Abstract

Mixing is pivotal to conservative and reactive transport behaviors in porous media. Methods for investigating mixing processes include mathematical models, laboratory experiments and numerical simulations. The latter have been historically limited by the extreme computational resources needed for solving flow and transport at the microscopic scale within the complex pore structure of a three-dimensional porous medium, while dealing with a sufficiently large domain in order to generate meaningful emergent continuum-scale observables. We present the results of such a set of virtual column experiments, which have been conducted by taking advantage of modern high-performance computing infrastructure and Computational Fluid Dynamics software capable of massively parallel simulations. The computational approach has important advantages such as full control over the experimental conditions as well as high spatial and temporal resolution of measurements. Hydrodynamic dispersion results agree with the empirical and theoretical literature and link dispersivity to median grain size, while elucidating the impact of grain size variability on the critical Péclet number. Reactive transport results also indicate that the relative degree of incomplete mixing is related to the granular material’s mean hydraulic radius and not directly to the median grain size. When compared to a well-known laboratory experiment with similar configuration, less incomplete mixing is observed in our simulations. We offer a partial explanation for this discrepancy, by showing how an apparent nonlinear absorbance–concentration relationship may induce laboratory measurement error in the presence of local concentration fluctuations.

Highlights

  • Mixing is a key element of flow and transport through porous media, playing a critical role in most aspects of solute plume behavior including homogenization, dilution, dispersion, and reaction

  • We have presented a set of extreme-resolution pore-scale flow and transport simulations emulating a long column experiment to study macroscopic dispersion, mixing and reaction in granular porous media under laminar saturated flow conditions

  • The permeability value is very closely predicted from the hydraulic radius by the Kozeny-Carman equation

Read more

Summary

Introduction

Mixing is a key element of flow and transport through porous media, playing a critical role in most aspects of solute plume behavior including homogenization, dilution, dispersion, and reaction. Performing a virtual, pore-scale column experiment to investigate solute mixing can overcome some of the typical difficulties of physical models thanks to (i) full control over the experimental setup and conditions, and (ii) high-resolution, accurate observations. This high degree of fidelity can be used to establish precise links between the local and the upscaled transport features, and to study the role of various contributing factors with little uncertainty. We describe the simulation methods and the virtual setup, which is in many ways analogous to a physical column experiment designed to study hydrodynamic mixing in saturated porous media

Generation of synthetic porous media
Flow and Transport
Meshing
Navier-Stokes
Advection-Diffusion
Conservative transport and dispersion
Asymptotic Dispersion
Pre-asymptotic and non-Fickian behavior
Reactive transport
Observations of mixing-limited reaction
Impact of local concentration variability on measurements
Findings
Summary and conclusions
Full Text
Published version (Free)

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call