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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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

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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

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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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