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Steady-state solutions. Press "Unsteady-state" button to go to transient solutions for circular aquifer.
"Well in center" tab of "Circular aquifer" dialog box.
Explanatory table for tab "Well in center"
Steady-state equations Recharge boundary (I kind): drawdown in observation well (non-leaky confined aquifer) drawdown in pumping well (non-leaky confined aquifer) drawdown in observation well (leaky aquifer) drawdown in pumping well (leaky aquifer) drawdown in observation well and pumping well (unconfined aquifer) distance from pumping well to point with maximum head (see "r, m" text box):
No-flow boundary (II kind): drawdown in observation well (leaky aquifer) drawdown in pumping well (leaky aquifer)
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"Eccentric well" tab of "Circular aquifer" dialog box.
Explanatory table for tab "Eccentric well"
Steady-state equations Recharge boundary (I kind): drawdown in observation well (non-leaky confined aquifer) drawdown in pumping well (non-leaky confined aquifer) drawdown in observation well (leaky aquifer) drawdown in pumping well (leaky aquifer)
No-flow boundary (II kind): drawdown in observation well (leaky aquifer) drawdown in pumping well (leaky aquifer)
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"Constant-head test" tab of "Circular aquifer" dialog box.
Explanatory table for tab "Constant-head test"
Steady-state equations Recharge boundary (I kind): drawdown in observation well (non-leaky aquifer) pumping rate (non-leaky aquifer) drawdown in observation well (leaky aquifer) pumping rate (leaky aquifer)
No-flow boundary (II kind): drawdown in observation well (leaky aquifer) pumping rate (leaky aquifer)
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"Leaky aquifer" tab of "Circular aquifer" dialog box.
Explanatory table for tab "Leaky aquifer"
Steady-state equations for the recharge boundary (I kind): drawdown in the main aquifer drawdown in the adjacent aquifer
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"Two aquifers" tab of "Circular aquifer" dialog box.
Explanatory table for tab "Two aquifers"
Steady-state equations for the recharge boundary (I kind): drawdown in pumping well Average hydraulic conductivity
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"Two aquifers - 2" tab of "Circular aquifer" dialog box.
Explanatory table for tab "Two aquifers - 2"
Steady-state equation (the adjacent aquifer is present): drawdown in the main aquifer drawdown in aquitard
Steady-state equation (no adjacent aquifer): drawdown in the main aquifer drawdown in aquitard Roots of transcendental equation are calculated in solutions:
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