K. Bajracharya et Da. Barry, MIXING CELL MODELS FOR NONLINEAR NONEQUILIBRIUM SINGLE SPECIES ADSORPTION AND TRANSPORT, Water resources research, 29(5), 1993, pp. 1405-1413
The oft-used ''standard'' mixing cell model describing reactive solute
transport is extended to cater for nonequilibrium reactions. For trac
er transport, the standard model is second-order accurate in the space
and time discretization used. However, an error analysis of the stand
ard model reveals that its accuracy is degraded when reactions are inc
luded. An ''improved'' model which maintains second-order accuracy is
developed. The improved mixing cell model is demonstrated to be more a
ccurate than the standard model. The solution obtained from the improv
ed model is found to agree very well with the results of a numerical C
rank-Nicolson solution for various isotherms. The improved mixing cell
predictions are also shown to agree very well with the exact solution
for the two-site adsorption model, where a linear isotherm is conside
red. Application of the improved model was illustrated by simulating t
he experimental data from a laboratory Ca-K exchange experiment in whi
ch a solution containing Ca was passed through a column filled with K-
saturated soil. The model was used in conjunction with the experimenta
lly determined nonlinear adsorption isotherm to predict the experiment
al breakthrough data. By changing the value of kinetic coefficient, it
was demonstrated that the predictions varied markedly. However, the s
imulations suggest that the equilibrium model is more appropriate than
the assumption of nonequilibrium.