We measure the pressure difference during two‐phase flow across a sandstone sample for
a range of injection rates and fractional flows of water, the wetting phase, during an …

The concept of linking pore‐scale data to continuum‐scale characteristics of porous media
relies on the existence of a representative elementary volume (REV). The current techniques …

We investigate the effects of geological stress on fluid flow and tracer transport in natural
fracture networks. We show the emergence of non‐Fickian (anomalous) transport from the …

Recirculation zones (RZs) are common in many geophysical flows. These zones form near
irregular solid boundaries and are separate from the main flow. Since mass can be trapped …

Subsurface substance migration in the fractured rock aquifer is mainly controlled by
fractures, and prediction of solute transport in fractures is important to many geophysical …

This study investigates the effects of compound‐specific diffusion/dispersion and
electrochemical migration on transient solute transport in saturated porous media. We …

It is often highly difficult to predict the main flow path of reactive fluids in porous media with
complexly distributed fractures and/or caves. Based on Darcy's law, this research defines the …

We study the upscaling of advective pore-scale dispersion in terms of the Eulerian velocity
distribution and advective tortuosity, both flow attributes, and of the average pore length, a …

In this work, the influence of pore space geometry on solute transport in porous media is
investigated performing computational fluid dynamics pore-scale simulations of fluid flow …

A pore-scale model is applied to investigate reactive mass transport in dual porosity media.
We use a framework based on the Stokes-Brinkman flow to model reactive flow in porous …