Solute transport in the subsurface is generally described quantitatively with the convection-dispersion transport equation. Accurate numerical solutions of this equation are important to ensure physically realistic predictions of contaminant transport in a variety of applications. An accurate third-
Mixing cell method for solving the solute transport equation with spatially variable coefficients
✍ Scribed by Guang-Te Wang; V. P. Singh; Shulin Chen
- Publisher
- John Wiley and Sons
- Year
- 1998
- Tongue
- English
- Weight
- 183 KB
- Volume
- 12
- Category
- Article
- ISSN
- 0885-6087
No coin nor oath required. For personal study only.
✦ Synopsis
The advection±dispersion equation with spatially variable coecients does not have an exact analytical solution and is therefore solved numerically. However, solutions obtained with several of the traditional ®nite dierence or ®nite element techniques typically exhibit spurious oscillation or numerical dispersion when advection is dominant. The mixing cell and semi-analytical solution methods proposed in this study avoid such oscillation or numerical dispersion when advection dominates. Both the mixing cell and semi-analytical solution methods calculate the spatial step size by equating numerical dispersion to physical dispersion. Because of the spatial variability of the coecients the spatial step size varies in space. When the time step size Dt 3 0, the mixing cell method reduces to the semi-analytical solution method. The results of application to two cases show that the mixing cell and semi-analytical solution methods are better than a ®nite dierence method used in the study.
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