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Автор Khan, Muhammad Yunus
Автор Kirkham, Don
Дата выпуска 1971
dc.description A theory is presented to determine spacing of identical drainage wells that, by discharging groundwater simultaneously from a layered aquifer, will lower a water table to a preassigned level and maintain it. The theory has been developed by solving a mathematical boundary value problem. The wells are located on a certain regular grid, and the aquifer receives a uniform vertical recharge from rainfall or excess irrigation. The theory shows that the spacing depends on the thickness and hydraulic conductivity of each permeable layer tapped by the wells, the maximum allowable drawdown, the uniform vertical recharge, the radius of the wells, and the well grid geometry. A table of values of a function, useful for determining spacing of wells to be tapped in an aquifer that may consist of any number of permeable layers, is given.
Формат application.pdf
Копирайт Copyright 1971 by the American Geophysical Union.
Название Spacing of Drainage Wells in a Layered Aquifer
Тип article
DOI 10.1029/WR007i001p00166
Electronic ISSN 1944-7973
Print ISSN 0043-1397
Журнал Water Resources Research
Том 7
Первая страница 166
Последняя страница 183
Выпуск 1
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Библиографическая ссылка Kirkham, Don, Graphs and formulas for zeros of cross product Bessel functions, J. Math. Phys., 36, 371–377, 1958.
Библиографическая ссылка Kirkham, Don, An upper limit for the height of the water table in drainage design formulas, Trans. Int. Congr. Soil Sci., 7th, 1, 486–492, 1961.
Библиографическая ссылка Kirkham, Don, W. L.Powers, Advanced Soil Physics, John Wiley, New York, 1971.
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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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