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Nonsteady Flow to Surface Reservoir
When ground water flows from an unconfined aquifer to a surface reservoir the position of the water table will change with time. The nonlinear partial differential equation for water table elevation is transformed to a nonlinear ordinary differential equation by similarity substitution and a numerical procedure for its solution is presented. A method of computing bank storage is presented. The solution compares favorably with the experimental results obtained by others.
Nonsteady Flow to Surface Reservoir
When ground water flows from an unconfined aquifer to a surface reservoir the position of the water table will change with time. The nonlinear partial differential equation for water table elevation is transformed to a nonlinear ordinary differential equation by similarity substitution and a numerical procedure for its solution is presented. A method of computing bank storage is presented. The solution compares favorably with the experimental results obtained by others.
Nonsteady Flow to Surface Reservoir
Yeh, William Wen-Gong (author)
Journal of the Hydraulics Division ; 96 ; 609-618
2021-01-01
101970-01-01 pages
Article (Journal)
Electronic Resource
Unknown
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