Intrinsic permeability of heterogeneous porous media

Providing a sound appraisal of the nature of the relationship between flow (Q) and pressure drop ($\Delta$P) for porous media is a longstanding fundamental research challenge. A wide variety of environmental, societal, and industrial issues, ranging, e.g., from water-soil system remediation to subsurface energy optimization, is affected by this critical issue. While such dependence is well represented by the Kozeny-Carman formulation for homogeneous media, the fundamental nature of such a relationship (Q vs $\Delta$P) within heterogeneous porous systems characterized by a broad range of pore sizes is still not fully understood. We design a set of controlled and complex porous structures and quantify their intrinsic permeability through detailed high-quality microfluidics experiments. We synthesize the results upon deriving an original analytical formulation relating the overall intrinsic permeability of the porous structure and its key features. Our formulation explicitly embeds the spatial variability of pore sizes into the medium permeability through a conceptualization of the system as a collection of smaller-scale porous media arranged in series. The resulting analytical formulation yields permeability values matching their experimentally based counterparts without the need for additional tunable parameters. Our study then documents and supports the strong role played by the microstructure on the overall medium permeability.