標題: Titlebook: Convection in Porous Media; Donald A. Nield,Adrian Bejan Textbook 19992nd edition Springer-Verlag New York 1999 energy.fluid mechanics.hea [打印本頁] 作者: Remodeling 時間: 2025-3-21 19:47
書目名稱Convection in Porous Media影響因子(影響力)
書目名稱Convection in Porous Media影響因子(影響力)學科排名
書目名稱Convection in Porous Media網(wǎng)絡公開度
書目名稱Convection in Porous Media網(wǎng)絡公開度學科排名
書目名稱Convection in Porous Media被引頻次
書目名稱Convection in Porous Media被引頻次學科排名
書目名稱Convection in Porous Media年度引用
書目名稱Convection in Porous Media年度引用學科排名
書目名稱Convection in Porous Media讀者反饋
書目名稱Convection in Porous Media讀者反饋學科排名
作者: 煩躁的女人 時間: 2025-3-21 21:44 作者: Emg827 時間: 2025-3-22 04:18 作者: deforestation 時間: 2025-3-22 04:46 作者: ANT 時間: 2025-3-22 09:23
https://doi.org/10.1007/978-94-015-7634-5the medium is isotropic, and where radiative effects, viscous dissipation, and the work done by pressure changes are negligible. Very shortly we shall assume that there is local thermal equilibrium so that .. = .. = ., where .. and .. are the temperatures of the solid and fluid phases, respectively.作者: 注意力集中 時間: 2025-3-22 13:24 作者: 注意力集中 時間: 2025-3-22 17:29 作者: Influx 時間: 2025-3-22 23:18 作者: 帶來的感覺 時間: 2025-3-23 02:19 作者: 節(jié)約 時間: 2025-3-23 08:46 作者: –FER 時間: 2025-3-23 10:09 作者: garrulous 時間: 2025-3-23 15:51
https://doi.org/10.1007/978-94-015-7293-4usual situation) or it undergoes small deformation. The interconnectedness of the void (the pores) allows the flow of one or more fluids through the material. In the simplest situation (“single-phase flow”) the void is saturated by a single fluid. In “two-phase flow” a liquid and a gas share the void space.作者: 現(xiàn)任者 時間: 2025-3-23 18:44 作者: eustachian-tube 時間: 2025-3-23 22:28 作者: resilience 時間: 2025-3-24 03:12
Springer-Verlag New York 1999作者: Melanocytes 時間: 2025-3-24 08:05
Mechanics of Fluid Flow Through a Porous Medium,usual situation) or it undergoes small deformation. The interconnectedness of the void (the pores) allows the flow of one or more fluids through the material. In the simplest situation (“single-phase flow”) the void is saturated by a single fluid. In “two-phase flow” a liquid and a gas share the void space.作者: Somber 時間: 2025-3-24 13:32
External Natural Convection,ortant. For small values of the Rayleigh number Ra, perturbation methods are appropriate. At large values of Ra thermal boundary layers are formed, and boundary layer theory is the obvious method of investigation. This approach forms the subject of much of this chapter. We follow, to a large extent, the discussion by Cheng (1985a).作者: 死亡率 時間: 2025-3-24 14:58 作者: 通便 時間: 2025-3-24 19:34 作者: 即席演說 時間: 2025-3-25 00:55
https://doi.org/10.1007/978-94-015-8030-4Since we have dealt with natural convection and forced convection in some detail, our treatment of mixed convection can be brief. It is guided by the review paper by Lai .. (1991a). We start with a treatment of boundary layer flow on heated plane walls inclined at some nonzero angle to the horizontal.作者: 新手 時間: 2025-3-25 07:05
Mass Transfer in a Porous Medium: Multicomponent and Multiphase Flows,The term “mass transfer” is used here in a specialized sense, namely the transport of a substance that is involved as a component (constituent, species) in a fluid mixture. An example is the transport of salt in saline water. As we shall see below, convective mass transfer is analogous to convective heat transfer.作者: Habituate 時間: 2025-3-25 07:39
Internal Natural Convection: Heating from Below,We start with the simplest case, that of zero flow through the fluid-saturated porous medium.For an equilibrium state the momentum equation is satisfied if..作者: Perineum 時間: 2025-3-25 14:22 作者: Type-1-Diabetes 時間: 2025-3-25 19:20
