共查询到10条相似文献,搜索用时 109 毫秒
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M. K. PARTHA 《应用数学和力学(英文版)》2010,31(5):565-574
In this paper, the natural convection in a non-Darcy porous medium is studied using a temperature-concentration-dependent density relation. The effect of the two parameters responsible for the nonlinear convection is analyzed for different values of the inertial parameter, dispersion parameters, Rayleigh number, Lewis number, Soret number, and Dufour number. In the aiding buoyancy, the tangential velocity increases steeply with an increase in the nonlinear temperature parameter and the nonlinear concentration parameter when the inertial effect is zero. However, when the inertial effect is non-zero, the effect of the nonlinear temperature parameter and the nonlinear concentration parameter on the tangential velocity is marginal. The concentration distribution varies appreciably and spreads in different ranges for different values of the double dispersion parameters, the inertial effect parameter, and also for the parameters which control the nonlinear temperature and the nonlinear concentration. Heat and mass transfer varies extensively with an increase in the nonlinear temperature parameter and the nonlinear concentration parameter depending on Dacry and non-Darcy porous media. The variation in heat and mass transfer when all the effects, i.e., the inertial effect, double dispersion ef- fects, and Soret and Dufour effects, are simultaneously zero and non-zero. The combined effects of the nonlinear temperature parameter, the nonlinear concentration parameter and buoyancy are analyzed. The effect of the nonlinear temperature parameter and the nonlinear concentration parameter and also the cross diffusion effects on heat and mass transfer are observed to be more in Darcy porous media compared with those in non- Darcy porous media. In the opposing buoyancy, the effect of the temperature parameter is to increase the heat and mass transfer rate, whereas that of the concentration parameter is to decrease. 相似文献
3.
Near wellbore flow in high rate gas wells shows the deviation from Darcy??s law that is typical for high Reynolds number flows, and prediction requires an accurate estimate of the non-Darcy coefficient (?? factor). This numerical investigation addresses the issues of predicting non-Darcy coefficients for a realistic porous media. A CT-image of real porous medium (Castlegate Sandstone) was obtained at a resolution of 7.57???m. The segmented image provides a voxel map of pore-grain space that is used as the computational domain for the lattice Boltzmann method (LBM) based flow simulations. Results are obtained for pressure-driven flow in the above-mentioned porous media in all directions at increasing Reynolds number to capture the transition from the Darcy regime as well as quantitatively predict the macroscopic parameters such as absolute permeability and ?? factor (Forchheimer coefficient). Comparison of numerical results against experimental data and other existing correlations is also presented. It is inferred that for a well-resolved realistic porous media images, LBM can be a useful computational tool for predicting macroscopic porous media properties such as permeability and ?? factor. 相似文献
4.
Double-diffusive natural convection in a fluid saturated porous medium has been investigated using the finite element method. A generalised porous medium model is used to study both Darcy and non-Darcy flow regimes in an axisymmetric cavity. Results indicate that the Darcy number should be a separate parameter to understand flow characteristics in non-Darcy regime. The influence of porosity on heat and mass transfer is significant and the transport rates may differ by 25% or more, at higher Darcy and Rayleigh numbers. When compared with the Darcy and other specialised models of Brinkman and Forchheimer, the present generalised model predicts the least heat and mass transfer rates. It is also observed that an increase in radius ratio leads to higher Nusselt and Sherwood numbers along the inner wall. 相似文献
5.
We consider upscaling of non-Darcy flow in heterogeneous porous media. Our approach extends the pressure-based numerical homogenization
procedure for linear Darcy flow, due to Durlofsky, to the nonlinear case. The effective coefficients are not constants but
rather mildly varying functions of prevailing gradients of pressure. The upscaled model approximates the fine grid model accurately
and, in some cases, more accurately than what is expected for Darcy flow; this is due to the non-Darcy effects which suppress
heterogeneity. We provide comparisons of alternative approaches as well as consider several variants of numerical realizations
of the non-Darcy flow model. Numerical results show effectiveness of the upscaling procedure. 相似文献
6.
A detailed numerical study of laminar forced convection in a porous channel which contains a fibrous medium saturated with
a power-law fluid was performed. Hydrodynamic and heat transfer results are presented for a configuration that has uniform
heat flux or uniform temperature heating at the walls. The flow in the porous medium was modeled using the modified Brinkman-Forchheimer-extended
Darcy model for power law fluids in which the non-Darcy effects of inertia and boundary were considered. Parametric studies
were conducted to examine the effects of Darcy number, power law index, inertia parameter and Prandtl number. The results
indicate that when the power law index is decreased, the velocity gradient near the walls increases but these effects are
reduced gradually as the Darcy number decreases until the Darcy regime (Da≤10−6) is reached in which case the effects of power law index become negligible. As the power law index is decreased, the thermal
boundary layer thickness decreases significantly only in the non-Darcy regime. Consequently, as the power law index decreases,
the fully developed Nusselt number increases considerably in the non-Darcy regime whereas in the Darcy regime the change in
Nusselt number is very small. As the Prandtl number increases, the local Nusselt number increases and this effect is more
significant for shear thinning fluids (n<1.0).
