A numerical experiment on pore size, pore connectivity, water retention, permeability, and solute transport using network models

By H. Vogel. 2000

200 citations recorded by the source corpus.

Subfields: Civil and Structural Engineering, Environmental Engineering, Geophysics

View Paper: https://www.semanticscholar.org/paper/0974e6cad5d937d191faf20030fbc1590cfa0e87

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

1. Kurt Roth
2. Hans-Jörg Vogel
3. Martin J. Blunt
4. Manfred Krafczyk
5. Jonas Tölke
6. V. Schulz
7. P. Valvatne
8. Philippe Renard

In Environmental Engineering

1. Martin J. Blunt
2. Kurt Roth
3. Manfred Krafczyk
4. Jonas Tölke
5. V. Schulz
6. Hans-Jörg Vogel
7. P. Valvatne
8. Steffen Schlüter

In Geophysics

1. Kurt Roth
2. Manfred Krafczyk
3. Jonas Tölke
4. V. Schulz
5. Hans-Jörg Vogel
6. Martin J. Blunt
7. P. Valvatne

Citations in the corpus

• Quantitative morphology and network representation of soil pore structure (2001, unknown): “However, there is no unique solution since the pressure±saturation relation depends on both the pore-size distribution and the pore topology [8].”
• Insights into the Relationships Among Capillary Pressure, Saturation, Interfacial Area and Relative Permeability Using Pore-Network Modeling (2008, unknown): “Vogel (1997, 2000), and Vogel and Roth (1998) used the serial sectioning technique to produce a representative pore-network, and modeled soil relative permeability.”
• Quantifying Soil Structure and Preferential Flow in Intact Soil Using X‐ray Computed Tomography (2008, background): “On the other hand, the pore network, especially pore size distribution and connectivity, is believed to control soil hydraulic properties (Vogel, 2000; Perret et al., 2000; Pierret et al., 2002).”
• Comparison of a Lattice‐Boltzmann Model, a Full‐Morphology Model, and a Pore Network Model for Determining Capillary Pressure–Saturation Relationships (2005, methodology): “To overcome this deficiency (Vogel, 2000), and residual saturations (Sok et al., 2002).a correction factor could be introduced, which could be Hence, a correct representation of the topology is essen-estimated from the detailed structure of the porous tial when using structure models.”
• Predictive pore‐scale modeling of two‐phase flow in mixed wet media (2004, background): “By adjusting the size distributions to match capillary pressure data, fairly good predictions of absolute and relative permeabilities have been reported for unsaturated soils [Fischer and Celia, 1999; Vogel, 2000].”
• Quantification of soil structure based on Minkowski functions (2010, background): “) The Euler number is a well defined characteristics to evaluate the topology of the pore space which has been shown to be critical for hydraulic properties as well as for flow and transport (Vogel, 2000).”