Stress diffusion in shear banding wormlike micelles

被引:28
|
作者
Fardin, Marc-Antoine [1 ,5 ]
Radulescu, Ovidiu [2 ]
Morozov, Alexander [3 ]
Cardoso, Olivier [4 ,5 ]
Browaeys, Julien [4 ,5 ]
Lerouge, Sandra [4 ,5 ]
机构
[1] Univ Paris Diderot, CNRS UMR 7592, Inst Jacques Monod, F-75205 Paris 13, France
[2] Univ Montpellier 2, UMR 5235, Dynam Interact Membranaires Normales & Pathol, F-34095 Montpellier 5, France
[3] Univ Edinburgh, Sch Phys & Astron, SUPA, JCMB, Edinburgh EH9 3FD, Midlothian, Scotland
[4] Univ Paris Diderot, CNRS UMR 7057, Lab Mat & Syst Complexes, F-75205 Paris 13, France
[5] Acad Bradylogists, Paris, France
基金
欧洲研究理事会; 英国工程与自然科学研究理事会;
关键词
INDUCED PHASE-SEPARATION; JOHNSON-SEGALMAN MODEL; ELASTIC INSTABILITIES; COMPLEX FLUIDS; TAYLOR-COUETTE; FLOW; RHEOLOGY; DYNAMICS; TRANSITIONS; INTERFACE;
D O I
10.1122/1.4930858
中图分类号
O3 [力学];
学科分类号
08 ; 0801 ;
摘要
In order to deal with strong inhomogeneities of the polymer stress in shear banding of wormlike micelles, rheological models usually include stress diffusion terms. These terms lift the degeneracy of steady flow solutions by selecting the steady-state positions of interfaces between bands and the values of the total mechanical stress. They are also responsible for slow transients of interface kinetics under imposed step shear flow. In our previous experiments, we estimated the typical lengthscale associated with these terms to be of the order of several nanometers, while several other experiments obtained significantly larger estimates. We report here a new set of experiments that reconcile our previous work with the rest of the literature and obtain a diffusive lengthscale of order of a few micrometers. Surprisingly, we find that this lengthscale is a strong function of the applied shear rate, decreasing rapidly across the stress plateau. We perform numerical simulations of several constitutive equations used to model shear-banded flows and conclude that they cannot predict this behavior. We argue that the strong dependence of the diffusive lengthscale on the applied shear rate should be incorporated into the classical constitutive models to obtain quantitative predictions. (C) 2015 The Society of Rheology.
引用
收藏
页码:1335 / 1362
页数:28
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