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Hydraulics of a Partially Penetrating Ditch Drainage System in a Layered Soil Receiving Water from a Ponded Field
Publisher: American Society of Civil Engineers
Abstract: This study deals with the development of an analytical solution for predicting seepage into an array of ditch drains dug in a three-layered soil underlain by an impervious barrier and receiving water from a ponded field ...
Analytical Solutions of Seepage into Ditches from Ponded Fields
Publisher: American Society of Civil Engineers
Abstract: A steady-state theory is developed for the seepage of ponded water into equally spaced drainage ditches in a homogeneous and anisotropic soil overlying an impervious barrier. Solutions are obtained for two general cases ...
Theory of Seepage into an Auger Hole in a Confined Aquifer
Publisher: American Society of Civil Engineers
Abstract: A steady-state theory is presented for predicting flow into an auger hole partially penetrating a homogeneous and anisotropic confined aquifer that is underlain by an impermeable layer. The developed equations can be ...
Ditch Drainage Theories for Homogeneous Anisotropic Soil
Publisher: American Society of Civil Engineers
Abstract: The problem of seepage of steady rainfall or irrigation recharge into a homogeneous and anisotropic soil medium, drained by equally spaced ditch drains overlying a barrier, is solved. Two general cases of the problem are ...
Theory of Seepage into an Auger Hole in a Confined Aquifer Overlying a Gravel Substratum
Publisher: American Society of Civil Engineers
Abstract: An analytical solution is presented to the problem of steady groundwater flow seeping into a pumped cylindrical hole partially penetrating a homogeneous and anisotropic confined aquifer overlying a gravel substratum. ...
Experimental and Analytical Investigation of Ponded Ditch Drainage System with Temporal Boundaries
Publisher: ASCE
Abstract: An analytical solution is proposed for a two-dimensional, fully-penetrating ditch drainage system by considering the boundaries at the ditch face and at the soil surface to change with time. The general assumption of ...