Coupling advection-dominated transport to reactive processes leads to addit
ional requirements and limitations for numerical simulation beyond those fo
r non-reactive transport. Particularly, both monotonicity avoiding the occu
rence of negative concentrations, and high-order accuracy suppressing artif
icial diffusion, are necessary to study accurately the reactive interaction
s of compounds transported in groundwater. These requirements are met by no
n-linear Eulerian methods. Two cell-centered Finite Volume schemes are pres
ented for the simulation of advection-dominated reactive transport. The fir
st scheme is based on rectangular grids, whereas the second scheme requires
streamline-oriented grids the generation of which is explained in an accom
panying paper. Although excellent results for conservative transport are ob
tained by the scheme for rectangular grids, some artificial transverse mixi
ng occurs in the case of multi-component transport. This may lead to errone
ous reaction rates if the compounds interact. The transport scheme for stre
amline-oriented grids, on the other hand, avoids artificial transverse mixi
ng. A quantitative comparison is given by two test cases. A conservative tr
acer simulation for a five-spot configuration in a heterogeneous aquifer sh
ows a high coincidence of the breakthrough curves obtained for the two meth
ods, whereas a test case of two reacting compounds shows significant differ
ences. In this test case, a rate of convergence with respect to the overall
reaction rates lower than first-order is calculated for the rectangular gr
id. (C) 1999 Elsevier Science Ltd. All rights reserved.