Modeling and scaling spontaneous imbibition with generalized fractional flow theory and non-Boltzmann transformation
Shaluka Senevirathna, Anna Zemlyanova, Shaina A. Kelly, Qinhong Hu,, Yong Zhang, Behzad Ghanbarian

TL;DR
This paper introduces a generalized fractional flow theory combined with non-Boltzmann scaling to improve modeling and prediction of spontaneous imbibition in various porous media, accounting for complex pore structures and fluid properties.
Contribution
The study develops a novel GFFT model using Hausdorff fractal derivatives and non-Boltzmann scaling, enhancing the accuracy of imbibition predictions across diverse porous materials.
Findings
Non-Boltzmann scaling better collapses SI data than traditional models.
Fractal index alpha varies with contact angle, viscosity, and pore structure.
Alpha values range from 0.88 to 1.54, indicating model adaptability.
Abstract
Spontaneous imbibition (SI) is a process by which liquid is drawn into partially saturated porous media by capillary forces, relevant for subsurface processes like underground fluid storage and withdrawal. Accurate modeling and scaling of counter-current SI have long been challenging. In this study, we proposed a generalized fractional flow theory (GFFT) using the Hausdorff fractal derivative, combined with non-Boltzmann scaling. The model links imbibition distance to time through the power law exponent alpha/2, where alpha is the fractal index (0 < alpha < 2 in this study). We applied the GFFT to various experimental and stimulated datasets of both porous and fractured media, finding that alpha varied with factors such as contact angle (of the imbibing fluid), dynamic viscosity, pore structure, and fracture properties. By analyzing SI data from sandstones, diatomite, carbonate, and…
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Taxonomy
TopicsLattice Boltzmann Simulation Studies · Rheology and Fluid Dynamics Studies