Received on 2 March 1998 相似文献
7.
Kirill Tsiberkin 《Transport in Porous Media》2018,125(2):259-269
The study considers the forced boundary-layer flow overlying the Darcy–Brinkman porous medium and gives a quantitative analysis of the nonlinear inertial terms in the Brinkman filtration equation. The inertial terms are shown to be larger than the Darcy’s drag near the porous medium interface. The applicability range of boundary-layer approach is determined. It is suitable in high-permeable media with moderate velocities of an external flow. If it is slow enough, the inertial terms can be omitted in spite of interface effect. On the other hand, fast external flow produces the filtration with large pore-scale Reynolds number; therefore, the Forchheimer’s drag should be taken into account. It is shown the Brinkman term as well as inertial terms have a significant role in boundary-layer formation within the porous medium. 相似文献
8.
A numerical study of mixed convection in a vertical channel filled with a porous medium including the effect of inertial forces
is studied by taking into account the effect of viscous and Darcy dissipations. The flow is modeled using the Brinkman–Forchheimer-extended
Darcy equations. The two boundaries are considered as isothermal–isothermal, isoflux–isothermal and isothermal–isoflux for
the left and right walls of the channel and kept either at equal or at different temperatures. The governing equations are
solved numerically by finite difference method with Southwell–Over–Relaxation technique for extended Darcy model and analytically
using perturbation series method for Darcian model. The velocity and temperature fields are obtained for various porous parameter,
inertia effect, product of Brinkman number and Grashof number and the ratio of Grashof number and Reynolds number for equal
and different wall temperatures. Nusselt number at the walls is also determined for three types of thermal boundary conditions.
The viscous dissipation enhances the flow reversal in the case of downward flow while it counters the flow in the case of
upward flow. The Darcy and inertial drag terms suppress the flow. It is found that analytical and numerical solutions agree
very well for the Darcian model.
An erratum to this article is available at . 相似文献
9.
A Criterion for Non-Darcy Flow in Porous Media 总被引:6,自引:0,他引:6
Non-Darcy behavior is important for describing fluid flow in porous media in situations where high velocity occurs. A criterion
to identify the beginning of non-Darcy flow is needed. Two types of criteria, the Reynolds number and the Forchheimer number,
have been used in the past for identifying the beginning of non-Darcy flow. Because each of these criteria has different versions
of definitions, consistent results cannot be achieved. Based on a review of previous work, the Forchheimer number is revised
and recommended here as a criterion for identifying non-Darcy flow in porous media. Physically, this revised Forchheimer number
has the advantage of clear meaning and wide applicability. It equals the ratio of pressure drop caused by liquid–solid interactions
to that by viscous resistance. It is directly related to the non-Darcy effect. Forchheimer numbers are experimentally determined
for nitrogen flow in Dakota sandstone, Indiana limestone and Berea sandstone at flowrates varying four orders of magnitude.
These results indicate that superficial velocity in the rocks increases non-linearly with the Forchheimer number. The critical
Forchheimer number for non-Darcy flow is expressed in terms of the critical non-Darcy effect. Considering a 10% non-Darcy
effect, the critical Forchheimer number would be 0.11. 相似文献
10.
Non-Darcy Flow of Water Through a Packed Column Test 总被引:2,自引:0,他引:2
As the flow velocity and Reynolds number increase in rockfilled porous media, the flow deviates from Darcy conditions and enters into a new phase known as non-Darcy conditions. Due to a linear relationship between hydraulic gradient and the flow velocity in Darcy formula, the flow can be analyzed with no difficulty. However, as the velocity increases the Darcy law is violated, the flow becomes turbulent, making the analysis more challenging. In this paper a laboratory packed column was built to study high-velocity flow through granular materials and new experimental data have been obtained. The laboratory experiments include application of for six different sizes of rounded aggregates and using different hydraulic gradients to assess the flow behavior. Using new experimental data, the validity of four widely-used head-loss equations were evaluated. The results indicated that the Sidiropoulou et al. (Hydrol Process 21:534–554, 2007) and Ergun’s head-loss equations yield satisfactory results comparing to other available relationships. 相似文献