2006
DOI: 10.1103/physreve.73.021104
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Space-fractional advection-diffusion and reflective boundary condition

Abstract: Anomalous diffusive transport arises in a large diversity of disordered media. Stochastic formulations in terms of continuous time random walks (CTRWs) with transition probability densities showing space- and/or time-diverging moments were developed to account for anomalous behaviors. A broad class of CTRWs was shown to correspond, on the macroscopic scale, to advection-diffusion equations involving derivatives of noninteger order. In particular, CTRWs with Lévy distribution of jumps and finite mean waiting ti… Show more

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Cited by 69 publications
(51 citation statements)
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“…Metzler, Klafter, 2000b;Metzler, Klafter, 2000a;Krepysheva et al 2006a;Krepysheva et al, 2006b) both for absorbing and reflective boundaries. Yet, to the authors' best knowledge, the analytical approach to subdiffusion through a two-layered medium and its connection with the underlying Monte Carlo microscopic dynamics are new and unexplored subjects.…”
Section: Analytical Formulation Of the Problemmentioning
confidence: 99%
“…Metzler, Klafter, 2000b;Metzler, Klafter, 2000a;Krepysheva et al 2006a;Krepysheva et al, 2006b) both for absorbing and reflective boundaries. Yet, to the authors' best knowledge, the analytical approach to subdiffusion through a two-layered medium and its connection with the underlying Monte Carlo microscopic dynamics are new and unexplored subjects.…”
Section: Analytical Formulation Of the Problemmentioning
confidence: 99%
“…Note that the second form of Eq. (19), in the case that β = φ, generates the known form of non-universal scaling of the hydraulic conductivity derived by Balberg [85]. As can be seen in Figure 9, the time value at the peak of arrival time distribution (t p ) for h= 0, 10, and 15 cm is about 20, 200, and 3000 min, respectively.…”
Section: Prediction Of Arrival Time Distribution At Different Saturatmentioning
confidence: 88%
“…Many alternative frameworks for understanding transport have been proposed, including the Fractional Advection-Dispersion Equation (FADE) [15][16][17][18][19][20][21][22], and the continuous time random walk (CTRW) [10,11,13,14,[23][24][25]. Since the FADE still underestimates solute arrivals at short times [11] and the dispersion coefficient of the FADE can still be scale-dependent [17], its relevance may be chiefly in the field of mathematics rather than to actual solute transport problems.…”
Section: Existing Models For Solute Transport In Porous Mediamentioning
confidence: 99%
“…Besides the unclear exact physical (or intuitive) meaning of a fractional derivative (see, e.g. [25]), there is the problem of the non-locality of fractional derivatives that implies a dependence of the explicit formulation of a fractional differential equation on the chosen boundary conditions, see, for example, Krepysheva et al [16] and Garcia-Garcia et al [3]. Another problem is how to treat sub-and superdiffusion simultaneously, as might be necessary in anisotropic media or in multi-process systems.…”
Section: Introductionmentioning
confidence: 99%