Effects of Spatiotemporal Upscaling on Predictions of Reactive Transport in Porous Media

TL;DR

This paper explores how spatiotemporal upscaling affects reactive transport predictions in porous media, emphasizing the influence of boundary forcing frequency on macroscopic behavior through homogenization techniques.

Contribution

It introduces a homogenization-based framework for spatiotemporal upscaling in reactive transport, accounting for time-dependent boundary conditions and deriving applicability conditions.

Findings

Macroscopic reactive transport equations depend on boundary forcing frequency.

Time-dependent boundary conditions significantly influence pore-scale to continuum-scale dynamics.

The interplay between signal frequency and transport processes determines macroscopic behavior.

Abstract

The typical temporal resolution used in modern simulations significantly exceeds characteristic time scales at which the system is driven. This is especially so when systems are simulated over time-scales that are much longer than the typical temporal scales of forcing factors. We investigate the impact of space-time upscaling on reactive transport in porous media driven by time-dependent boundary conditions whose characteristic time scale is much smaller than that at which transport is studied or observed at the macroscopic level. The focus is on transport of a reactive solute undergoing diffusion, advection and heterogeneous reaction on the solid grain boundaries. We first introduce the concept of spatiotemporal upscaling in the context of homogenization by multiple-scale expansions, and demonstrate the impact of time-dependent forcings and boundary conditions on macroscopic reactive transport. We then derive the macroscopic equation as well as the corresponding applicability conditions based on the order of magnitude of the P\'{e}clet and Damk\"{o}hler dimensionless numbers. Finally, we demonstrate that the dynamics at the continuum scale is strongly influenced by the interplay between signal frequency at the boundary and transport processes at the pore level.