Abstract
Patterns and fronts arise in most fluid flow situations. Waves, clouds, convection patterns, and turbulence are well-known examples. In porous media the displacement of one fluid by another fluid leads to fronts and patterns that are often fractal (Mandelbrot, 1982; Feder, 1988). The disorder of the porous matrix plays a key role that is not well understood. Depending on the displacement rates, viscosity ratios, miscibility, interfacial tensions, and pore geometry a bewildering variety of displacement fronts arise. Lenormand (Lenormand and Zarcone, 1985a, Lenormand and Zarcone, 1985b; Lenormand, 1985; Lenormand et al., 1988) has studied many of the regimes observed under various conditions during two fluid displacement processes in micromodels of porous media. In our group (Måløy et al., 1985; Feder et al., 1986; Måløy et al., 1987; Furuberg et al., 1988; Oxaal et al., 1987; Måløy et al., 1987; Måløy et al., 1988; Hinrichsen et al., 1989; Oxaal, 1991; Oxaal et al., 1991; Birovljev et al., 1991; Meakin et al., 1992; Frette et al., 1992) we have also studied displacement fronts in two-dimensional micromodels and random bead packs. We have also studied the three-dimensional displacement in transparent models (Frette et al., 1990, Frette et al., 1992). Theoretical simulations are compared in detail to the observed displacement fronts.
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Feder, J., Jøssang, T. (1995). Fractal Patterns in Porous Media Flow. In: Barton, C.C., La Pointe, P.R. (eds) Fractals in Petroleum Geology and Earth Processes. Springer, Boston, MA. https://doi.org/10.1007/978-1-4615-1815-0_10
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