2009
DOI: 10.1007/s11242-009-9383-4
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Fracture-Flow-Enhanced Matrix Diffusion in Solute Transport Through Fractured Porous Media

Abstract: Over the past few decades, significant progress of assessing chemical transport in fractured rocks has been made in laboratory and field investigations as well as in mathematic modeling. In most of these studies, however, matrix diffusion on fracture-matrix surfaces is considered as a process of molecular diffusion only. Mathematical modeling based on this traditional concept often had problems in explaining or predicting tracer transport in fractured rock. In this article, we propose a new conceptual model of… Show more

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Cited by 33 publications
(13 citation statements)
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“…Effective water‐in‐water diffusivities for flow in cracked rocks have been estimated to be ∼2 × 10 −9 m 2 s −1 (Wu et al, ; Wu et al, ; Rudge et al, ). We use this to obtain a value of D ϕ =1×10 −6 kg·m −1 ·s −1 (here representing the diffusivity multiplied by the fluid density ρ f ), which appears in equation .…”
Section: Resultsmentioning
confidence: 99%
“…Effective water‐in‐water diffusivities for flow in cracked rocks have been estimated to be ∼2 × 10 −9 m 2 s −1 (Wu et al, ; Wu et al, ; Rudge et al, ). We use this to obtain a value of D ϕ =1×10 −6 kg·m −1 ·s −1 (here representing the diffusivity multiplied by the fluid density ρ f ), which appears in equation .…”
Section: Resultsmentioning
confidence: 99%
“…In all benchmarks, a black-box approach is used in the IFMM for constructing the initial low-rank operators in Equation 8. More precisely, interpolation based on Chebyshev polynomials 80 is used (with n Chebyshev nodes in each direction), followed by an additional singular value decomposition to reduce the rank.…”
Section: Numerical Benchmarksmentioning
confidence: 99%
“…Subsurface flows,() erosion,() fuel cells, and filtration systems() are a few examples of physical processes that are governed by low Reynolds number porous media flow. Accurately resolving such flows is essential for modelling transport, mixing,() anomalous diffusion,() breakthrough curves, carbon dioxide sequestration,() uncertainty quantification of pore‐scale simulations,() chemical reactions,() and many other applications. In most of these works, in particular, those that focus on numerics and modelling, the porous medium is assumed to be two dimensional.…”
Section: Introductionmentioning
confidence: 99%
“…is the half-width of the fracture 133 (taken as 1 mm), is the half-width of the rock matrix (50 m), and is the caprock 134 length (100 m). The fracture is assumed to be partially filled with porous material 135 (Wealthall et al, 2001;Wu et al, 2010;Laubach et al, 2010;Liu et al, 2013) and has 136 an initial porosity of 0.60. The porosity of the rock matrix is taken as 0.12.…”
Section: Model Description 108mentioning
confidence: 99%