We present the boundary-domain integral method, one of the numerical methods for solving the transport phenomena in porous media. The results for the case of double diffusive natural convection in a porous horizontal layer, which is fully saturated with an incompressible fluid, are obtained. Modified Navier-Stokes equations were used to describe the fluid motion in porous media in the form of conservation laws for mass, momentum, energy and species. Several results for different cases of double diffusive natural convection in a porous horizontal layer are presented and compared with some published studies in which calculations with other numerical methods were performed.

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URN

URN:NBN:SI:DOC-9HO02H9I

COBISSID

13341718

Added

21.05.2020

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Citation

APA:

Jecl, Renata, Kramer Stajnko, Janja, Škerget, Leopold (2009). Double diffusive natural convection in a horizontal porous layer with the boundary domain integral method. Acta geotechnica Slovenica, volume 6, issue 1, str. 4-18. URN:NBN:SI:DOC-9HO02H9I from http://www.dlib.si

MLA:

Jecl, Renata, Kramer Stajnko, Janja, Škerget, Leopold. "Double diffusive natural convection in a horizontal porous layer with the boundary domain integral method." Acta geotechnica Slovenica volume 6. issue 1 (2009) str. 4-18.
<http://www.dlib.si/?URN=URN:NBN:SI:DOC-9HO02H9I>

Acta geotechnica Slovenica
2004-
(Assembly record)

Double diffusive natural convection in a horizontal porous layer with the boundary domain integral methodNaravna konvekcija v poroznem sloju zaradi dvojne difuzije z robno območno integralsko metodo

Double diffusive natural convection in a horizontal porous layer with the boundary domain integral method
Naravna konvekcija v poroznem sloju zaradi dvojne difuzije z robno območno integralsko metodo