Abstract

AbstractWe propose an approach to upscale solute transport in spatially periodic porous media. Our methodology relies on pore‐scale information to predict large‐scale transport features, including explicit reconstruction of the solute plume, breakthrough curves at fixed distances, and spatial spreading transverse to the main flow direction. The proposed approach is grounded on the recently proposed trajectory‐based spatial Markov model (tSMM), which upscales transport based on information collected from advective‐diffusive particle trajectories across one periodic element. In previous works, this model has been applied solely to one‐dimensional transport in a single periodic pore geometry. In this work we extend the tSMM to the prediction of multidimensional solute plumes. This is obtained by analyzing the joint space‐time probability distribution associated with discrete particles, as yielded by the tSMM. By comparing numerical results from fully resolved simulations and predictions obtained with the tSMM over a wide range of Péclet numbers, we demonstrate that the proposed approach is suitable for modeling transport of conservative and linearly decaying solute species in a realistic pore space and showcase the applicability of the model to predict steady‐state solute plumes. Additionally, we evaluate the model performance as a function of numerical parameters employed in the tSMM parameterization.

Highlights

  • Solute transport in porous media is a fundamental problem across many disciplines, including subsurface geological systems and the performance optimization of engineered materials such as filtration membranes

  • Results obtained through the trajectory-based Spatial Markov model (tSMM) are in close agreement with those yielded by the direct numerical simulation (DNS)

  • Our study proposes a methodology for upscaling solute plumes in periodic porous media through a trajectory based spatial Markov Model

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Summary

Introduction

Solute transport in porous media is a fundamental problem across many disciplines, including subsurface geological systems and the performance optimization of engineered materials such as filtration membranes. The solution of three closure prob lems is required to fully parameterize solute transport based on pore scale information 43 through volume averaging (Valdes-Parada et al, 2016) These separate closures are nec essary to isolate and characterize the separate effects of diffusion and advection on trans port. 49 these effects can still be represented with Eulerian nonlocal (integro-differential) mod els In principle these models can be derived by applying upscaling approaches, such as 51 volume averaging, that can relate pore scale geometry and fluid velocities with the emerg ing transport dynamics through a set of closure differential equations Wood & Valdes Parada (2013). It is often found that resorting to such approaches leads to formidable mathematical and numerical complexity (Davit et al, 2012; Porta et al, 2016), which is associated with i) the numerical resolution of various closure problems and ii) the ap proximation of integro-differential equations to obtain the desired large scale outputs

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