Modelling Fluid Flow in Saturated Porous Media and at Interfaces

2002 ◽  
pp. 1-19 ◽  
Author(s):  
D.A. Nield
Keyword(s):  
Porous Media ◽  
Fluid Flow ◽  
Saturated Porous Media

Effect of fluid flow on freezing and thawing of saturated porous media

1978 ◽  
Vol 364 (1716) ◽  
pp. 45-73 ◽  
Keyword(s):  
Porous Media ◽  
Fluid Flow ◽  
Seepage Flow ◽  
Saturated Porous Media ◽  
Ground Water Flow ◽  
Freezing And Thawing ◽  
Variable Theory ◽  
Complex Variable Theory ◽  
Protection Devices ◽  
Flow Effects

In this paper we obtain an analytical solution that describes the effect of seepage flow on the freezing and thawing of saturated porous media. This solution is obtained by using techniques from complex variable theory. Results are presented to show how fluid flow effects the shape and growth rates of frozen regions embedded in the porous media. The effect of a heat sink is included for both single and multiple frozen regions. Examples are presented to illustrate the effect of this ground water flow on the thawing of arctic permafrost with and without the presence of perma­frost protection devices.

scholarly journals An Enhanced Particle Method for Simulation of Fluid Flow Interactions with Saturated Porous Media

2017 ◽  
Vol 73 (2) ◽  
pp. I_841-I_846 ◽  
Author(s):  
Abbas KHAYYER ◽  
Hitoshi GOTOH ◽  
Yuma SHIMIZU ◽  
Kohji GOTOH ◽  
Songdong SHAO
Keyword(s):  
Porous Media ◽  
Fluid Flow ◽  
Particle Method ◽  
Saturated Porous Media ◽  
Flow Interactions

Interaction between crack tip advancement and fluid flow in fracturing saturated porous media

2017 ◽  
Vol 80 ◽  
pp. 24-37 ◽  
Author(s):  
Toan Duc Cao ◽  
Enrico Milanese ◽  
Ernst W. Remij ◽  
Paolo Rizzato ◽  
Joris J.C. Remmers ◽  
...  
Keyword(s):  
Porous Media ◽  
Fluid Flow ◽  
Crack Tip ◽  
Saturated Porous Media

Temperature and Chemistry Effects in Porous-Media Electrokinetics

1996 ◽  
Vol 463 ◽  
Author(s):  
David B. Pengra ◽  
Po-Zen Wong
Keyword(s):  
Porous Media ◽  
Fluid Flow ◽  
Electric Fields ◽  
Glass Bead ◽  
Pore Surface ◽  
Saturated Porous Media ◽  
Electrokinetic Phenomena ◽  
Sample Group ◽  
Natural Rock ◽  
Brine Chemistry

ABSTRACTElectrokinetic phenomena in brine-saturated porous media, such as electroosmosis (fluid-flow induced by applied electric fields) and streaming current (the complementary process) depend on the density of ions adsorbed on the pore surface and the characteristic thickness of the diffuse space-charge layer λ. These, in turn, depend on brine chemistry, ambient temperature and possibly other parameters. We report on a series of measurements of natural rock and synthetic glass-bead samples: for one sample group, we varied the temperature over 0–50 ° C; for another, we changed the brine cation species. We find that the electrokinetic coefficients depend only weakly on temperature; this is shown to follow from the expected trends in λ, η, and σ. The chemistry dependence follows qualitatively but not quantitatively the predictions of the Debye-Hiickel approximation.

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