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Titlebook: Emerging Technologies and Techniques in Porous Media; Derek B. Ingham,Adrian Bejan,Ioan Pop Conference proceedings 2004 Springer Science+B

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发表于 2025-3-21 19:51:30 | 显示全部楼层 |阅读模式
书目名称Emerging Technologies and Techniques in Porous Media
编辑Derek B. Ingham,Adrian Bejan,Ioan Pop
视频video
丛书名称NATO Science Series II: Mathematics, Physics and Chemistry
图书封面Titlebook: Emerging Technologies and Techniques in Porous Media;  Derek B. Ingham,Adrian Bejan,Ioan Pop Conference proceedings 2004 Springer Science+B
描述Heat and fluid flow in fluid-saturated porous media has become increas­ ingly more attractive to researchers and thus it has become a very pro­ ductive field for many researchers and practical engineers in very diverse range of fields. The great interest in the topic stems from its widespread number of different practical applications in modern industries and in many environmental issues, such as nuclear waste management, build­ ing thermal insulators, geothermal power plants, grain storage, etc. In building sciences and thermal insulation engineering, an appreciable in­ sulating effect has been derived by placing porous material in the gap between the cavity walls and multishield structures of nuclear reactors between the pressure vessel and the reactor. Geophysical applications include modeling of the spread of pollutants (e. g. radioactive mater­ ial), water movements in geothermal reservoirs, enhanced recovery of petroleum reservoirs, etc. These, and many other, important practical applications have resulted in a rapid expansion of research in the general area of porous media and thus generated a vast amount of both theor­ etical and experimental research work. It has attracted
出版日期Conference proceedings 2004
关键词Vibration; algorithm; algorithms; construction; genetic algorithms; layers; model; modeling; stability; therm
版次1
doihttps://doi.org/10.1007/978-94-007-0971-3
isbn_softcover978-1-4020-1874-9
isbn_ebook978-94-007-0971-3Series ISSN 1568-2609
issn_series 1568-2609
copyrightSpringer Science+Business Media Dordrecht 2004
The information of publication is updating

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Modeling the Flow Through Porous Media,c levels are described by taking mean values of the microscopic quantities and there are several methods of doing this. In this chapter we are interested in the homogenization method. In fact a more descriptive name for this method is .. This means that the method consists of taking the mean value f
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Techniques for Solving the Boundary-Layer Equations,nsity, can only be found for bodies with very simple geometries. It is also possible to find solutions when the Reynolds number is very small (Stokes flow), but the flow of an almost inviscid fluid, e.g. air, past a body requires us to develop the theory of boundary layers. These flows are of great
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Compressible Fluid Dynamics in Porous Media by the Boundary Element Method,taining the solutions of some transport phenomena in porous media, e.g. the finite-difference method (FDM), finite element method (FEM), finite volume method (FVM), as well as the boundary element method (BEM). The main comparative advantage of the BEM, the application of which requires the given pa
发表于 2025-3-22 17:08:41 | 显示全部楼层
Laplacian Decomposition of Steady Free Convection in Porous Media,l technique based on a Laplacian decomposition. This results in the need to solve three Laplace’s equations for the temperature and two other auxiliary harmonic functions which arise from the ideas of Goursat decomposition, whilst using a finite difference approach requires the evaluation of the gra
发表于 2025-3-23 01:00:45 | 显示全部楼层
Genetic Algorithms and their Application to the Identification of Hydraulic Properties of Rocks,hly nonlinear or non-monotonie, may have a very complex form or its analytical expression may be unknown. Traditional, gradient based, optimisation algorithms are likely to fail for objective functions that exhibit multiple local optima and for such a gradient based algorithms in practice it is ofte
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The Mixed Convection Number for Porous Media Flow,id above lower density fluid. Where a density gradient is present, buoyancy may initiate an additional velocity component upward or downward, i.e. in direction of gravity. It depends on three system properties if the buoyancy impetus changes the flow field in the system. When there is a strong diffu
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