The exact solution to a problem of unconfined saturated flow of groundwater in a semi-infinite homogeneous and isotropic permeable medium is presented. The inflow and outflow occurs along an arbitrary number of segments of the phreatic surface. The inflow and outflow rates are constant along each segment but may vary from segment to segment. The solution is determined by conformal mapping techniques applying boundary integrals.
|Original language||English (US)|
|Number of pages||15|
|Journal||Journal of Hydrology|
|State||Published - Dec 1978|