A pore-scale numerical model based on Smoothed Particle Hydrodynamics (SPH) is described for modelling #uid #ow phenomena in porous media. Originally developed for astrophysics applications, SPH is extended to model incompressible #ows of low Reynolds number as encountered in groundwater #ow systems
β¦ LIBER β¦
Scaling of water flow through porous media and soils
β Scribed by K. Roth
- Book ID
- 108718625
- Publisher
- John Wiley and Sons
- Year
- 2007
- Tongue
- English
- Weight
- 191 KB
- Volume
- 59
- Category
- Article
- ISSN
- 1351-0754
No coin nor oath required. For personal study only.
π SIMILAR VOLUMES
A pore-scale numerical model for flow th
β
Zhu, Yi; Fox, Patrick J.; Morris, Joseph P.
π
Article
π
1999
π
John Wiley and Sons
π
English
β 425 KB
π 2 views
Stabilization of flows through porous me
β
Joachim Escher; Zhaoyong Feng
π
Article
π
2007
π
Springer
π
English
β 177 KB
Flow-through drying of porous media
β
Jagannathan Mahadevan; Mukul M. Sharma; Yannis C. Yortsos
π
Article
π
2006
π
American Institute of Chemical Engineers
π
English
β 527 KB
## Abstract The flow of a gas (saturated or dry) through a porous medium, which is partially occupied by a liquid phase, causes evaporation. The latter occurs, even if the inlet gas is fully saturated, as a result of volume expansion. This process, referred to as flowβthrough drying, is important i
Single-phase flow through porous media
β
John C. Slattery
π
Article
π
1969
π
American Institute of Chemical Engineers
π
English
β 653 KB
Two-phase flow through porous media
β
John C. Slattery
π
Article
π
1970
π
American Institute of Chemical Engineers
π
English
β 766 KB
Multiphase viscoelastic flow through por
β
John C. Slattery
π
Article
π
1968
π
American Institute of Chemical Engineers
π
English
β 708 KB