Abstract

Mathematical models based on probability density functions (PDF) have been extensively used in hydrology and subsurface flow problems, to describe the uncertainty in porous media properties (e.g., permeability modelled as random field). Recently, closer to the spirit of PDF models for turbulent flows, some approaches have used this statistical viewpoint also in pore-scale transport processes (fully resolved porous media models). When a concentration field is transported, by advection and diffusion, in a heterogeneous medium, in fact, spatial PDFs can be defined to characterise local fluctuations and improve or better understand the closures performed by classical upscaling methods. In the study of hydrodynamical dispersion, for example, PDE-based PDF approach can replace expensive and noisy Lagrangian simulations (e.g., trajectories of drift-diffusion stochastic processes). In this work we derive a joint position-velocity Fokker–Planck equation to model the motion of particles undergoing advection and diffusion in in deterministic or stochastic heterogeneous velocity fields. After appropriate closure assumptions, this description can help deriving rigorously stochastic models for the statistics of Lagrangian velocities. This is very important to be able to characterise the dispersion properties and can, for example, inform velocity evolution processes in continuous time random walk dispersion models. The closure problem that arises when averaging the Fokker–Planck equation shows also interesting similarities with the mixing problem and can be used to propose alternative closures for anomalous dispersion.

Highlights

  • The evolution of solute and particle transport in heterogeneous porous media is determined by the heterogeneity of the medium, the consequent flow heterogeneity and small scale diffusion (Saffman 1959; de Josselin de Jong 1958; Bear 1972)

  • Small scale velocity fluctuations and mass transfer processes give rise to large scale transport dynamics characterised by hydrodynamic dispersion, and non-Fickian transport characteristics such as long tails in breakthrough curves and non-linear evolution of solute dispersion (Liu and Kitanidis 2012; Kang et al 2014; de Anna et al 2013; Dentz et al 2018a; Puyguiraud et al 2019)

  • We focus here on an alternative approach based on probability density functions, in the following termed PDF methods (Pope and Pope 2000)

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Summary

Introduction

The evolution of solute and particle transport in heterogeneous porous media is determined by the heterogeneity of the medium, the consequent flow heterogeneity and small scale diffusion (Saffman 1959; de Josselin de Jong 1958; Bear 1972) These processes determine the average transport behaviours and the fluctuation dynamics. Small scale velocity fluctuations and mass transfer processes give rise to large scale transport dynamics characterised by hydrodynamic dispersion, and non-Fickian transport characteristics such as long tails in breakthrough curves and non-linear evolution of solute dispersion (Liu and Kitanidis 2012; Kang et al 2014; de Anna et al 2013; Dentz et al 2018a; Puyguiraud et al 2019) The understanding of these behaviours plays a central role in a series of applications across different fields and applications ranging from geothermal energy to packed bead reactors. PDF methods in porous media have been used both for the upscaling of fluctuating small scale

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Joint position-velocity PDF equation
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Velocity marginal PDF and closures
Constant shear
Equilibrium Eulerian velocity PDF
Perturbation near equilibrium
Interaction by exchange with the mean
Deterministic shear flows
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D u 20 L2
Discussion and conclusions
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A Appendix
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Full Text
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