We consider the flow of an incompressible Newtonian fluid through an
idealized porous medium consisting of an array of identical solid symmetric
lamellae, whose profile varies in space and time due to a stress induced
erosion process. The focus is on the influence of mass exchange between
solid and fluid on the macroscopic flow. By means of the upscaling procedure
illustrated in [6] we derive the governing system of
equations for the macroscopic flow, encompassing various physical
situations. We show that Darcy's law no longer applies in the classical
sense. The corresponding mathematical problem turns out to be surprisingly
complicated. Existence and uniqueness are proved. Numerical simulations are
presented.
Citation: Leda Bucciantini, Angiolo Farina, Antonio Fasano. Flows in porous media with erosion of the solid matrix[J]. Networks and Heterogeneous Media, 2010, 5(1): 63-95. doi: 10.3934/nhm.2010.5.63
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Abstract
We consider the flow of an incompressible Newtonian fluid through an
idealized porous medium consisting of an array of identical solid symmetric
lamellae, whose profile varies in space and time due to a stress induced
erosion process. The focus is on the influence of mass exchange between
solid and fluid on the macroscopic flow. By means of the upscaling procedure
illustrated in [6] we derive the governing system of
equations for the macroscopic flow, encompassing various physical
situations. We show that Darcy's law no longer applies in the classical
sense. The corresponding mathematical problem turns out to be surprisingly
complicated. Existence and uniqueness are proved. Numerical simulations are
presented.