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- W2021472017 abstract "Steady upward and downward flows are discussed on the basis of a three-parameter empirical relationship between the pressure head and the hydraulic conductivity. For two soils and given fluxes, pressure head profiles are presented. The results show that for a given depth of the water table below the surface, there exists a maximum possible upward flux. It is also shown that there exist two types of downward flows, either one of which may occur in the region above an interface between two different soil layers." @default.
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- W2021472017 date "1973-06-01" @default.
- W2021472017 modified "2023-10-14" @default.
- W2021472017 title "STEADY UPWARD AND DOWNWARD FLOWS IN A CLASS OF UNSATURATED SOILS" @default.
- W2021472017 doi "https://doi.org/10.1097/00010694-197306000-00002" @default.
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