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Vertical Recharge of Unconfined Aquifer
Linearized, unsteady seepage solutions are obtained for some flows which result when groundwater percolates vertically downward to the water table. Solutions are given for the case when the recharge water is spread uniformly over both a two-dimensional strip of finite width and a circular region of finite radius. Finally, the mathematical solution is compared with experimental results and with a solution obtained from the Dupuit theory.
Vertical Recharge of Unconfined Aquifer
Linearized, unsteady seepage solutions are obtained for some flows which result when groundwater percolates vertically downward to the water table. Solutions are given for the case when the recharge water is spread uniformly over both a two-dimensional strip of finite width and a circular region of finite radius. Finally, the mathematical solution is compared with experimental results and with a solution obtained from the Dupuit theory.
Vertical Recharge of Unconfined Aquifer
Hunt, Bruce W. (author)
Journal of the Hydraulics Division ; 97 ; 1017-1030
2021-01-01
141971-01-01 pages
Article (Journal)
Electronic Resource
Unknown
Discussion by “Vertical Recharge of Unconfined Aquifer”
| ASCE | 2021
Closure to “Vertical Recharge of Unconfined Aquifer”
| ASCE | 2021
Closure to “Vertical Recharge of Unconfined Aquifer”
| ASCE | 2021
Discussion by “Vertical Recharge of Unconfined Aquifer”
| ASCE | 2021