Abstract
The non-smooth motion of a single foam lamella traversing an idealised rock pore can lead to a significant pressure drop. We vary two parameters defining the shape of a biconical pore in two dimensions, and use Surface Evolver simulations and geometric arguments to demarcate the four different types of possible motion. We predict the transitions between different-shaped pores in which the lamella makes a symmetric or an asymmetric jump, an asymmetric crawl, or undergoes smooth motion. We give the time-averaged pressure drop as a function of pore shape. (C) 2013 Elsevier B.V. All rights reserved.
Original language | English |
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Pages (from-to) | 56-62 |
Number of pages | 7 |
Journal | Colloids and Surfaces A: Physicochemical and Engineering Aspects |
Volume | 438 |
Early online date | 21 Feb 2013 |
DOIs | |
Publication status | Published - 05 Dec 2013 |
Keywords
- Foam
- Porous media
- Surface Evolver
- Pressure drop
- MOBILIZATION PRESSURE-GRADIENT
- POROUS-MEDIA
- FLOWING FOAMS
- VISCOSITY
- CHANNELS
- FILMS
- TUBES