Non-local and localized analyses of non-reactive solute transport in bounded randomly heterogeneous porous media : Theoretical framework
By E. Morales-Casique, Shlomo P. Neuman, Alberto Guadagnini. 2006
98 citations recorded by the source corpus.
Subfields: Civil and Structural Engineering, Environmental Engineering, Mechanical Engineering
View Paper: https://www.semanticscholar.org/paper/2686a462f90cabe6148cd7993556f41126c52720
How researchers see this paper
The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.
In Civil and Structural Engineering
- Daniel M. Tartakovsky
- Shlomo P. Neuman
- M. Dentz
- H. Zhan
- Quanzhong Huang
- Yong Zhang
- Donald M. Reeves
- David A. Benson
In Environmental Engineering
- Daniel M. Tartakovsky
- Shlomo P. Neuman
- M. Dentz
- H. Zhan
- Quanzhong Huang
- Ming Ye
- Hoshin V. Gupta
- Yong Zhang
In Mechanical Engineering
Citations in the corpus
- The role of scaling laws in upscaling (2009, unknown): “[23]).”
- Perspective on theories of non-Fickian transport in heterogeneous media (2009, methodology): “It has been demonstrated theoretically [20,15,42,65,94,61, 91,22] and computationally [37,57,56] that even if transport in each random realization is governed by the ADE, the ensemble mean deterministic transport through randomly heterogeneous media is generally non-Fickian.”
- Diffusion in Porous Media: Phenomena and Mechanisms (2019, background): “Nonlocal analogues of (60) for non-Fickian advection–dispersion transport can be found in Fiori et al. (2007), Koch and Brady (1988),Morales-Casique et al. (2006), Neuman (1993), among others.”
- A finite element solution for the fractional advection–dispersion equation (2008, background): “Several attempts have been made to model the anomalous transport, including the mobile–immobile (MIM) model [9,44], the multiple-rate and fractal MIM [39,16], the continuous time random walk (CTRW) [5,4], the non-local stochastic transport theories [30,31], and the fractional advection–dispersion eq”