Skip to main content Accessibility help
×
Hostname: page-component-848d4c4894-wg55d Total loading time: 0 Render date: 2024-04-30T15:01:00.509Z Has data issue: false hasContentIssue false

4 - Remarks on complex fluid models

Published online by Cambridge University Press:  05 November 2012

P. Constantin
Affiliation:
Princeton University
James C. Robinson
Affiliation:
University of Warwick
José L. Rodrigo
Affiliation:
University of Warwick
Witold Sadowski
Affiliation:
Uniwersytet Warszawski, Poland
Get access

Summary

Abstract We review recent global existence and uniqueness results of solutions for models of complex fluids in ℝd. We describe results concerning the Oldroyd-B and related models.

Introduction

Complex fluids are ubiquitous in nature and manifest a rather large number of different behaviours. There is no single accepted general model for all these, and the presence of a large array of complicated models is an indication of the difficulties encountered at a fundamental level. In this article I will describe some of the mathematical issues. A complex fluid is a mixture between a solvent, which is treated as a normal fluid, and particulate matter in it. The particles are sufficiently many and sufficiently small compared to the characteristic scales of the motions of the solvent, so that one may hope for a description that does not have to resolve the fluid mechanical problem of flow past the particles. The particles themselves are treated in a simplified manner as objects m ∈ M, where M is a finite-degrees-of-freedom configuration space accounting for the salient features of the particles. For instance M can be a subset of ℝN or a more complicated metric space. Models have been devised to deal with microscopic elastic thread-like objects such as polymers (Doi & Edwards, 1998, Öttinger, 1996). The complicated hydrodynamic interactions are simplified using the separation of scales, replacing the many degrees of freedom due to them by a few representative ones.

Type
Chapter
Information
Publisher: Cambridge University Press
Print publication year: 2012

