We present a nonlinear model for Johnson–Segalman type polymeric fluids in porous media, accounting for thermal effects of Oldroyd-B type. We provide a thermodynamic development of the Darcy’s theory, which is consistent with the interlacement between thermal and viscoelastic relaxation effects and diffusion phenomena. The appropriate invariant convected time derivative for the flux vector and the stress tensor is discussed. This is performed by investigating the local balance laws and entropy inequality in the spatial configuration, within the single-fluid approach. For constant parame- ters, our thermomechanical setting is of Jeffreys type with two delay time parameters, and hence, in the linear/linearized version, it is strictly related ...
We study nonlinear stability of steady state solutions of partial differential equations governing t...
<p>This article examines the extensional flow and viscosity and the converging-diverging geometry as...
The stability of the conduction regime of natural convection in a porous vertical slab saturated wit...
We present a nonlinear model for Johnson–Segalman type polymeric fluids in porous media, accounting ...
Dans ce travail de thèse tant théorique que numérique, on étudie les différentes instabilités pouva...
The linear stability of a viscoelastic fluid saturated densely packed horizontal porous layer heated...
A numerical investigation of the viscosity variation effect upon entropy generation in time-dependen...
The present work aims to investigate the influence of different aspects, such as non-standard steady...
The propagation of linear acoustic waves in isotropic media in which mechanical relaxation phenomena...
The stability of mixed convection in a Newtonian fluid medium heated from below and cooled from abov...
AbstractIn this article we present a review of the single-phase flow of non-Newtonian fluids in poro...
In this paper a non linear mathematical model to describe absorption phenomena in polymers is propos...
The linear and weakly nonlinear stability analysis of the quiescent state in a viscoelastic fluid su...
Non-Newtonian fluids are employed in a wide range of industrial applications. Non-Newtonian fluids t...
We investigate nonlinear stability in a model for thermal convection in a saturated porous material ...
We study nonlinear stability of steady state solutions of partial differential equations governing t...
<p>This article examines the extensional flow and viscosity and the converging-diverging geometry as...
The stability of the conduction regime of natural convection in a porous vertical slab saturated wit...
We present a nonlinear model for Johnson–Segalman type polymeric fluids in porous media, accounting ...
Dans ce travail de thèse tant théorique que numérique, on étudie les différentes instabilités pouva...
The linear stability of a viscoelastic fluid saturated densely packed horizontal porous layer heated...
A numerical investigation of the viscosity variation effect upon entropy generation in time-dependen...
The present work aims to investigate the influence of different aspects, such as non-standard steady...
The propagation of linear acoustic waves in isotropic media in which mechanical relaxation phenomena...
The stability of mixed convection in a Newtonian fluid medium heated from below and cooled from abov...
AbstractIn this article we present a review of the single-phase flow of non-Newtonian fluids in poro...
In this paper a non linear mathematical model to describe absorption phenomena in polymers is propos...
The linear and weakly nonlinear stability analysis of the quiescent state in a viscoelastic fluid su...
Non-Newtonian fluids are employed in a wide range of industrial applications. Non-Newtonian fluids t...
We investigate nonlinear stability in a model for thermal convection in a saturated porous material ...
We study nonlinear stability of steady state solutions of partial differential equations governing t...
<p>This article examines the extensional flow and viscosity and the converging-diverging geometry as...
The stability of the conduction regime of natural convection in a porous vertical slab saturated wit...