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標(biāo)題: Titlebook: Emerging Technologies and Techniques in Porous Media; Derek B. Ingham,Adrian Bejan,Ioan Pop Conference proceedings 2004 Springer Science+B [打印本頁(yè)]

作者: 斷頭臺(tái)    時(shí)間: 2025-3-21 19:51
書目名稱Emerging Technologies and Techniques in Porous Media影響因子(影響力)




書目名稱Emerging Technologies and Techniques in Porous Media影響因子(影響力)學(xué)科排名




書目名稱Emerging Technologies and Techniques in Porous Media網(wǎng)絡(luò)公開(kāi)度




書目名稱Emerging Technologies and Techniques in Porous Media網(wǎng)絡(luò)公開(kāi)度學(xué)科排名




書目名稱Emerging Technologies and Techniques in Porous Media被引頻次




書目名稱Emerging Technologies and Techniques in Porous Media被引頻次學(xué)科排名




書目名稱Emerging Technologies and Techniques in Porous Media年度引用




書目名稱Emerging Technologies and Techniques in Porous Media年度引用學(xué)科排名




書目名稱Emerging Technologies and Techniques in Porous Media讀者反饋




書目名稱Emerging Technologies and Techniques in Porous Media讀者反饋學(xué)科排名





作者: 讓你明白    時(shí)間: 2025-3-21 23:26

作者: palette    時(shí)間: 2025-3-22 03:48
Modeling the Flow Through Porous Media,c levels are described by taking mean values of the microscopic quantities and there are several methods of doing this. In this chapter we are interested in the homogenization method. In fact a more descriptive name for this method is .. This means that the method consists of taking the mean value f
作者: 壁畫    時(shí)間: 2025-3-22 05:23
Techniques for Solving the Boundary-Layer Equations,nsity, can only be found for bodies with very simple geometries. It is also possible to find solutions when the Reynolds number is very small (Stokes flow), but the flow of an almost inviscid fluid, e.g. air, past a body requires us to develop the theory of boundary layers. These flows are of great
作者: 吹氣    時(shí)間: 2025-3-22 09:35

作者: companion    時(shí)間: 2025-3-22 13:40
Compressible Fluid Dynamics in Porous Media by the Boundary Element Method,taining the solutions of some transport phenomena in porous media, e.g. the finite-difference method (FDM), finite element method (FEM), finite volume method (FVM), as well as the boundary element method (BEM). The main comparative advantage of the BEM, the application of which requires the given pa
作者: companion    時(shí)間: 2025-3-22 17:08
Laplacian Decomposition of Steady Free Convection in Porous Media,l technique based on a Laplacian decomposition. This results in the need to solve three Laplace’s equations for the temperature and two other auxiliary harmonic functions which arise from the ideas of Goursat decomposition, whilst using a finite difference approach requires the evaluation of the gra
作者: 悅耳    時(shí)間: 2025-3-23 01:00
Genetic Algorithms and their Application to the Identification of Hydraulic Properties of Rocks,hly nonlinear or non-monotonie, may have a very complex form or its analytical expression may be unknown. Traditional, gradient based, optimisation algorithms are likely to fail for objective functions that exhibit multiple local optima and for such a gradient based algorithms in practice it is ofte
作者: modish    時(shí)間: 2025-3-23 04:48
The Mixed Convection Number for Porous Media Flow,id above lower density fluid. Where a density gradient is present, buoyancy may initiate an additional velocity component upward or downward, i.e. in direction of gravity. It depends on three system properties if the buoyancy impetus changes the flow field in the system. When there is a strong diffu
作者: Paraplegia    時(shí)間: 2025-3-23 07:33

作者: Heretical    時(shí)間: 2025-3-23 11:40
Active Control of the Onset of Convection in Porous Medium by Mechanical Vibration,weakly nonlinear stability analyses have been developed by Gresho and Sani [.], Clever . [.] and by the Russian workers Gershuni and Lyubimov [.]. As shown by these studies, the Rayleigh number for the onset of synchronous convection increases with the frequency of vibration for a layer oscillating
作者: Blemish    時(shí)間: 2025-3-23 16:50