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

Barrett, J.W., Schwab, C., & Süli, E. (2010) Existence and equilibration of global weak solutions to finitely extensible nonlinear bead-spring chain models for dilute polymers, preprint 2010.
Chemin, J.-Y. & Masmoudi, N. (2001) About lifespan of regular solutions of equations related to viscoelastic fluids. SIAM J. Math. Anal. 33, 84–112.Google Scholar
Constantin, P. (2005) Nonlinear Fokker–Planck Navier–Stokes Systems. Commun. Math. Sci. 3, 531–544.Google Scholar
Constantin, P. (2007) Smoluchowski Navier–Stokes systems, in Contemporary Mathematics 429 G-Q, ChenE., HsuM., Pinsky editors, AMS, Providence, 85–109.
Constantin, P. (2010) The Onsager equation for corpora. Journal of Computational and Theoretical Nanoscience 7 (4), 675–682.Google Scholar
Constantin, P., Fefferman, C., Titi, E., & Zarnescu, A. (2007) Regularity for coupled two-dimensional nonlinear Fokker–Planck and Navier–Stokes systems. Commun. Math. Phys. 270, 789–811.Google Scholar
Constantin, P. & Masmoudi, N. (2008) Global well-posedness for a Smoluchowski equation coupled with Navier–Stokes equations in 2D. Commun. Math. Phys. 278, 179–191.Google Scholar
Constantin, P. & Seregin, G. (2010a) Hölder Continuity of Solutions of 2D Navier–Stokes Equations with Singular Forcing. In Nonlinear partial differential equations and related topics, Amer. Math. Soc. Transl. Ser. 2, 229, Amer. Math. Soc., Providence, Rhode Island, USA
Constantin, P. & Seregin, G. (2010b) Global regularity of solutions of coupled Navier–Stokes equations and nonlinear Fokker–Planck equations. DCDSA 26, 1185–1186.Google Scholar
Constantin, P. & Sun, W. (2012) Remarks on Oldroyd-B and Related Complex Fluid Models. Comm. Math. Sciences, 10, 33–73.Google Scholar
Constantin, P. & Zlatos, A. (2010) On the high intensity limit of interacting corpora. Comm. Math. Sciences 8, 173–186.Google Scholar
Doi, M. & Edwards, S.F. (1998) The Theory of Polymer Dynamics. Oxford University Press, Oxford.
Guillopé, C. & Saut, J.-C. (1990) Existence results for the flow of viscoelastic fluids with a differential constitutive law. Nonlinear Anal. 15, 849–869.Google Scholar
Kupferman, R., Mangoubi, C., & Titi, E. (2008) A Beale–Kato–Majda breakdown criterion for an Oldroyd-B fluid in the creeping flow regime. Commun. Math. Sciences 6, 235–256.Google Scholar
LeBris, C. & Lelièvre, T. (2009) Multiscale modelling of complex fluids: a mathematical initiation. In Multiscale modelling and simulation in science. Lect. Notes Comput. Sci. Eng. 66, Springer, Berlin.
Lei, Z. & Zhou, Y. (2005) Global existence of classical solutions for the twodimensional Oldroyd model via the incompressible limit. SIAM. J. Math. Anal. 37, 797–814.Google Scholar
Lei, Z., Masmoudi, N., & Zhou, Y. (2010) Remarks on the blowup criteria for Oldroyd models. J. Diff. Eqns. 248, 328–341.Google Scholar
Lin, F., Liu, C., & Zhang, P. (2005) On hydrodynamics of viscoelastic fluids. Comm. Pure Appl. Math 58, 1437–1471.Google Scholar
Lin, F., Liu, C., & Zhang, P. (2007) On a micro-macro model for polymeric fluids near equilibrium. Comm. Pure Appl. Math 60, 838–866.Google Scholar
Lin, F., Zhang, P., & Zhang, Z. (2008) On the global existence of smooth solution to the 2D FENE dumbbell model. Commun. Math. Phys. 277, 531–553.Google Scholar
Lions, P.-L. & Masmoudi, N. (2007) Global existence of weak solutions to some micro-macro models. C.R. Acad. Sci. Paris 345, 131–141.Google Scholar
Lions, P.-L. & Masmoudi, N. (2000) Global solutions for some Oldroyd models of non-Newtonian flows. Chinese Ann. Math. Ser.B 21, 131–146.Google Scholar
Masmoudi, N. (2010) Global existence of weak solutions to the FENE dumbbell model of polymeric flows, preprint.
Masmoudi, N., Zhang, P., & Zhang, Z. (2008) Global well-posedness for 2D polymeric fluid models and growth estimate. Phys.D 237, 1663–1675.Google Scholar
Öttinger, H. C. (1996) Stochastic processes in polymeric fluids, Springer-Verlag, Berlin.
Otto, F. & Tzavaras, A.E. (2008) Continuity of velocity gradients in suspensions of rod-like molecules. Comm. Math. Phys. 277, 729–758.Google Scholar
Renardy, M. (1991) An existence theorem for model equations resulting from kinetic theories of polymer solutions. SIAM J. Math. Anal. 22, 3131–327.Google Scholar
Thomases, B. & Shelley, M. (2007) Emergence of singular structures in Oldroyd-B fluids. Phys. Fluids 19.Google Scholar
Thomases, B. (2011) An analysis of the effect of stress diffusion on the dynamics of creeping viscoelastic flow. J. Non-Newtonian Fluid Mech. 166, 1221–1228Google Scholar

Save book to Kindle

To save this book to your Kindle, first ensure coreplatform@cambridge.org is added to your Approved Personal Document E-mail List under your Personal Document Settings on the Manage Your Content and Devices page of your Amazon account. Then enter the ‘name’ part of your Kindle email address below. Find out more about saving to your Kindle.

Note you can select to save to either the @free.kindle.com or @kindle.com variations. ‘@free.kindle.com’ emails are free but can only be saved to your device when it is connected to wi-fi. ‘@kindle.com’ emails can be delivered even when you are not connected to wi-fi, but note that service fees apply.

Find out more about the Kindle Personal Document Service.

Available formats
×

Save book to Dropbox

To save content items to your account, please confirm that you agree to abide by our usage policies. If this is the first time you use this feature, you will be asked to authorise Cambridge Core to connect with your account. Find out more about saving content to Dropbox.

Available formats
×

Save book to Google Drive

To save content items to your account, please confirm that you agree to abide by our usage policies. If this is the first time you use this feature, you will be asked to authorise Cambridge Core to connect with your account. Find out more about saving content to Google Drive.

Available formats
×