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Автор Khan, Muhammad Yunus
Автор Kirkham, Don
Автор Toksöz, Sadik
Дата выпуска 1971
dc.description Theoretical expressions for the hydraulic head and the stream function are derived for three‐dimensional, axisymmetric steady flow around a well in a two‐layered aquifer. The aquifer receives a steady vertical recharge, and the well is pumped at a constant rate; the hydraulic head at the outer cylindrical boundary is kept constant. Two sets of flow nets and a table of values are presented to show the effect of hydraulic conductivities of the two layers on flow lines, equipotentials, and the height of the water table. Graphs showing the effect of the problem variables on the height of the water table are presented.
Формат application.pdf
Копирайт Copyright 1971 by the American Geophysical Union.
Название Steady State Flow around a Well in a Two‐Layered Aquifer
Тип article
DOI 10.1029/WR007i001p00155
Electronic ISSN 1944-7973
Print ISSN 0043-1397
Журнал Water Resources Research
Том 7
Первая страница 155
Последняя страница 165
Выпуск 1
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Библиографическая ссылка Zaslavsky, Dan, DonKirkham, The streamline function for axially symmetric groundwater movement, Soil Sci. Soc. Amer. Proc., 28, 156–160, 1964.

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