Abstract
In the reported studies of vertical drainage (for example, [1, 2]) a constant infiltration rate acts in the course of an entire year. Since infiltration arises as a result of irrigation or input from atmospheric water, it actually acts in certain seasons of the year and not all year long.
We shall investigate how the motion parameters vary in cases with and without irrigation, and also the question of how well justified is the consideration of the infiltration rate as a function acting throughout the the course of the entire year.
This is a preview of subscription content, log in via an institution to check access.
Similar content being viewed by others
References
S. F. Aver'yanov and V. S. Useako, “Methods of calculating systematic vertical drainage,” in collection: Control of Surface and Underground Water Resources and Their Utilization [in Russian], Izd-vo AN SSSR, 1961.
V. S. Usenko, “Unsteady inflow of ground water to wells with infiltration from the surface of the earth,” Mosk. int. inzh. vodn. khoz-va, Nauchn. zap., 22, 1960.
M. Muskat, Flow of Homogeneous Fluids in Porous Media [Russian translation], Gostoptekhizdat, 1949.
L. S. Leibenzon, Underground Hydro- and Gas dynamics, in collection: L. S. Leibenzon, collected works, vol. 2 [in Russian], Izdvo AN SSSR, 1953.
Author information
Authors and Affiliations
Additional information
In conclusion I wish to thank P. Ya. Kochina for her interest in this investigation.
Rights and permissions
About this article
Cite this article
Begmatov, A. Calculation of systematic vertical. Drainage. Fluid Dyn 1, 109–111 (1966). https://doi.org/10.1007/BF01106891
Issue Date:
DOI: https://doi.org/10.1007/BF01106891