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Hydraulic conductivity, velocity, and the order of the fractional dispersion derivative in a highly heterogeneous system (2002)

by M Herrick, D Benson, M Meerschaert, K McCall
Venue:Water Resour. Res
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Finite Difference Approximations for Fractional Advection-Dispersion Flow Equations

by Mark M. Meerschaert, Charles Tadjeran , 2004
"... Fractional advection-dispersion equations are used in groundwater hydrology tomqU- the transport of passive tracers carried by fluid flow in a porous mrousq In this paper we develop practical numtical mumti to solve one dimUEBDqyU fractional advection-dispersion equations with variable coefficients ..."
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Fractional advection-dispersion equations are used in groundwater hydrology tomqU- the transport of passive tracers carried by fluid flow in a porous mrousq In this paper we develop practical numtical mumti to solve one dimUEBDqyU fractional advection-dispersion equations with variable coefficients on a finite domeqV The practical application of these results is illustrated by mqUEIB# a radial flow problem Use of the fractional derivative allows the model equations to capture the early arrival of tracer observed at a field site.

Radial fractionalorder dispersion through fractured rock

by David A. Benson, Charles Tadjeran, Mark M. Meerschaert, Irene Farnham, Greg Pohll - Water Resources Research , 2004
"... [1] A solute transport equation with a fractional-order dispersion term is a model of solute movement in aquifers with very wide distributions of velocity. The equation is typically formulated in Cartesian coordinates with constant coefficients. In situations where wells may act as either sources or ..."
Abstract - Cited by 5 (1 self) - Add to MetaCart
[1] A solute transport equation with a fractional-order dispersion term is a model of solute movement in aquifers with very wide distributions of velocity. The equation is typically formulated in Cartesian coordinates with constant coefficients. In situations where wells may act as either sources or sinks in these models, a radial coordinate system provides a more natural framework for deriving the resulting differential equations and the associated initial and boundary conditions. We provide the fractional radial flow advection-dispersion equation with nonconstant coefficients and develop a stable numerical solution using finite differences. The hallmark of a spatially fractional-order dispersion term is the rapid transport of the leading edge of a plume compared to the classical Fickian model. The numerical solution of the fractional radial transport equation is able to reproduce the early breakthrough of bromide observed in a radial tracer test conducted in a fractured granite aquifer. The early breakthrough of bromide is underpredicted by the classical radial transport model. Another conservative, yet nonnaturally occurring solute (pentaflourobenzoate), also shows early breakthrough but does not conclusively support the bromide model due to poor detection at very low concentrations. The solution method includes, through a procedure called subordination, the effects of solute partitioning on immobile water.

advection–dispersion

by Mark M. Meerschaert, Charles Tadjeran , 2004
"... di$erence approximations for fractional ..."
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di$erence approximations for fractional
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... &ux based on statistical mechanics. The classical model corresponds to a value of 0 = 1. Values of 0¡ 1 lead to superdispersion, in which solute spreads faster than the classical model predicts. See =-=[6,15]-=- for some practical methods of estimating the order 0 of the fractional derivative from data. In the limiting case of 0 = 0, the dispersion process is replaced by an advection process in the di$erenti...

Acknowledgments

by Mark M. Meerschaert, Erkan Nane , 2015
"... Fractional derivatives were invented by Leibniz soon after their integer-order cousins. Recently, they have found practical appli-cations in many areas of science and engineering. Fractional dif-fusion equations replace the integer derivatives in the traditional diffusion equation with their fractio ..."
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Fractional derivatives were invented by Leibniz soon after their integer-order cousins. Recently, they have found practical appli-cations in many areas of science and engineering. Fractional dif-fusion equations replace the integer derivatives in the traditional diffusion equation with their fractional counterparts. These mod-els for anomalous diffusion govern limits of continuous time ran-dom walks, where a random waiting time separates random parti-cle jumps. A power law probability distribution for particle jumps leads to fractional derivatives in space. Power law waiting times correspond to time-fractional derivatives. Particle traces are ran-dom fractals, whose dimension relates to the orders of the frac-tional derivatives. Parameter estimation requires novel statisti-cal techniques, since power law data contains many outliers, and these tail values are the most important feature of the data. Nu-merical methods apply nonlocal variants of standard Euler finite

Article Diffusion in Relatively Homogeneous Sand Columns: A Scale-Dependent or Scale-Independent Process?

by Yong Zhang, Hongxia Xu, Xueyan Lv, Jichun Wu , 2013
"... entropy ..."
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... tail is one of the typical characteristics of super-diffusion), this does not mean that the sand column with a small diameter must constrain super-diffusion. Previous studies, such as Herrick et al. =-=[41]-=- and Kohlbecker et al. [42], showed that the heavy-tailed and long-range-dependent hydraulic conductivity (K) field is needed to generate heavy-tailed solute displacement. In this study, the repacked ...

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by Im Forschungsverbund Berlin E. V, Karl Sabelfeld , 946
"... A stochastic fractal model of the Universe related to the fractional Laplacian ..."
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A stochastic fractal model of the Universe related to the fractional Laplacian
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...l. We mention in conclusion that the stochastic correlation analysis of PDEs with random boundary conditions is used in different fields of science and technology, for instance, flows in porous media =-=[9]-=-, [18], turbulence [5], [10], diffusion and transport [23], [22], elasticity and elastography [13], [19], [20], and many others (e.g., see the bibliography in [7] and [19]). The present paper is the f...

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"... on September 18, ..."
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on September 18,
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...effects cannot be predicted by the conventional mass transport equations. It was demonstrated in a number of publications (e.g. Meerschaert et al. 1999; Benson et al. 2000, 2001; Baeumer et al. 2001; =-=Herrick et al. 2002-=-; Schumer et al. 2003) that fractional differential equations can simulate the anomalous character of solute transport in highly heterogeneous media. Suggesting the inclusion of fractional-in-time der...

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by Sergei A Fomin, Toshiyuki Hashida, Sergei Fomin, Vladimir Chugunov, Toshiyuki Hashida
"... The effect of non-Fickian diffusion into surrounding rocks on contaminant transport in a fractured porous aquifer ..."
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The effect of non-Fickian diffusion into surrounding rocks on contaminant transport in a fractured porous aquifer
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...effects cannot be predicted by the conventional mass transport equations. It was demonstrated in a number of publications (e.g. Meerschaert et al. 1999; Benson et al. 2000, 2001; Baeumer et al. 2001; =-=Herrick et al. 2002-=-; Schumer et al. 2003) that fractional differential equations can simulate the anomalous character of solute transport in highly heterogeneous media. Suggesting the inclusion of fractional-in-time der...

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