2014
DOI: 10.1016/j.advwatres.2014.08.005
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Shear dispersion in a fracture with porous walls

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Cited by 70 publications
(27 citation statements)
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“…While our conceptual model relies on a simplification of the actual pore space, it enables us to derive simple analytical formulations for the double‐continuum model parameters. Our approach is also consistent with previous findings showing that this simplified geometry can provide powerful guidance for the interpretation of flow and transport phenomena taking place in complex pore spaces [e.g., Davit et al ., ; Orgogozo et al ., ; Wang et al ., ; Porta et al ., ; Dejam et al ., ; Bianchi Janetti et al ., ]. We now discuss the key developments leading to the definition of our effective transport models.…”
Section: Modeling Approachmentioning
confidence: 99%
“…While our conceptual model relies on a simplification of the actual pore space, it enables us to derive simple analytical formulations for the double‐continuum model parameters. Our approach is also consistent with previous findings showing that this simplified geometry can provide powerful guidance for the interpretation of flow and transport phenomena taking place in complex pore spaces [e.g., Davit et al ., ; Orgogozo et al ., ; Wang et al ., ; Porta et al ., ; Dejam et al ., ; Bianchi Janetti et al ., ]. We now discuss the key developments leading to the definition of our effective transport models.…”
Section: Modeling Approachmentioning
confidence: 99%
“…[9][10][11][12][13]20,24] A detailed review of these assumptions can be found elsewhere. [12,13] By taking into consideration these assumptions and using Equation (2) and making some rearrangements, Equation (7) reduces to the following:…”
Section: Governing Equationmentioning
confidence: 99%
“…Now, we apply three significant assumptions adopted from Taylor [14] and Fischer et al [20] for determination of a dispersion coefficient during dispersive chemical species transport. These assumptions are as follows: the chemical species transport occurs under a quasisteady state condition (@C 0 D =@t D % 0), [9][10][11][12][13][14][20][21][22][23] C 0 D is a slowly varying function, [20] and the longitudinal advection is dominant compared to the longitudinal diffusion (…”
Section: Governing Equationmentioning
confidence: 99%
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