Momani, Shaher; Odibat, Zaid Numerical solutions of the space-time fractional advection-dispersion equation. (English) Zbl 1148.76044 Numer. Methods Partial Differ. Equations 24, No. 6, 1416-1429 (2008). Summary: Fractional advection-dispersion equations are used in groundwater hydrologhy to model the transport of passive tracers carried by fluid flow in a porous medium. In this paper we present two reliable algorithms, the Adomian decomposition method and variational iteration method, to construct numerical solutions of the space-time fractional advection-dispersion equation in the form of a rabidly convergent series with easily computable components. The fractional derivatives are described in the Caputo sense. Some examples are given. Numerical results show that the two approaches are easy to implement and accurate when applied to space-time fractional advection-dispersion equations. Cited in 31 Documents MSC: 76M25 Other numerical methods (fluid mechanics) (MSC2010) 76M30 Variational methods applied to problems in fluid mechanics 76R99 Diffusion and convection 76S05 Flows in porous media; filtration; seepage 86A05 Hydrology, hydrography, oceanography Keywords:Caputo fractional derivative; variational iteration method; Adomian decomposition method PDF BibTeX XML Cite \textit{S. Momani} and \textit{Z. Odibat}, Numer. Methods Partial Differ. 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