標(biāo)題: Titlebook: Convection in Porous Media; Donald A. Nield,Adrian Bejan Book 19921st edition Springer-Verlag New York 1992 convection.energy.environment. [打印本頁] 作者: 快樂 時(shí)間: 2025-3-21 16:11
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(xué)科排名
書目名稱Convection in Porous Media網(wǎng)絡(luò)公開度
書目名稱Convection in Porous Media網(wǎng)絡(luò)公開度學(xué)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(xué)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(xué)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(xué)科排名
作者: 流動才波動 時(shí)間: 2025-3-21 20:52
http://image.papertrans.cn/c/image/237711.jpg作者: 身體萌芽 時(shí)間: 2025-3-22 04:10
R. R. Van der Ploeg,F. Beese,P. Beneckeusual 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: CURT 時(shí)間: 2025-3-22 06:47 作者: 沒血色 時(shí)間: 2025-3-22 09:56
https://doi.org/10.1007/978-94-011-5957-9erence. In nature, many saturated porous media interact thermally with one another, and with solid surfaces that confine them or are embedded in them. In this chapter we analyze the basic heat transfer question by looking only at . situations, in which the fluid flow is caused (forced) by an externa作者: ARBOR 時(shí)間: 2025-3-22 13:58
R. R. Van der Ploeg,F. Beese,P. Beneckeortant. For small values of the Rayleigh number ., perturbation methods are appropriate. At large values of . 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作者: ARBOR 時(shí)間: 2025-3-22 19:06
N. Klearchou,J. Bontis,S. Mantalenakis, industrial cold-storage installations, and cryogenics. As in the earlier chapters, we begin with the most fundamental aspects of the convection heat 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,作者: 淡紫色花 時(shí)間: 2025-3-22 23:18
Voluntary Termination of Pregnancyreview paper by Lai, Prasad, and Kulacki (1991). We start with a treatment of boundary layer flow on heated plane walls inclined at some nonzero angle to the horizontal. This configuration is illustrated in Fig. 8.1. The boundary layer equations [compare Eqs. (5.5) and (5.6)] for steady flow are ., 作者: 無王時(shí)期, 時(shí)間: 2025-3-23 05:20 作者: 我要沮喪 時(shí)間: 2025-3-23 08:41 作者: 鬧劇 時(shí)間: 2025-3-23 10:32 作者: Deadpan 時(shí)間: 2025-3-23 16:34
https://doi.org/10.1007/978-1-4757-2175-1convection; energy; environment; fluid mechanics; heat transfer; nuclear; pollution; porous media; fluid- an作者: 老人病學(xué) 時(shí)間: 2025-3-23 20:53
Springer-Verlag New York 1992作者: 和音 時(shí)間: 2025-3-24 01:15 作者: exorbitant 時(shí)間: 2025-3-24 03:18
External Natural Convection,ortant. For small values of the Rayleigh number ., perturbation methods are appropriate. At large values of . 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: 語言學(xué) 時(shí)間: 2025-3-24 06:45 作者: 緊張過度 時(shí)間: 2025-3-24 11:23
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 area in the field of convection in porous media.作者: judiciousness 時(shí)間: 2025-3-24 18:13
https://doi.org/10.1007/978-94-011-5957-9The 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: heterogeneous 時(shí)間: 2025-3-24 21:44
Inner Product of Functions. Norm, MetricWe 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: 有發(fā)明天才 時(shí)間: 2025-3-24 23:37
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: photophobia 時(shí)間: 2025-3-25 05:49 作者: intimate 時(shí)間: 2025-3-25 11:02
R. R. Van der Ploeg,F. Beese,P. Beneckeusual 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: 檢查 時(shí)間: 2025-3-25 13:05 作者: unstable-angina 時(shí)間: 2025-3-25 17:14
Voluntary Termination of Pregnancyreview paper by Lai, Prasad, and Kulacki (1991). We start with a treatment of boundary layer flow on heated plane walls inclined at some nonzero angle to the horizontal. This configuration is illustrated in Fig. 8.1. The boundary layer equations [compare Eqs. (5.5) and (5.6)] for steady flow are ., ..作者: FACET 時(shí)間: 2025-3-25 22:32
H. Abramovici,A. Rofe,J. Atad,J. H. Faktor 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 area in the field of convection in porous media.作者: TAIN 時(shí)間: 2025-3-26 00:24 作者: GRIEF 時(shí)間: 2025-3-26 04:51 作者: 強(qiáng)化 時(shí)間: 2025-3-26 12:20 作者: 單調(diào)女 時(shí)間: 2025-3-26 15:48
External Natural Convection,ortant. For small values of the Rayleigh number ., perturbation methods are appropriate. At large values of . 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作者: 變態(tài) 時(shí)間: 2025-3-26 19:45 作者: Perineum 時(shí)間: 2025-3-26 23:08 作者: mechanical 時(shí)間: 2025-3-27 03:06
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: 洞穴 時(shí)間: 2025-3-27 08:27
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 ar作者: 預(yù)知 時(shí)間: 2025-3-27 13:27 作者: nephritis 時(shí)間: 2025-3-27 16:14
Book 19921st editionersant with the basic elements of fluid mechanics and heat transfer, but otherwise the book is self-contained. Only routine classical mathematics is employed. We hope that the book will be useful both as a review (for reference) and as a tutorial work (suitable as a textbook in a graduate course or 作者: DAMP 時(shí)間: 2025-3-27 21:46 作者: 演講 時(shí)間: 2025-3-27 22:41 作者: SIT 時(shí)間: 2025-3-28 04:46 作者: comely 時(shí)間: 2025-3-28 08:44
Geophysical Aspects, and Lippmann (1986), and Bjornsson and Stefansson (1987). In this chapter we discuss a number of topics which involve additional physical processes or which lead to theoretical developments beyond those which we have already covered.作者: 拱墻 時(shí)間: 2025-3-28 13:36
er is conversant with the basic elements of fluid mechanics and heat transfer, but otherwise the book is self-contained. Only routine classical mathematics is employed. We hope that the book will be useful both as a review (for reference) and as a tutorial work (suitable as a textbook in a graduate 作者: DNR215 時(shí)間: 2025-3-28 16:52 作者: deadlock 時(shí)間: 2025-3-28 22:15
N. Klearchou,J. Bontis,S. Mantalenakis 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: NAIVE 時(shí)間: 2025-3-29 02:16
Forced Convection, In this chapter we analyze the basic heat transfer question by looking only at . situations, in which the fluid flow is caused (forced) by an external agent unrelated to the heating effect. First we discuss the results that have been developed based on the Darcy flow model, and later we address the more recent work on the non-Darcy effects.作者: blight 時(shí)間: 2025-3-29 06:03 作者: engagement 時(shí)間: 2025-3-29 11:18
https://doi.org/10.1007/978-94-011-5957-9 More complex situations will be considered in Section 6.5. Here we also assume that heat conduction in the solid and fluid phases takes place in parallel so that there is no net heat transfer from one phase to the other.作者: DOSE 時(shí)間: 2025-3-29 13:22 作者: 先兆 時(shí)間: 2025-3-29 16:44
Stretch-induced Abortion at Mid-trimester and Lippmann (1986), and Bjornsson and Stefansson (1987). In this chapter we discuss a number of topics which involve additional physical processes or which lead to theoretical developments beyond those which we have already covered.
