Titlebook: Convection in Porous Media; Donald A. Nield,Adrian Bejan Book 2017Latest edition Springer International Publishing AG 2017 Convection in P

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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).

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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.

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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.

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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

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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

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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