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標(biāo)題: Titlebook: Convection in Porous Media; Donald A. Nield,Adrian Bejan Book 2017Latest edition Springer International Publishing AG 2017 Convection in P [打印本頁]

作者: oxidation    時(shí)間: 2025-3-21 16:52
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作者: LASH    時(shí)間: 2025-3-22 00:16
Picornarvirus Receptors in Pathogenesis,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. More complex situations will be considered in Sect. .. The fundamentals of heat transfer in porous media also are presented in Bejan et al. (2004) and Bejan (2004a).
作者: 衣服    時(shí)間: 2025-3-22 03:09

作者: corpus-callosum    時(shí)間: 2025-3-22 06:27

作者: 1分開    時(shí)間: 2025-3-22 11:49
Book 2017Latest editionts with the elements of fluid mechanics and heat transfer, and covers a wide range of applications from fibrous insulation and catalytic reactors to geological strata, nuclear waste disposal, geothermal reservoirs, and the storage of heat-generating materials. As the standard reference in the field,
作者: 專心    時(shí)間: 2025-3-22 12:54

作者: 專心    時(shí)間: 2025-3-22 17:09
L. Holland,W. Steckelmacher,J. Yarwoodd 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), supplemented by surveys by Pop and Ingham (2000, 2001) and Pop (2004).
作者: Salivary-Gland    時(shí)間: 2025-3-22 22:21
https://doi.org/10.1007/978-94-011-8120-4on the non-Darcy effects. We end this chapter with a review of current engineering applications of the method of forced convection through porous media. Some fundamental aspects of the subject have been discussed by Lage and Narasimhan (2000) and the topic has been reviewed by Lauriat and Ghafir (2000) and Zhang et al. (2011).
作者: ABOUT    時(shí)間: 2025-3-23 04:29
Vitamin C, modern lifestyle and hazards, al. (2000, 2001). An important book dealing with geological fluid dynamics is that by Phillips (2009). In this book, the emphasis is on flow patterns and specifically geological processes, involving dissolution, chemical reaction, and deposition. Some examples are discussed below in Sect. 11.12. Another important book is that by Woods (2014).
作者: 蔓藤圖飾    時(shí)間: 2025-3-23 06:31

作者: pulse-pressure    時(shí)間: 2025-3-23 10:17

作者: 赤字    時(shí)間: 2025-3-23 16:55
Heat Transfer Through a Porous Medium,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. More complex situations will be considered in Sect. .. The fundamentals of heat transfer in porous media also are presented in Bejan et al. (2004) and Bejan (2004a).
作者: 強(qiáng)行引入    時(shí)間: 2025-3-23 18:53

作者: depreciate    時(shí)間: 2025-3-24 01:02
Influenza Viruses and Vaccines,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: CRACY    時(shí)間: 2025-3-24 03:24

作者: reject    時(shí)間: 2025-3-24 09:55
Picornarvirus Receptors in Pathogenesis,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: needle    時(shí)間: 2025-3-24 10:43
https://doi.org/10.1007/978-94-011-8120-4erence. 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 external
作者: lipoatrophy    時(shí)間: 2025-3-24 17:42
L. Holland,W. Steckelmacher,J. Yarwoodortant. 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 t
作者: lattice    時(shí)間: 2025-3-24 21:26

作者: Glucocorticoids    時(shí)間: 2025-3-24 23:55
https://doi.org/10.1007/978-94-011-9839-4 matter how intense the heating or cooling effect. In this 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 and activ
作者: 新星    時(shí)間: 2025-3-25 05:00
Vitamin C, modern lifestyle and hazards,ysical ramifications; see, for example, the reviews by Cheng (1978a, b, 1985b). On the other hand, geothermal reservoir modeling involves several features that are outside the scope of this book, and it usually involves specialist computer packages and techniques. Relevant reviews include those by D
作者: 代理人    時(shí)間: 2025-3-25 08:59

作者: FILTH    時(shí)間: 2025-3-25 14:37

作者: 必死    時(shí)間: 2025-3-25 18:37

作者: 面包屑    時(shí)間: 2025-3-25 21:45
Infinite beam on elastic foundationDetailed studies of some material in this chapter have been made in the books by Straughan (2008, 2015a, b, c, d).
作者: miscreant    時(shí)間: 2025-3-26 00:43
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: pineal-gland    時(shí)間: 2025-3-26 07:11
Internal Natural Convection: Heating from Below,Detailed studies of some material in this chapter have been made in the books by Straughan (2008, 2015a, b, c, d).
作者: 諂媚于人    時(shí)間: 2025-3-26 10:04
https://doi.org/10.1007/978-3-319-49562-0Convection in Porous Media Book; External Natural Convection Porous Medium; Forced Convection Porous M
作者: 船員    時(shí)間: 2025-3-26 16:00
978-3-319-84189-2Springer International Publishing AG 2017
作者: Perceive    時(shí)間: 2025-3-26 16:54

作者: Conscientious    時(shí)間: 2025-3-26 22:36
ccessible introduction for graduate students and others entering the field. The new edition features 2700 new references covering a number of rapidly expanding fields, including the heat transfer properties of nanofluids and applications involving local thermal non-equilibrium and microfluidic effects..978-3-319-84189-2978-3-319-49562-0
作者: 適宜    時(shí)間: 2025-3-27 04:58
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
作者: 神圣將軍    時(shí)間: 2025-3-27 07:16

作者: 笨拙的你    時(shí)間: 2025-3-27 10:23
Forced Convection,erence. 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 external
作者: Institution    時(shí)間: 2025-3-27 17:08
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 t
作者: 迅速成長    時(shí)間: 2025-3-27 18:22
Internal Natural Convection: Heating from the Side,, 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: conscience    時(shí)間: 2025-3-28 01:04

作者: 精確    時(shí)間: 2025-3-28 06:03

作者: 輕快來事    時(shí)間: 2025-3-28 06:47

作者: WATER    時(shí)間: 2025-3-28 13:38
Book 2018ematology topics such as post-natal management of an RhD negative woman for the preventionof hemolytic disease of the newborn due to anti-Rh(D) are included..Written by transfusion medicine, coagulation, obstetrical, and anesthesiology experts, .Transfusion Management of the Obstetrical Patient: A C
作者: Nmda-Receptor    時(shí)間: 2025-3-28 16:34

作者: Vulnerable    時(shí)間: 2025-3-28 22:43

作者: 態(tài)度暖昧    時(shí)間: 2025-3-29 01:36





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