A finite element solution of the one‐dimensional diffusion‐convection equation
Author:
- Gary L. GuymonGGGary L. Guymon
- 1 February 1970
- journal article
- Published by American Geophysical Union (AGU) in Water Resources Research
- Vol. 6 (1) , 204-210
Abstract
The one‐dimensional diffusion‐convection equation has been widely used to describe approximately the transient motion of a subset of particles in river flow or porous media flow. An equivalent variational principle to the governing partial differential equations of motion is given, and a finite element solution is developed requiring only approximations in the space domain. The solution is applicable to a wide variety of field problems because it can account for a variety of boundary conditions. Additionally, the solution is not dependent upon constant parameters of motion over the entire domain of interest.Keywords
This publication has 3 references indexed in Scilit:
- A Method of Analyzing Transient Fluid Flow in Multilayered AquifersWater Resources Research, 1969
- Numerical Methods of Higher-Order Accuracy for Diffusion- Convection EquationsSociety of Petroleum Engineers Journal, 1968
- Solution of Anisotropic Seepage by Finite ElementsJournal of the Engineering Mechanics Division, 1966