# A pore-scale study of transport of inertial particles by water in porous media

## TL;DR

This study investigates how inertial particles move and accumulate in water flowing through porous media, revealing two accumulation regimes and the conditions leading to clogging, with implications for flow behavior and clog formation.

## Contribution

It introduces a pore-scale analysis of inertial particle transport, highlighting the role of hydrodynamic effects and media heterogeneity in particle accumulation and clogging.

## Key findings

- Two accumulation regimes identified: low and high flow velocities.
- Clog formation occurs at high velocities at pore entrances.
- Heterogeneous media promote accumulation, unlike homogeneous media.

## Abstract

We study the transport of inertial particles in water flow in porous media. Our interest lies in understanding the accumulation of particles including the possibility of clogging. We propose that accumulation can be a result of hydrodynamic effects: the tortuous paths of the porous medium generate regions of dominating strain/vorticity, which favour the accumulation/dispersion of the inertial particles. Numerical simulations show that essentially two accumulation regimes are identified: for low and for high flow velocities. When particles accumulate in high-velocity regions, at the entrance of a pore throat, a clog is formed. The formation of a clog significantly modifies the flow, as the partial blockage of the pore causes a local redistribution of pressure. This redistribution can divert the upstream water flow into neighbouring pores. Moreover, we show that accumulation in high velocity regions occurs in heterogeneous media, but not in homogeneous media, where we refer to homogeneity with respect to the distribution of the pore throat diameters.