نتایج جستجو برای: darcy low

تعداد نتایج: 1203191  

2011
M. Sankar Youngyong Park Younghae Do

0017-9310/$ see front matter 2010 Elsevier Ltd. A doi:10.1016/j.ijheatmasstransfer.2010.11.043 ⇑ Corresponding author. Tel.: +82 53 950 7951; fax E-mail addresses: [email protected] (M. Sa (Y. Park), [email protected] (J.M. Lopez), yhdo@knu In this paper natural convection flows in a vertical annulus filled with a fluid-saturated porous medium has been investigated when the inner wall is ...

Journal: :transport phenomena in nano and micro scales 2013
g. a. sheikhzadeh s. nazari

steady state natural convection of al2o3-water nanofluid inside a square cavity filled with a porous medium is investigated numerically. the temperatures of the two side walls of the cavity are maintained at th and tc, where tc has been considered as the reference condition. the top and the bottom horizontal walls have been considered to be insulated i.e., non-conducting and impermeable to mass...

2011
S. Sreenadh S. Rajender N. Krishna Y. V. K. Ravi Kumar

This paper is concerned with the study of the peristaltic flow of Herschel – Bulkley fluid in an inclined flexible channel lined with porous material under long wave length and low Reynolds number assumptions. This model may be applicable to describe blood flow in the sense that erythrocytes region and the plasma regions may be described as plug flow and non-plug flow regions. The effect of yie...

Journal: :Water research 2010
Hyunjung N Kim Sharon L Walker Scott A Bradford

The coupled role of solution ionic strength (IS), hydrodynamic force, and pore structure on the transport and retention of viable Cryptosporidium parvum oocyst was investigated via batch, packed-bed column, and micromodel systems. The experiments were conducted over a wide range of IS (0.1-100 mM), at two Darcy velocities (0.2 and 0.5 cm/min), and in two sands (median diameters of 275 and 710 m...

Journal: :Computers & mathematics with applications 2021

The coupled Darcy–Stokes problem is widely used for modeling fluid transport in physical systems consisting of a porous part and free part. In this work we consider preconditioners monolithic solution algorithms the problem, where Darcy primal form. We employ operator preconditioning framework utilize fractional solver at interface between problems to obtain order optimal schemes that are robus...

2014
Timo Koch

Mathematical models of fluid exchange in the microcirculation can help to understand complex processes and may guide treatment of diseases in the future. To this end, a model with reduced computational demand is investigated making it possible to model large networks of vessels in interaction with the surrounding tissue. We derive a reduced model from a spatially resolved model and assess the e...

2011
Osman Anwar Bêg Oluwole Daniel Makinde Joaquin Zueco Swapan Kumar Ghosh

A mathematical model is presented for the steady, axisymmetric, magnetohydrodynamic (MHD) flow of a viscous, Newtonian, incompressible, electrically-conducting liquid in a highly porous regime intercalated between two concentric rotating cylinders in the presence of a radial magnetic field. The porous medium is modeled using a Darcy-Forchheimer drag force approach to simulate the impedance effe...

In this paper, we analyze the thermal radiation and chemical reaction impacts on MHD peristaltic motion of the Eyring-Powell fluid through a porous medium in a channel with compliant walls under slip conditions for velocity, temperature, and concentration. Assumptions of a long wave length and low Reynolds number are considered. The modeled equations are computed by using the perturbation metho...

2014
Mohammed J. Uddin Waqar A. Khan Norsarahaida S. Amin

The unsteady two-dimensional laminar g-Jitter mixed convective boundary layer flow of Cu-water and Al2O3-water nanofluids past a permeable stretching sheet in a Darcian porous is studied by using an implicit finite difference numerical method with quasi-linearization technique. It is assumed that the plate is subjected to velocity and thermal slip boundary conditions. We have considered tempera...

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