2014
DOI: 10.1016/j.jhydrol.2014.01.008
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Application of tracer injection tests to characterize rock matrix block size distribution and dispersivity in fractured aquifers

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Cited by 18 publications
(4 citation statements)
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“…Although analytical solutions are generally considered to be more rigorous than numerical methods due to providing exact solutions, sometimes these methods might not be able to handle complex problems with specific assumptions. As it mentioned in previous section, three different cases with different boundary condition will be discussed in this study in which only the first case is solved using analytical methods in literature 25 .…”
Section: Resultsmentioning
confidence: 99%
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“…Although analytical solutions are generally considered to be more rigorous than numerical methods due to providing exact solutions, sometimes these methods might not be able to handle complex problems with specific assumptions. As it mentioned in previous section, three different cases with different boundary condition will be discussed in this study in which only the first case is solved using analytical methods in literature 25 .…”
Section: Resultsmentioning
confidence: 99%
“…The analytical solution of a mass transfer equation is solved in base case (Eqs. 29 and 30 ) which is simple case, using the following formula in Laplace (S) domain 25 : In which the and represent the concentration values of higher and lower permeability layers in Laplace domain respectively. The above equations can be solved by introducing the Ai as Airy function.…”
Section: Resultsmentioning
confidence: 99%
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“…For example, measurements of vertical flow velocities in a borehole under ambient and forced hydraulic conditions are used to estimate the properties of individual fractures that intersect the borehole (Klepikova et al, 2013;Paillet et al, 2012;Roubinet et al, 2015), and piezometric data collected in observation boreholes allow one to provide models of fracture network organization (Fischer et al, 2018;Le Goc et al, 2010;Lods et al, 2020). Chemical tracer experiments, typically comprising the interpretation of breakthrough curves, yield information on the short and long paths in the fractured rock; these characterize the discrete fracture network (DFN) and matrix block properties, respectively (Haddad et al, 2014;Roubinet et al, 2013).…”
Section: Introductionmentioning
confidence: 99%