A computer program to calculate coupled mass transport and fluid rock inter
actions has been developed. CHEMFRONTS is based on the quasi-stationary sta
te approximation and it uses a kinetic expression to describe mineral disso
lution and precipitation rates. It simulates the chemical evolution of the
mineral and aqueous phases over time along a streamline. For fast kinetics,
local equilibrium conditions are approached. In the aqueous phase, complex
ation and redox reactions are included. Reactions with gas phases such as c
arbonation may also be handled by the program in some special cases. The qu
asi-stationary state approximation makes it possible to solve problems that
would require an extremely large computer effort with conventional models.
Such problems arise when the mass of minerals is large compared to the con
centrations in the water. The program is especially suited to handle sharp
reaction fronts. As the program does not use spatial discretization, the se
paration between closely located fronts can be resolved and the movements o
f the fronts may be computed with high spatial resolution. Sharp fronts are
usual in the ground and typical examples an redox fronts and dissolution a
nd precipitation fronts. The capabilities of the program are shown in the i
nterpretation of two field-scale processes. (C) 1999 Elsevier Science B.V.
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