Radial well aquifer benchmark (Water Module): Difference between revisions
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===Formulas=== | ===Formulas=== | ||
<math>\phi(r) - \phi_0 = \frac {Q_0}{2\pi\cdot kD} \ln{\left ( \frac{r}{R} \right )}</math> | <math>\phi(r) - \phi_0 = \frac {Q_0}{2\pi\cdot kD} \ln{\left ( \frac{r}{R} \right )}</math> | ||
where: | |||
: <math>phi(0)</math>: stable water level at the considered edge | |||
: <math>phi(r)</math>: water level between the considered edge and the well | |||
: <math>phi(rw)</math>: water level in the well |
Revision as of 17:03, 15 December 2020
This testcase demonstrates a situation where a pipe drainage is located below ground and is pumping up ground water. A characteristic water water level curve will form over time. File:Drainage freatic benchmark.png
Formulas
where:
- : stable water level at the considered edge
- : water level between the considered edge and the well
- : water level in the well