A fictitious domain/distributed Lagrange multiplier method for the particulate flow of Oldroyd-B fluids: A positive definiteness preserving approach

被引:34
作者
Hao, Jian [1 ]
Pan, Tsorng-Whay [1 ]
Glowinski, Roland [1 ]
Joseph, Daniel D. [2 ]
机构
[1] Univ Houston, Dept Math, Houston, TX 77204 USA
[2] Univ Minnesota, Dept Aerosp Engn & Mech, Minneapolis, MN 55455 USA
关键词
Oldroyd-B fluid; Positive definiteness; Fictitious domain; Particulate flow; Finite element; Operator splitting; INCOMPRESSIBLE VISCOUS-FLOW; MOVING RIGID BODIES; DIRECT SIMULATION; DOMAIN METHOD; NUMERICAL-SIMULATION; DYNAMIC SIMULATION; POISEUILLE FLOW; SEDIMENTATION; PARTICLES; MOTION;
D O I
10.1016/j.jnnfm.2008.07.006
中图分类号
O3 [力学];
学科分类号
08 ; 0801 ;
摘要
In this article we present a numerical method for simulating the sedimentation of circular particles in a two-dimensional channel filled with an Oldroyd-B fluid. We have combined a fictitious domain/distributed Lagrange multiplier method with a factorization approach from Lozinski and Owens [J. Non-Newtonian Fluid Mech. 112 (2003) 161] via an operator splitting technique. The new scheme preserves the positive definiteness of the conformation tensor at the discrete level. The method is validated by performing a convergence Study which shows that the results are independent of the mesh and time step sizes. Our results show that when the elasticity number(E) is less than a critical value (which depends upon the blockage ratio), two particles will sediment in the channel-like particles in Newtonian fluids; when the elasticity number is greater than the critical value, chains are formed for the case of two particles sedimenting in an Oldroyd-B fluid and the center line is aligned with the falling direction. These results agree with those presented in [P.Y. Huang, H.H. Hu, and D.D. Joseph, J. Fluid Mech. 362 (1998) 297]. For the cases of three and six particles, when the elasticity number is greater than a critical value and the viscoelastic Mach number is less than one, chains are also formed and move to the center of the channel. (c) 2008 Elsevier B.V. All rights reserved.
引用
收藏
页码:95 / 111
页数:17
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