A NEW ALGORITHM FOR REPRESENTING TRANSPORT IN POROUS-MEDIA IN ONE-DIMENSION, INCLUDING CONVECTION, DISPERSION, AND INTERACTION WITH THE IMMOBILE PHASE WITH 1ST-ORDER KINETICS
F. Delay et al., A NEW ALGORITHM FOR REPRESENTING TRANSPORT IN POROUS-MEDIA IN ONE-DIMENSION, INCLUDING CONVECTION, DISPERSION, AND INTERACTION WITH THE IMMOBILE PHASE WITH 1ST-ORDER KINETICS, Mathematical geology, 25(6), 1993, pp. 689-712
The model uses, in one-dimensional flow, the random-walk method on par
ticles and integrates them into a discretized representation of space
which eliminates the individual management of each particle. The metho
d of computing allows a simulation of mass transfer in adsorbing media
by dissociating the roles of convection, dispersion, and the exchange
occurring between the mobile and immobile phases. This gives the para
meters that have to be fitted, such as the dispersivity or the exchang
e rate, a meaning which is closer to their physical reality than that
defined by global models (e.g., apparent dispersivity without consider
ing exchange between phases). The model was tested first on analytical
solutions and also on data from laboratory experiments on a double po
rosity chalk column and showed that, with the same limited set of para
meters, it could fit concentration/time restitutions at different dist
ances from the injection point. Because of its structure, the algorith
m can easily be modified so as to simulate distributed injections and
transfers in a regime of variable flow rates.