Soil Physics - Chapter 3 - Fluids In Porous Media - Skript - Kurt Roth - Institut FR Umweltphysik - UniversitT Heidelberg - 2006.pdf
3 Fluids in Porous Media In a large partment – a river, lake, or the atmosphere – the dynamics is typically dominated by the nonlinear inertia term [v ]v which causes turbulence. Boundary conditions on the other hand are ·simpl∇ e because the direct influence of the boundaries extends only through a small fraction of the flow domain. In contrast, the dynamics of fluids in porous media is generally dominated by the porous matrix which pervades the entire volume and causes a very efficient dissipation of the fluid’s momentum and ic energy. This also leads to a simple internal dynamics, essentially described by Stokes’ law. In the following, we thus first look at the nature of porous media and then at mon approach to handle the difficulties introduced by plicated shape of the flow domain.
Porous Media As essential properties of a porous medium we postulate: 1. The total volume is divided into solid matrix and pore space, with the latter filled by one or more fluids. 2. Every volume element down to a characteristic size ! contains solid matrix as well as pore space. 3. Since we focus on fluid movement, only the connected fraction of the pore space is of interest. Closer scrutiny of the last two points reveals that a precise and general definition of a porous medium is cumbersome. What is the size of !, for instance? Choosing it too small would exclude stony soils while a value that is too large would modate strange media like karstic caverns. Whatever the eventually chosen size, ! has to be very much smaller than the extent of the total volume of interest. After all, there is no point in considering three grains of sand and the space between them as a porous medium. For 39 40 3 Fluids in Porous Media Figure . Artificial porous medium created from sieved sand poured between two parallel glass plates, a so-called Hele-Shaw cell. This may serve as a simple two- 1 mm dimensional model for a porous medium. such objects, the shape of t
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