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Benson et al. 2000
Benson, D.A., Wheatcraft, S.W. and Meerschaert, M.M. (2000). The fractional-order governing equation of Lévy motion. Water Resources Research 36: doi: 10.1029/2000WR900032. issn: 0043-1397.

A governing equation of stable random walks is developed in one dimension. This Fokker-Planck equation is similar to, and contains as a subset, the second-order advection dispersion equation (ADE) except that the order (&agr;) of the highest derivative is fractional (e.g. the 1.65th derivative). Fundamental solutions are L¿vy's &agr;-stable densities that resemble the Gaussian except that they spread proportional to time1/&agr;, have heavier tails, and incorporate any degree of skewness. The measured variance of a plume undergoing L¿vy motion would grow faster than Fickian plume, at a rate of time2/&agr;, where 0<&agr;≤2. The equation is parsimonious since the parameters are not functions of time or distance. The scaling behavior of plumes that undergo L¿vy motion is accounted for by the fractional derivatives, which are appropriate measures of fractal functions. In real space the fractional derivatives are integrodifferential operators, so the fractional ADE describes a spatially nonlocal process that is ergodic and has analytic solutions for all time and space. ¿ 2000 American Geophysical Union

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Abstract

Keywords
Hydrology, Groundwater transport, Hydrology, Stochastic processes, Mathematical Geophysics, Modeling, Mathematical Geophysics, Fractals and multifractals
Journal
Water Resources Research
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Publisher
American Geophysical Union
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