H. Rubin et al., Simulation of contaminant transport in fractured permeable formations by multiporosity modeling, J HYDROL, 223(3-4), 1999, pp. 107-130
This paper concerns contaminant transport in aquifers comprising fractured
porous formations. It is considered that the aquifer subject to contaminati
on is composed of macro-blocks, which embed two sets of macro-fractures, Ea
ch macro-block incorporates numerous micro-blocks of low permeability, whic
h embed micro-fractures. Therefore, the basic conceptual model, used in thi
s study, is a triple-porosity two-dimensional model.
It is shown that five dimensionless parameters govern contaminant transport
in the triple-porosity domain. However, a group of eight so-called practic
al parameters is convenient to be used for consideration of possible scenar
ios. From this group, major effects of contaminant diffusion into the micro
-blocks are attributed to the density of micro-fractures and porosity of th
e microblocks. Coefficient of diffusivity of contaminant into the micro-blo
ck is also a significant parameter. Its effective value increases due to th
e presence of vertical fractures, which do not transfer contaminant by adve
ction, and it is dependent on the tortuosity of the micro-block material.
Simulations of various possible scenarios were carried out by solving the b
asic dimensionless equations developed in the present study. The solutions
were obtained by a combination of analytical and numerical solutions. The s
imulations indicate that at a comparatively high porosity of the micro-bloc
ks, of the order 10(-1), the effect of contaminant diffusion into the micro
blocks can be approximated as a retardation phenomenon, similar to contamin
ant adsorption. An increase of the fracture density reduces that retardatio
n effect. If the micro-block porosity is comparatively low, of the order 10
(-3), then contaminant diffusion into the micro-blocks changes the shape of
the breakthrough curves, which are ended with very long tails. This phenom
enon is reduced by the increase of the fracture density. (C) 1999 Elsevier
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