4.2 Article

Modeling single-phase fluid flow in porous media through non-local fractal continuum equation

Journal

JOURNAL OF ENGINEERING MATHEMATICS
Volume 138, Issue 1, Pages -

Publisher

SPRINGER
DOI: 10.1007/s10665-022-10245-4

Keywords

Fractal continuum; Fractional derivative; Non-local flow; Porous media; Radial flow

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Modeling fluid flow in highly heterogeneous porous media is a challenging research topic due to the complexities and uncertainties caused by spatial variations of media properties. In this study, a non-local model based on fractal continuum theory is proposed to describe single-phase flow in such media. The model incorporates generalized Laplacian operator and non-local Darcy's law to capture the effects of non-locality in fractal porous media. The analysis of flow dynamics reveals the significant influence of anomalous parameters on pressure and rate transients, providing valuable insights for understanding fluid flow in porous media with complex geometries.
Modeling fluid flow in highly heterogeneous porous media is an open research topic due to the degree of complexities and uncertainties attributable mainly to the spatial variations of media properties. Mathematical models capable of effectively capturing such complexities are valuable tools to obtain insights into the underlying phenomenology and characterize the system behavior under different boundary conditions or model parameters. In this context, we present a non-local model complemented by the fractal continuum theory to describe single-phase flow in highly heterogeneous porous media. We use the generalized Laplacian operator and the non-local (subdiffusive) Darcy's law to formulate a fluid flow model suitable for fractal porous media with non-local effects. We analyze the dynamics of radially symmetric flow geometry according to radially convergent flow appearing in reservoirs and aquifers. Pressure-transient drop and rate-transient flow scenarios were analyzed for different fractal dimensions and anomalous parameters. The results show that the model parameters associated with the anomalous flow have clear and distinctive effects in field tests, providing a theoretical tool to explore different scenarios under anomalous flow that could be useful for improving our understanding of fluid flow in porous media with complex geometries.

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