The fractional‐order governing equation of Lévy Motion
By David A. Benson, S. Wheatcraft, Mark M. Meerschaert. 2000
774 citations recorded by the source corpus.
Subfields: Computational Mechanics, Modeling and Simulation, Ocean Engineering
View Paper: https://www.semanticscholar.org/paper/61ddfb882971908dea79f7e2ce003a5fd7b02232
How researchers see this paper
The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.
In Computational Mechanics
- Mark M. Meerschaert
- Charles Tadjeran
- Boris Baeumer
- Fawang Liu
- John Paul Roop
- Ian L Turner
- Vo Anh
- Hans-Peter Scheffler
In Modeling and Simulation
- Mark M. Meerschaert
- Fawang Liu
- Charles Tadjeran
- Ian L Turner
- Vo Anh
- Pinghui Zhuang
- Hans-Peter Scheffler
- John Paul Roop
In Ocean Engineering
- Mark M. Meerschaert
- Boris Baeumer
- Fawang Liu
- Ian L Turner
- Vo Anh
- Daniel M. Tartakovsky
- M. Dentz
- Charles Tadjeran
Citations in the corpus
- Possible problems of scale dependency in applications of the three‐dimensional fractional advection‐dispersion equation to natural porous media (2002, methodology): “…explanation for the observed scale dependence of the traditional dispersivity is that the resulting dispersion is based on the mechanics of Brownian motion [Benson et al., 2000, 2001], while macroscopic random trajectories in heterogeneous porous media may be better described by Levy motion.”
- Parameter estimation for fractional transport: A particle‐tracking approach (2009, background): “Parameter estimation for fractional transport:”
- A Fourier method for the fractional diffusion equation describing sub-diffusion (2007, methodology): “[8],[9] used a fractional advection-dispersion equation to simulate transport processes with heavy tails and demonstrated the equivalence between these heavy-tailed motions and transport equations that use fractional-order derivatives.”
- Diffusion in Porous Media: Phenomena and Mechanisms (2019, methodology): “CTRW is related to both Levy walk models (Metzler and Klafter 2000; Cushman et al. 2009) and fractional advection–dispersion equations (Benson et al. 2000; Cushman and Ginn 2000) that are characterized by spatiotemporal kernel functions with an asymptotic powerlaw scaling.”
- Modeling non‐Fickian transport in geological formations as a continuous time random walk (2006, background): “[225] In contrast to the temporal FDE a spatial FDE assumes a transition time distribution y(t) with a finite first moment and a transition length distribution p(s) with a diverging second moment.”
- Time and space nonlocalities underlying fractional-derivative models: Distinction and literature review of field applications (2009, methodology): “This similarity might be the motivation behind the application of the space nonlocal model to simulate the retention process (see for example, [12,45,46,74,143]).”