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Titlebook: Convection in Porous Media; Donald A. Nield,Adrian Bejan Textbook 19992nd edition Springer-Verlag New York 1999 energy.fluid mechanics.hea

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書目名稱Convection in Porous Media
編輯Donald A. Nield,Adrian Bejan
視頻videohttp://file.papertrans.cn/238/237714/237714.mp4
圖書封面Titlebook: Convection in Porous Media;  Donald A. Nield,Adrian Bejan Textbook 19992nd edition Springer-Verlag New York 1999 energy.fluid mechanics.hea
描述Papers on convection in porous media continue to be published at the rate of over 100 per year. This indication of the continued importance 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 nevertheless there are over 600 new references. We also made an effort to highlight new conceptual developments and engineering applications. In the introductory material, we judged that Chapters 2 and 3 needed little alteration (though there is a new Section 2.6 on other approaches to the topic), but our improved understanding of the basic modeling of flow through a porous medium has led to a number of changes in Chapter 1, both within the old sections and by the addition of a section on turbulence in porous media, and a section on fractured media, deformable media, and complex porous structures. In Chapter 4, on forced convection, we have added major new sections on compact heat exchangers, on heatlines for visualizing convection, and on constructa
出版日期Textbook 19992nd edition
關(guān)鍵詞energy; fluid mechanics; heat transfer; mechanics; multiphase flow; nuclear; porous media
版次2
doihttps://doi.org/10.1007/978-1-4757-3033-3
isbn_ebook978-1-4757-3033-3
copyrightSpringer-Verlag New York 1999
The information of publication is updating

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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.
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