Titlebook: Convection in Porous Media; Donald A. Nield,Adrian Bejan Book 19921st edition Springer-Verlag New York 1992 convection.energy.environment.

Perineum

mechanical

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

洞穴

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

預(yù)知

nephritis

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

DAMP

演講

SIT

comely

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.

拱墻

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