Mechanics of Fluid Flow Through a Porous Medium,usual situation) or it undergoes small deformation. The interconnectedness of the void (the pores) allows the flow of one or more fluids through the material. In the simplest situation (“single-phase flow”) the void is saturated by a single fluid. In “two-phase flow” a liquid and a gas share the voi作者: 頭腦冷靜 時間: 2025-3-25 20:50
Heat Transfer Through a Porous Medium,the medium is isotropic, and where radiative effects, viscous dissipation, and the work done by pressure changes are negligible. Very shortly we shall assume that there is local thermal equilibrium so that .. = .. = ., where .. and .. are the temperatures of the solid and fluid phases, respectively.作者: 放逐 時間: 2025-3-26 00:45 作者: 艱苦地移動 時間: 2025-3-26 06:16
External Natural Convection,ortant. For small values of the Rayleigh number Ra, perturbation methods are appropriate. At large values of Ra thermal boundary layers are formed, and boundary layer theory is the obvious method of investigation. This approach forms the subject of much of this chapter. We follow, to a large extent,作者: Detonate 時間: 2025-3-26 10:32 作者: Accommodation 時間: 2025-3-26 14:44
Double-Diffusive Convection,s that provide the driving buoyancy force are induced by the combined effects of temperature and species concentration nonuniformities present in the fluid saturated medium. The present chapter is guided by the review of Trevisan and Bejan (1990), which began by showing that the conservation stateme作者: debble 時間: 2025-3-26 20:07
Convection with Change of Phase, matter how intense the heating or cooling effect. In the present chapter we turn our attention to situations in which a change of phase occurs, for example, melting or evaporation upon heating, and solidification or condensation upon cooling. These convection problems constitute a relatively new an作者: 放逐某人 時間: 2025-3-27 00:43 作者: minimal 時間: 2025-3-27 02:58
of the subject, together with the wide acceptance of the first edition, has encouraged us to prepare an expanded second edition. We have retained the basic structure and most of the text of the first edition. With space considerations in mind, we have been selective in our choice of references, but 作者: Negligible 時間: 2025-3-27 05:46
https://doi.org/10.1007/978-94-015-7939-1 transfer process when the flow is steady and in the Darcy regime. Later, we examine the special features of flows that deviate from the Darcy regime, flows that are time-dependent, and flows that are confined in geometries more complicated than the two-dimensional rectangular space shown in Fig. 7.1.作者: 憤世嫉俗者 時間: 2025-3-27 11:16
Harmonic Response of Rotor-Bearing Systems,xample, melting or evaporation upon heating, and solidification or condensation upon cooling. These convection problems constitute a relatively new and active area in the field of convection in porous media.作者: 兵團 時間: 2025-3-27 14:42 作者: 切掉 時間: 2025-3-27 20:11 作者: 工作 時間: 2025-3-27 23:01 作者: 等待 時間: 2025-3-28 05:38 作者: cyanosis 時間: 2025-3-28 09:42
Internal Natural Convection: Heating from the Side, transfer process when the flow is steady and in the Darcy regime. Later, we examine the special features of flows that deviate from the Darcy regime, flows that are time-dependent, and flows that are confined in geometries more complicated than the two-dimensional rectangular space shown in Fig. 7.1.作者: Melatonin 時間: 2025-3-28 12:52
Convection with Change of Phase,xample, melting or evaporation upon heating, and solidification or condensation upon cooling. These convection problems constitute a relatively new and active area in the field of convection in porous media.作者: growth-factor 時間: 2025-3-28 17:37 作者: 動脈 時間: 2025-3-28 19:53
