2013
DOI: 10.1007/s11242-013-0263-6
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Slow Motion of a Porous Sphere Translating Along the Axis of a Circular Cylindrical Pore Subject to a Stress Jump Condition

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Cited by 13 publications
(5 citation statements)
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“…The review of the known analytical solutions and basic applications of the micropolar liquids are given in Khanukaeva and Filippov. 6 Using the numerical techniques, Saad and Faltas 7 solved the coupled flow problem of an incompressible viscous fluid flow over a porous sphere located in a circular cylindrical pore and calculated the normalized hydrodynamic drag of the porous particle. Using linear slip and Basset-type boundary conditions, the motion of a solid spherical particle in an incompressible axisymmetric micropolar Stokes flow was investigated by Faltas and Saad 8,9 for two cases: perpendicular translation to the free surface and rotation about a diameter which is also perpendicular to the free surface and parallel translation to the free surface and rotation about a diameter which is lying in the free surface.…”
Section: Introductionmentioning
confidence: 99%
“…The review of the known analytical solutions and basic applications of the micropolar liquids are given in Khanukaeva and Filippov. 6 Using the numerical techniques, Saad and Faltas 7 solved the coupled flow problem of an incompressible viscous fluid flow over a porous sphere located in a circular cylindrical pore and calculated the normalized hydrodynamic drag of the porous particle. Using linear slip and Basset-type boundary conditions, the motion of a solid spherical particle in an incompressible axisymmetric micropolar Stokes flow was investigated by Faltas and Saad 8,9 for two cases: perpendicular translation to the free surface and rotation about a diameter which is also perpendicular to the free surface and parallel translation to the free surface and rotation about a diameter which is lying in the free surface.…”
Section: Introductionmentioning
confidence: 99%
“…The solution of the external and internal flow of the porous particle in spherical coordinates can be expressed using the stream functions (Saad & Faltas 2014):…”
Section: Solution Based On Stream Functionmentioning
confidence: 99%
“…By substituting the stream function given by (2.19) into (2.56), we can obtain the simple relation (Saad & Faltas 2014):…”
Section: Drag Force and Velocities Of Particlesmentioning
confidence: 99%
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“…Using the ratio of pore size to the macroscopic length scale as a small parameter, the dominant jump conditions are found at the first order, and the generality of such asymptotic analysis allows them to make direct comparison with several pre-existing models such as the pioneering slip model by Beavers and Joseph 21 . It is worth mentioning that the approach adopted by Angot et al [22][23][24] was suggested by Worster et al 25,26 , where the empirical formula for the jump boundary conditions is similar to those used and/or derived in many other works [27][28][29][30][31][32][33][34][35][36][37] .…”
Section: Introductionmentioning
confidence: 99%