Self-similar solutions for displacement of non-Newtonian fluids through porous media

1991 ◽  
Vol 6 (1) ◽  
pp. 13-33 ◽  
Author(s):  
Zhongxiang Chen ◽  
Ciqun Liu
1998 ◽  
Vol 22 (3) ◽  
pp. 285-297 ◽  
Author(s):  
C.J van Duijn ◽  
L.A Peletier ◽  
R.J Schotting

2019 ◽  
Vol 26 (1/2) ◽  
pp. 167-178 ◽  
Author(s):  
Dongming Wei ◽  
Samer Al-Ashhab

The reduced problem of the Navier–Stokes and the continuity equations, in two-dimensional Cartesian coordinates with Eulerian description, for incompressible non-Newtonian fluids, is considered. The Ladyzhenskaya model, with a non-linear velocity dependent stress tensor is adopted, and leads to the governing equation of interest. The reduction is based on a self-similar transformation as demonstrated in existing literature, for two spatial variables and one time variable, resulting in an ODE defined on a semi-infinite domain. In our search for classical solutions, existence and uniqueness will be determined depending on the signs of two parameters with physical interpretation in the equation. Illustrations are included to highlight some of the main results.


1990 ◽  
Vol 68 (12) ◽  
pp. 1456-1463 ◽  
Author(s):  
H. Pascal

The question of the rheological effects of non-Newtonian fluids on the natural convection mechanism in a porous medium is addressed. These effects are illustrated for a power-law fluid with a yield stress, in which the yield stress is temperature dependent. The case of a constant-temperature boundary along a heated vertical plate embedded in a porous medium is investigated. For this case the approximate self-similar solutions in closed form of steady and transient states are presented and discussed. The rheological effects on the convection pattern are shown.


2016 ◽  
Vol 11 (2) ◽  
pp. 226-232
Author(s):  
U.R. Ilyasov

The problem of heating of liquid saturated thermo-poroelastic media, without taking into account the phase transitions are solved. Self-similar solutions describing the pressure field, temperature and stress of the porous skeleton are obtained. The dependence of the thermal impact on the parameters of the external action and properties of the medium is studied. It is shown that near of the heating boundary of a porous media, skeleton are tested both compressive and tensile stress. It was found that the main factor affecting the value of the stress-strain state is the thermal expansion of porous media.


2012 ◽  
Vol 699 ◽  
pp. 94-114 ◽  
Author(s):  
Ilenia Battiato

AbstractIn this paper we derive self-similar solutions of flows through both a porous medium and a pure fluid. Self-similar filtration velocity and hydrodynamic shear profiles are obtained by means of asymptotic analysis in the limit of infinitely small permeability, and for both laminar and turbulent regimes over the porous medium. We show that a spatial length scale, related to the porous layer thickness, naturally emerges from the limiting process and suggests a more formal definition of thick and thin porous media. We finally specialize the analysis to porous media constituted of patterned cylindrical obstacles, which can freely deflect under the aerodynamic shear exerted by the fluid flowing through and over the forest. A self-similar solution for the bending profile of the elastic cylindrical obstacles is obtained as intermediate asymptotics, and applied to carbon nanotube (CNT) forests’ response to aerodynamic stresses. This self-similar solution is successfully used to estimate flexural rigidity of CNTs by linear fit of appropriately rescaled maximum deflection and average velocity measurements.


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