作者: 敏捷    時(shí)間: 2025-3-23 19:30

作者: 發(fā)酵劑    時(shí)間: 2025-3-24 01:12
Nonlinear Vortex Instabilities in Free Convective Boundary Layers in Porous Media,n becomes valid only at sufficiently large distances from the leading edge. If the heated surface is upward-facing, then instability of the flow takes the form of longitudinal vortices, and these form at a critical distance from the leading edge which is dependent on the inclination of the surface a
作者: 消息靈通    時(shí)間: 2025-3-24 02:25
Thermal Non-Equilibrium Free Convection in a Cavity Filled With a Non-Darcy Porous Medium,olid structure are assumed to be in local thermal equilibrium. This assumption is satisfactory for small-pore media such as geothermal reservoirs and fibrous insulations and small temperature differences between phases. In the second kind of approach, the fluid and solid structure are assumed to be
作者: 做事過(guò)頭    時(shí)間: 2025-3-24 08:15
Entropy Generation for Free and Forced Convection in a Porous Cavity and a Porous Channel,The theories of reversibility and irreversibility are important in thermodynamics and crucial to the exergy method. Understanding the nature of irreversibility and how to minimise them in practice is essential for an engineering thermodynamicist. Contemporary engineering thermodynamics uses the rate
作者: 生命    時(shí)間: 2025-3-24 13:04
Natural Convection in Anisotropic Heterogeneous Porous Medium,This phenomena, occurs through porous media in many systems and in nature, including the disposal of waste material, groundwater contamination, chemical transport in packed-bed reactors, food processing, etc. Double-diffusion may exhibit unsteadiness and complex flows patterns, bifurcations, etc., s
作者: 柱廊    時(shí)間: 2025-3-24 17:50

作者: 初次登臺(tái)    時(shí)間: 2025-3-24 20:03

作者: 違反    時(shí)間: 2025-3-25 01:50
Sergio Elaskar,Ezequiel del Ríobout 4°C. Since in many parts of the world, groundwater will be near this temperature for at least part of the year, it is important to examine the effects of the density maximum on convection in porous media.
作者: 大方不好    時(shí)間: 2025-3-25 06:53

作者: CURB    時(shí)間: 2025-3-25 09:46
Sidewall Heating in Shallow Cavities Near the Density Maximum,bout 4°C. Since in many parts of the world, groundwater will be near this temperature for at least part of the year, it is important to examine the effects of the density maximum on convection in porous media.
作者: 馬賽克    時(shí)間: 2025-3-25 13:03
1568-2609 ro- ductive field for many researchers and practical engineers in very diverse range of fields. The great interest in the topic stems from its widespread number of different practical applications in modern industries and in many environmental issues, such as nuclear waste management, build- ing the
作者: 笨拙處理    時(shí)間: 2025-3-25 18:05

作者: predict    時(shí)間: 2025-3-25 22:49

作者: 遠(yuǎn)足    時(shí)間: 2025-3-26 03:00

作者: 突襲    時(shí)間: 2025-3-26 07:13
Nikki P. Lee,C.Y. Cheng,John M. Lukshown by these studies, the Rayleigh number for the onset of synchronous convection increases with the frequency of vibration for a layer oscillating with constant vertical amplitude until a certain frequency of modulation is reached and at which the onset is in the form of subharmonic motions.
作者: Blanch    時(shí)間: 2025-3-26 10:53

作者: 王得到    時(shí)間: 2025-3-26 15:38
Techniques for Solving the Boundary-Layer Equations,flow), but the flow of an almost inviscid fluid, e.g. air, past a body requires us to develop the theory of boundary layers. These flows are of great practical interest, e.g. in aerodynamical flows, and in these flows, in general, we have the Reynolds number, Re ? 1.
作者: Cloudburst    時(shí)間: 2025-3-26 19:06
Laplacian Decomposition of Steady Free Convection in Porous Media,y harmonic functions which arise from the ideas of Goursat decomposition, whilst using a finite difference approach requires the evaluation of the gradient of the temperature inside the domain. These equations, which become coupled through the boundary conditions, are numerically solved using the boundary element method (BEM).
作者: fulmination    時(shí)間: 2025-3-27 00:50
Active Control of the Onset of Convection in Porous Medium by Mechanical Vibration,shown by these studies, the Rayleigh number for the onset of synchronous convection increases with the frequency of vibration for a layer oscillating with constant vertical amplitude until a certain frequency of modulation is reached and at which the onset is in the form of subharmonic motions.
作者: Granular    時(shí)間: 2025-3-27 05:00

作者: 并排上下    時(shí)間: 2025-3-27 08:36
Molecular Nevogenesis: An Update,edia: scale analysis, heat lines, and the intersection of asymptotes method. Another objective is to draw attention to the growing literature that is devoted to the development and application of these methods, see Bejan . [.].
作者: Cocker    時(shí)間: 2025-3-27 11:45

