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Results and discussion Samples and simulation technique Sébastien Vincent-Bonnieu, Reinhard Höhler, Sylvie Cohen-Addad Recent experiments have shown that 3D coarsening aqueous foams respond to a small constant shear stress by a creep deformation that linearly increases with time [1]. Moreover, in situ light scattering studies have shown that this phenomenon scales linearly with the rate of coarsening induced intermittent local bubble rearrangements. These findings are in qualitative agreement with 2D numerical foam simulations by Kermode et al [2] which demonstrate that coarsening leads to a viscoelastic relaxation. However, this pioneering work only has proved the existence of this effect, and a systematic quantitative analysis such as the one presented here has not been published to our knowledge. [1] Cohen-Addad S., Höhler R., Khidas Y. Interplay between interfacial rheology, bubble rearrangements and the slow macroscopic rheological response of aqueous foam. Abstract to EUFOAM [2] Weaire D., Hutzler S.: The Physics of Foams, Oxford University Press, New York Creep in 3D foam: Experimental results* Light scattering data suggest that linear viscoelastic creep is the consequence of coarsening induced bubble rearrangements*. Aim of this 2D simulation study: Clarify the creep mechanism on the bubble scale. Experiment: Strain response (t) to an imposed stress. 0 Steady creep Yield stress Time * Cohen-Addad, Höhler, Khidas, Phys. Rev. Lett. in press stress Can these rearrangements explain macroscopic creep ? Origin of coarsening: Differences in Laplace pressure drive gas transfer between bubbles. T2 & T1 events T2 event T1 event This coarsening induces rearrangements : or Coarsening provokes topological changes Numerical simulation creep using the surface evolver For our simulations diffusion constant = Find structure of minimal energy Make T1 or T2 rearrangements if necessary Transfer gas between bubbles during time t Adjust strain to maintain an imposed stress t T Gas diffusion and numerical convergence occur simultaneously. The diffusion constant must be chosen small enough to ensure quasistatic conditions. Strain-jumps de correspond to T1 time Shear strain de Yield stress The onset of creep depends on the initial foam structure. Strain evolution between jumps Strain-jump Strain evolution between successive rearrangements does not contribute to macroscopic creep. Full agreement with experimental data (Cohen-Addad et al, abstract to EUFOAM 2004) The strain-jump scales linearly with stress on the average. Average over 10 samples We have studied creep in 2D disordered coarsening dry foams using the Surface Evolver software. This work shows that: The mechanism of steady creep on the bubble scale is strain relaxation via coarsening induced T1 rearrangements. Using the simulation results, we have validated a schematic mesoscopic model of creep based on continuum mechanics. Our findings are in good agreement with recent experimental results. Conclusions Mesoscopic model of the steady creep Hypothesis: upon a rearrangement in an area fraction f, foam locally and temporarily looses its elasticity. Under constant stress s, this leads to an increase of macroscopic strain de, as if the macroscopic shear modulus G were reduced: Since we observe in the simulations that most rearrangements involve 4 bubbles, one would expect 4 / 50 This is in rough agreement with the simulation data: Periodic boundary conditions µ 2 = second central moment of the distribution of bubble coordination numbers, a measure of disorder At the end of sample preparation, shear and normal stresses are relaxed 100 bubbles Three types of 2D model systems Voronoi Coarsened Relaxed Minimize energy using the Surface Evolver Coarsening Shear Voronoi Sheared Relaxed 50 bubbles m 2 = bubbles m 2 =1.12 Voronoi Relaxed 50 bubbles m 2 =1.5 Introduction Voronoi Relaxed 0 s = 0.12 s = 0.15 Voronoi Relaxed stress 1 sample Average over 10 samples The Rheology of Coarsening 2d Dry Foams: A Numerical Simulation Study The Rheology of Coarsening 2d Dry Foams: A Numerical Simulation Study

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