From conservative to reactive transport under diffusion-controlled conditions
Abstract
We assess the possibility to use conservative transport information, such as that contained in
transit time distributions, breakthrough curves and tracer tests, to predict non-linear fluid-rock
interactions in fracture/matrix or mobile/immobile conditions. Reference simulated data are
given by conservative and reactive transport simulations in several diffusive porosity
structures differing by their topological organization. Reactions includes non-linear
kinetically-controlled dissolution and desorption. Effective Multi-Rate Mass Transfer models
(MRMT) are calibrated solely on conservative transport information without pore topology
information and provide concentration distributions on which effective reaction rates are
estimated. Reference simulated reaction rates and effective reaction rates evaluated by
MRMT are compared, as well as characteristic desorption and dissolution times. Although not
exactly equal, these indicators remain very close whatever the porous structure, differing at
most by 0.6% and 10% for desorption and dissolution. At shorter times, this close agreement
arises from the fine characterization of the diffusive porosity close to the mobile zone that
controls fast mobile-diffusive exchanges. At intermediate to larger times, concentration
gradients are strongly reduced by diffusion, and reactivity can be captured by a very limited
number of rates. We conclude that effective models calibrated solely on conservative
transport information like MRMT can accurately estimate monocomponent kinetically-
controlled non-linear fluid-rock interactions. Their relevance might extend to more advanced
biogeochemical reactions because of the close representation of conservative concentration
distributions, even by parsimonious models (e.g., MRMT with 3-5 rates). We propose a methodology to estimate reactive transport from conservative transport in mobile-immobile
conditions.
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