Next Article in Journal
Water Quality Dynamics of Urban Water Bodies during Flooding in Can Tho City, Vietnam
Next Article in Special Issue
Simulating the Fate and Transport of Coal Seam Gas Chemicals in Variably-Saturated Soils Using HYDRUS
Previous Article in Journal
Study on Variations in Climatic Variables and Their Influence on Runoff in the Manas River Basin, China
Previous Article in Special Issue
Understanding the Budyko Equation
Article Menu
Issue 4 (April) cover image

Export Article

Open AccessArticle
Water 2017, 9(4), 252;

Effects of Pore-Scale Geometry and Wettability on Two-Phase Relative Permeabilities within Elementary Cells

Dipartimento di Ingegneria Civile e Ambientale (DICA), Politecnico di Milano, Piazza Leonardo da Vinci 32, 20133 Milano, Italy
Department of Hydrology and Atmospheric Sciences, Tucson, AZ 85721, USA
Author to whom correspondence should be addressed.
Academic Editor: Boris Faybishenko
Received: 26 January 2017 / Revised: 23 March 2017 / Accepted: 27 March 2017 / Published: 5 April 2017
(This article belongs to the Special Issue Water and Solute Transport in Vadose Zone)
Full-Text   |   PDF [5849 KB, uploaded 5 April 2017]   |  


We study the relative role of the complex pore space geometry and wettability of the solid matrix on the quantification of relative permeabilities of elementary cells of porous media. These constitute a key element upon which upscaling frameworks are typically grounded. In our study we focus on state immiscible two-phase flow taking place at the scale of elementary cells. Pressure-driven two-phase flow following simultaneous co-current injection of water and oil is numerically solved for a suite of regular and stochastically generated two-dimensional explicit elementary cells with fixed porosity and sharing main topological/morphological features. We show that the relative permeabilities of the randomly generated elementary cells are significantly influenced by the formation of preferential percolation paths, called principal pathways, giving rise to a strongly nonuniform distribution of fluid fluxes. These pathways are a result of the spatially variable resistance that the random pore structures exert on the fluid. The overall effect on relative permeabilities of the diverse organization of principal pathways, as driven by a given random realization at the scale of the elementary cell, is significantly larger than that of the wettability of the host rock. In contrast to what can be observed for the random cells analyzed, the relative permeabilities of regular cells display a clear trend with contact angle at the investigated scale. View Full-Text
Keywords: relative permeability; wettability; porous media; pore-scale simulations; two-phase flow relative permeability; wettability; porous media; pore-scale simulations; two-phase flow

Figure 1

This is an open access article distributed under the Creative Commons Attribution License which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited (CC BY 4.0).

Share & Cite This Article

MDPI and ACS Style

Bianchi Janetti, E.; Riva, M.; Guadagnini, A. Effects of Pore-Scale Geometry and Wettability on Two-Phase Relative Permeabilities within Elementary Cells. Water 2017, 9, 252.

Show more citation formats Show less citations formats

Note that from the first issue of 2016, MDPI journals use article numbers instead of page numbers. See further details here.

Related Articles

Article Metrics

Article Access Statistics



[Return to top]
Water EISSN 2073-4441 Published by MDPI AG, Basel, Switzerland RSS E-Mail Table of Contents Alert
Back to Top