.5 m/day and effective porosity of 40%. The time taken for water to move from one well to the other in days is \(\underline{\hspace{2cm}}\).
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Time for water flow in confined aquifers can be approximated using Darcy's law for radial flow.