作者: Canyon    時(shí)間: 2025-3-27 15:30
Yu-Hsun Chen,Marco Ceccarelli,Hong-Sen Yannsity, can only be found for bodies with very simple geometries. It is also possible to find solutions when the Reynolds number is very small (Stokes flow), but the flow of an almost inviscid fluid, e.g. air, past a body requires us to develop the theory of boundary layers. These flows are of great
作者: WAIL    時(shí)間: 2025-3-27 19:40

作者: 提名的名單    時(shí)間: 2025-3-28 00:38

作者: 季雨    時(shí)間: 2025-3-28 02:37

作者: intricacy    時(shí)間: 2025-3-28 08:32

作者: 情愛(ài)    時(shí)間: 2025-3-28 10:28

作者: 吹牛需要藝術(shù)    時(shí)間: 2025-3-28 16:28

作者: forebear    時(shí)間: 2025-3-28 22:26
Nikki P. Lee,C.Y. Cheng,John M. Lukweakly nonlinear stability analyses have been developed by Gresho and Sani [.], Clever . [.] and by the Russian workers Gershuni and Lyubimov [.]. As shown by these studies, the Rayleigh number for the onset of synchronous convection increases with the frequency of vibration for a layer oscillating
作者: NOCT    時(shí)間: 2025-3-28 23:52
Global Population and Demographic Trends,n double-diffusive convection has been reviewed by Nield and Bejan [.]. Numerical simulation of convective flows within porous media has considerably improved during the last three decades. Clearly, this is mainly due to the improvement in numerical techniques and high speed computers with large mem
作者: 淡紫色花    時(shí)間: 2025-3-29 04:53

作者: Coeval    時(shí)間: 2025-3-29 07:17

作者: glisten    時(shí)間: 2025-3-29 14:12
An Overview on Animal Models of ALL,olid structure are assumed to be in local thermal equilibrium. This assumption is satisfactory for small-pore media such as geothermal reservoirs and fibrous insulations and small temperature differences between phases. In the second kind of approach, the fluid and solid structure are assumed to be
作者: foreign    時(shí)間: 2025-3-29 17:32

作者: 大廳    時(shí)間: 2025-3-29 20:44

作者: 強(qiáng)壯    時(shí)間: 2025-3-30 00:56

作者: Confidential    時(shí)間: 2025-3-30 05:03
Molecular Nevogenesis: An Update,edia: scale analysis, heat lines, and the intersection of asymptotes method. Another objective is to draw attention to the growing literature that is devoted to the development and application of these methods, see Bejan . [.].
作者: 沉著    時(shí)間: 2025-3-30 09:35
Fundamentals of Scale Analysis, Heatline Visualization, and the Intersection of Asymptotes,edia: scale analysis, heat lines, and the intersection of asymptotes method. Another objective is to draw attention to the growing literature that is devoted to the development and application of these methods, see Bejan . [.].
作者: 偏離    時(shí)間: 2025-3-30 13:35
978-1-4020-1874-9Springer Science+Business Media Dordrecht 2004
作者: 道學(xué)氣    時(shí)間: 2025-3-30 16:37
Emerging Technologies and Techniques in Porous Media978-94-007-0971-3Series ISSN 1568-2609
作者: Conduit    時(shí)間: 2025-3-30 23:00

作者: arthroscopy    時(shí)間: 2025-3-31 04:00
New Advances in Histamine ResearchModeling of macroscopic transport for incompressible flows in porous media has been based on the volume-average methodology for either heat, see Hsu and Cheng [.
作者: Arthritis    時(shí)間: 2025-3-31 09:04

作者: 我沒(méi)有命令    時(shí)間: 2025-3-31 09:32
Turbulent Heat and Mass Transfer in Porous Media,Modeling of macroscopic transport for incompressible flows in porous media has been based on the volume-average methodology for either heat, see Hsu and Cheng [.
作者: Magnificent    時(shí)間: 2025-3-31 14:48

作者: 新義    時(shí)間: 2025-3-31 20:19
New Actions of Parathyroid Hormone is possible to obtain new results concerning different macroscopic equations arising in flow through porous media, to indicate the correct boundary conditions, or to make clearer the dimensionless parameters which are significant in such phenomena.
作者: FLAGR    時(shí)間: 2025-3-31 23:33
Functional Materials and Informationcommon cases, in general, involve transient convection, which is non-similar and hence more complicated mathematically. The interested reader can find an excellent collection of papers on unsteady convective flow problems over heated bodies embedded in a fluid-saturated porous medium in the review p
作者: 引起痛苦    時(shí)間: 2025-4-1 04:58

作者: Militia    時(shí)間: 2025-4-1 06:29





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