Field measurement of permeability is performed by pumping ground water with flow rate q at a pumping well and observing ground water table changes at two observation wells. Equations for permeability, k are different depending on confinement conditions. Using nomenclature shown in below two figures, derive equations for permeability, k. A. k for unconfined radial flow B. k for radial flow in confined aquifer Hints: 1) Derive a flow rate equation using Darcy's law, q = kiA. 2) Solve a differential equation and express in terms of k. Pumping well Observation wells KXK KVK q D DUI N. Z₂ Original GWT M₂ h₁ hu Aquiclude A. Field measurement of permeability for unconfined radial flow. ho
ho Pumping well 9 DI h₁ N Observation wells Al M₂ Aquifer Original GWT Tw VA B. Field measurement of permeability for radial flow in confined aquifer. Aquiclude Aquiclude
Field measurement of permeability is performed by pumping ground water with flow rate q at a pumping well and observing
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Field measurement of permeability is performed by pumping ground water with flow rate q at a pumping well and observing
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