Abstract

This paper presents an analytical solution to the problem of unsteady free flow of water from a leaky confined aquifer, fed by an external supply source and draining into a ditch. Both the non-homogeneous governing equation and the boundary conditions are converted to Sturm-Liouville problems. The closed form solution so obtained is significant because it not only illustrates the process of groundwater recharge and depletion, but can constitute a bench-test for numerical models.

Full Text
Published version (Free)

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call