1984
DOI: 10.1111/j.1745-6584.1984.tb01403.x
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Matrix Diffusion Effects on Contaminant Migration from an Injection Well in Fractured Sandstone

Abstract: Deep‐well injection into fractured sandstone is an option for the disposal of contaminated mine dewatering discharge from an open pit uranium mine. As part of the assessment of potential contaminant migration from deep‐well injection, the effect of matrix diffusion was evaluated. An analytical mathematical model was developed for the simulation of the radial movement of a contaminant front away from an injection point under steady flow conditions in a planar fracture with uniform properties. The model includes… Show more

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Cited by 51 publications
(16 citation statements)
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“…There are several mathematical definitions of R a in the literature (Lever et al 1983;Feenstra et al 1984;Maloszewski and Zuber 1993) of which Equation 4 is consistent with the formulation of Equation 3 (e.g., Younger 1990, developed from expressions given by Lever et al 1983):…”
Section: Model Developmentmentioning
confidence: 98%
“…There are several mathematical definitions of R a in the literature (Lever et al 1983;Feenstra et al 1984;Maloszewski and Zuber 1993) of which Equation 4 is consistent with the formulation of Equation 3 (e.g., Younger 1990, developed from expressions given by Lever et al 1983):…”
Section: Model Developmentmentioning
confidence: 98%
“…However, either of these tests would yield the apparent diffusion coefficient by describing the concentration development in the reservoir with an appropriate solution of Fick's 2nd law (Crank, 1975). In throughdiffusion experiments (Feenstra et al, 1984), the diffusive flux is observed between a reservoir cell with high concentration across a porous rock sample and a receiving cell with an initial concentration of zero. The analytical solution of Fick's 2nd law for through-diffusion experiments, outlined below, yields the effective diffusion coefficient and the capacity factor of the rock sample, and hence also the apparent diffusion coefficient (using Equation 7).…”
Section: Determination Of the Diffusion Coefficientmentioning
confidence: 99%
“…In modeling diffusion of strontium and plutonium in fractured granite, Krishnamoorthy et al (1992) chose a range of values from 4.8 x 10 -7 to 1.9 x 10 -6 cm 2 /s (5.2 x 10 -10 to 2.1 x 10 -9 ft 2 /s). Feenstra et al (1984) measured diffusion through intact sandstone cores and obtained a range of values from 3.4 x 10 -8 to 3.2 x 10 -7 cm 2 /s (3.7 x 10 -11 to 3.4 x 10 -10 ft 2 /s) with a mean of 1.5 x 10-7 cm 2 /s (1.6 x 10 -10 ft 2 /s). In mudstone, Barone et al (1992) measured a diffusion coefficient of 1.5 x 10 -6 to 2.0 x 10 -6 cm 2 /s (1.6 x 10 -9 to 2.2 x 10 -9 ft 2 /s).…”
Section: Matrix Diffusionmentioning
confidence: 99%