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Direct numerical simulation of colloid transport at the microscopic scale: influence of ionic strength in the presence of a rough surface

Communication sans acte
Auteur
SEFRIOUI, Nisrine
ccAHMADI-SENICHAULT, Azita
BERTIN, Henri
17163 Transferts, écoulements, fluides, énergétique [TREFLE]
OMARI, Aziz

URI
http://hdl.handle.net/10985/9928
Date
2012

Résumé

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 simulations of the transport of a single particle near the fluid/solid interface have been performed. For this purpose, new routines have been implemented in a research code in order to take into account DLVO forces for smooth and rough pore surfaces. A dimensional analysis is performed, pointing out the important role of the ratio of electrostatic forces to the hydrodynamic forces on the particle behaviour. The test cases considered are chosen on the basis of experimental results presented in the literature. Transport of a particle near a solid surface is simulated for a given Reynolds number at different values of ionic strength and the influence of various surface roughness types are analysed. The simulations illustrate three different behaviours: (i) the particle is transported by the bulk fluid (ii) the particle is adsorbed and rolls on the solid surface (iii) the particle is adsorbed by the surface and is blocked. An analysis in terms of residence time is proposed. Simulations also show that an increase in the Reynolds number leads to the mobilisation of the particle in all cases studied.

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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 ...
  • 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. ...
  • Numerical simulation of retention and release of colloids in porous media at the pore scale 
    Article dans une revue avec comité de lecture
    SEFRIOUI, Nisrine; ccAHMADI-SENICHAULT, Azita; OMARI, Aziz; BERTIN, Henri (Elsevier, 2013)
    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 ...
  • 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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