Eine Plattform für die Wissenschaft: Bauingenieurwesen, Architektur und Urbanistik
Unsteady Free Surface Ground Water Seepage
Seepage in a two-dimensional unconfined aquifer of rectangular cross-section is analyzed to allow prediction of the fall of the free surface and the rate of outflow into an adjoining water body which fully penetrates the aquifer. Use is made of saturated Darcy flow theory with and without the Dupuit assumptions. It was found that if the length of the aquifer is larger than four times its depth, the Dupuit assumptions can be applied to predict positions of the water table with adequate precision. The present numerical results obtained by the two-dimensional flow model are in agreement with those obtainable experimentally by means of the Hele-Shaw model.
Unsteady Free Surface Ground Water Seepage
Seepage in a two-dimensional unconfined aquifer of rectangular cross-section is analyzed to allow prediction of the fall of the free surface and the rate of outflow into an adjoining water body which fully penetrates the aquifer. Use is made of saturated Darcy flow theory with and without the Dupuit assumptions. It was found that if the length of the aquifer is larger than four times its depth, the Dupuit assumptions can be applied to predict positions of the water table with adequate precision. The present numerical results obtained by the two-dimensional flow model are in agreement with those obtainable experimentally by means of the Hele-Shaw model.
Unsteady Free Surface Ground Water Seepage
Verma, Rameshwar D. (Autor:in) / Brutsaert, Wilfried (Autor:in)
Journal of the Hydraulics Division ; 97 ; 1213-1229
01.01.2021
171971-01-01 pages
Aufsatz (Zeitschrift)
Elektronische Ressource
Unbekannt
Closure to “Unsteady Free Surface Ground Water Seepage”
ASCE | 2021
|Closure to “Unsteady Free Surface Ground Water Seepage”
ASCE | 2021
|Unsteady Seepage toward Sink beneath Free Surface
ASCE | 2021
|Unsteady Seepage toward Narrow Ditch
ASCE | 2021
|