Existence and equilibration of global weak solutions to finitely extensible nonlinear bead-spring chain models for dilute polymers

Details Existence and equilibration of global weak solutions to finitely extensible nonlinear bead-spring chain models for dilute polymers Existence and equilibration of global weak solutions to finitely extensible nonlinear bead-spring chain models for dilute polymers

2010-04-08

arxiv.org/abs/1004.1432v2

Mathematical Models and Methods in Applied Sciences, Vol. 21, No. 6 (2011) 1211-1289

Mathematics

Analysis of PDEs

75 pages

Scientific paper

10.1142/S0218202511005313

We show the existence of global-in-time weak solutions to a general class of coupled FENE-type bead-spring chain models that arise from the kinetic theory of dilute solutions of polymeric liquids with noninteracting polymer chains. The class of models involves the unsteady incompressible Navier-Stokes equations in a bounded domain in two or three space dimensions for the velocity and the pressure of the fluid, with an elastic extra-stress tensor appearing on the right-hand side in the momentum equation. The extra-stress tensor stems from the random movement of the polymer chains and is defined by the Kramers expression through the associated probability density function that satisfies a Fokker-Planck-type parabolic equation, a crucial feature of which is the presence of a center-of-mass diffusion term. We require no structural assumptions on the drag term in the Fokker-Planck equation; in particular, the drag term need not be corotational. With a square-integrable and divergence-free initial velocity datum for the Navier-Stokes equation and a nonnegative initial probability density function for the Fokker-Planck equation, which has finite relative entropy with respect to the Maxwellian of the model, we prove the existence of a global-in-time weak solution to the coupled Navier-Stokes-Fokker-Planck system. It is also shown that in the absence of a body force, the weak solution decays exponentially in time to the equilibrium solution, at a rate that is independent of the choice of the initial datum and of the centre-of-mass diffusion coefficient.

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