Gt. Wang et al., MIXING CELL METHOD FOR SOLVING THE SOLUTE TRANSPORT-EQUATION WITH SPATIALLY-VARIABLE COEFFICIENTS, Hydrological processes, 12(5), 1998, pp. 781-795
The advection-dispersion equation with spatially variable coefficients
does not have an exact analytical solution and is therefore solved nu
merically. However, solutions obtained with several of the traditional
finite difference or finite element techniques typically exhibit spur
ious oscillation or numerical dispersion when advection is dominant. T
he mixing cell and semi-analytical solution methods proposed in this s
tudy avoid such oscillation or numerical dispersion when advection dom
inates. Both the mixing cell and semi-analytical solution methods calc
ulate the spatial step size by equating numerical dispersion to physic
al dispersion. Because of the spatial variability of the coefficients
the spatial step size varies in space. When the time step size Delta t
--> 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 finite dif
ference method used in the study. (C) 1998 John Wiley & Sons, Ltd.