Abstract
Finite element formulations based on the Galerkin and variational principles have been developed for the self‐adjoint and non‐self‐adjoint problems represented respectively by the flow and convective‐dispersion equations in the cylindrical polar system of co‐ordinates. The formulation based on the variational principle is shown to be restricted to dispersion‐dominant transports only. The Galerkin method is demonstrated to be more versatile and free from convergence and stability problems. The computational scheme based on the Galerkin principle is shown to be equally valid for both convection and dispersion dominant transports. The numerical results obtained are verified with known analytical solutions. It is concluded that the suggested scheme can be used in solving a variety of field problems involving groundwater dispersion.

This publication has 4 references indexed in Scilit: