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Numerical simulation of retention and release of colloids in porous media at the pore scale

Article dans une revue avec comité de lecture
Auteur
SEFRIOUI, Nisrine
ccAHMADI-SENICHAULT, Azita
OMARI, Aziz
BERTIN, Henri

URI
http://hdl.handle.net/10985/8835
DOI
10.1016/j.colsurfa.2013.03.005
Date
2013
Journal
Colloids and Surfaces A: Physicochemical and Engineering Aspects

Résumé

Transport of a solid colloidal particle was simulated at the pore scale in presence of surface roughness and particle/pore physicochemical interaction by adopting a “one fluid” approach. A code developed in our laboratory was used to solve equations of motion, while implementing additional modules in order to take into account lubrication and physicochemical forces. Particles were recognized through a phase indicator function and the particle/fluid interface position at each instant was obtained by solving a transport equation. Roughnesses of different shapes were considered and the magnitude of the particle/pore physicochemical interaction was monitored through the change of the ionic strength of the suspending fluid. We first show that if pore surface is smooth no retention of the transported particle occurs whether the particle/pore surface is attractive or repulsive. However for shape roughnesses of “peak” or “valley”, particles may be retained inside pores or not depending on the considered ionic strength. In absence of particle retention, the residence time (the time needed for a particle to travel a characteristic pore distance) is finite and was found to be an increasing function of ionic strength for every considered roughness at fixed hydrodynamic conditions.

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  • Institut de Mécanique et d’Ingénierie de Bordeaux (I2M)

Documents liés

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  • Mise en évidence du facteur de retard dans la cinétique de dépôt colloïdal en milieux poreux 
    Communication avec acte
    SEFRIOUI, Nisrine; ccAHMADI-SENICHAULT, Azita; BERTIN, Henri; OMARI, Aziz (SFP, 2011)
    Les milieux poreux naturels, comme les sols ou les aquifères, contiennent des particules colloïdales naturelles dont le diamètre est inférieur au micron. Selon des conditions hydrodynamiques et géochimiques, celles-ci ...
  • Direct numerical simulation of colloid transport at the microscopic scale: influence of ionic strength in the presence of a rough surface 
    Communication sans acte
    SEFRIOUI, Nisrine; ccAHMADI-SENICHAULT, Azita; BERTIN, Henri; OMARI, Aziz (2012)
    The way colloids are transported, deposited or detached in porous media is of great importance in many practical problems such as filtration, environmental issues, petroleum engineering, … In this work, direct numerical ...
  • On the influence of ionic strength on colloid transport in porous media in the presence of a rough surface : numerical simulation at the microscopic scale 
    Communication avec acte
    SEFRIOUI, Nisrine; ccAHMADI-SENICHAULT, Azita; BERTIN, Henri; OMARI, Aziz (IFP Energies nouvelles, 2012)
    The understanding of Colloids transport, deposit or detachment in porous media is of central importance in many practical problems such as filtration, environmental issues and petroleum engineering. In particular, the ...
  • Displacement of colloidal dispersions in Porous Media: experimental & numerical approaches 
    Article dans une revue avec comité de lecture
    ccAHMADI-SENICHAULT, Azita; CANSECO, Vladimir; SEFRIOUI-CHAIBAINOU, Nisrine; OMARI, Aziz; BERTIN, Henri (Trans Tech Publications Ltd, 2016)
    The main objective of this paper is to give more insight on colloids deposition and re-entrainment in presence of a rough surface. Experiments on retention and release of colloids in a porous medium are first presented. ...
  • Macroscopic modeling of colloids adsorption in porous media 
    Communication avec acte
    SEFRIOUI, Nisrine; ccAHMADI-SENICHAULT, Azita; BERTIN, Henri; OMARI, Aziz (2011)
    Natural porous media such as soils or aquifers, contain colloidal particles. Depending on geochemical and hydrodynamic conditions, they can be transported by water, developing high reactivity and mobility. They may therefore ...

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