Experimental and numerical study of the rotation and the erosion of fillers suspended in viscoelastic fluids under simple shear flow

• Published in: Rheologica acta 2003-09, Vol.42 (5), p.421-431
• Main Authors: ASTRUC, Marianne, VERVOORT, Sylvie, NOUATIN, Hervé O, COUPEZ, Thierry, DE PUYDT, Yves, NAVARD, Patrick, PEUVREL-DISDIER, Edith
• Format: Article
• Language: English
• Subjects: Agglomerates; Agglomeration; Applied sciences; Axis movements; Carbon black; Compounding ingredients; Computational fluid dynamics; Computer simulation; Elasticity; Engineering Sciences; Erosion; Exact sciences and technology; Fillers; Fillers and reinforcing agents; Finite element method; Fluid flow; Fluids; Materials; Mathematical models; Polymer industry, paints, wood; Rotation; Shear flow; Size reduction; Technology of polymers; Viscoelastic fluids; Viscoelasticity; Vorticity
• ISSN: 0035-4511; 1435-1528
• DOI: 10.1007/s00397-003-0296-9

When a porous agglomerate immersed in a fluid is submitted to a shear flow, hydrodynamic stresses acting on its surface may cause a size reduction if they exceed the cohesive stress of the agglomerate. The aggregates forming the agglomerate are slowly removed from the agglomerate surface. Such a behaviour is known when the suspending fluid is Newtonian but unknown if the fluid is viscoelastic. By using rheo-optical tools, model fluids, carbon black agglomerates and particles of various shapes, we found that the particles had a rotational motion around the vorticity axis with a period which is independent on shape (flat particles not considered), but which is exponentially increasing with the elasticity of the medium expressed by the Weissenberg number (We). Spherical particles are always rotating for We up to 2.6 (largest investigated We in this study) but elongated particles stop rotating for We>0.9 while orienting along the flow direction. Erosion is strongly reduced by elasticity. Since finite element numerical simulation shows that elasticity increases the local stress around a particle, the origin of the erosion reduction is interpreted as an increase of cohesiveness of the porous agglomerate due to the infiltration of a viscoelastic fluid.