Viscoelastic flow instability in planar shear flow

We report direct numerical simulations of elastic turbulence in shear-driven flow of a dilute polymer solution within a three-dimensional straight channel. Most existing approaches in the literature employ the Oldroyd-B model or its advanced version, the finite extensible nonlinear elastic model int...

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Detalles Bibliográficos
Autores: Novikau S., Ivan, Kantorovich S., Sofia, Altmeyer, Sebastian Andreas|||0000-0001-5964-0203
Tipo de recurso: artículo
Fecha de publicación:2025
País:España
Institución:Universitat Politècnica de Catalunya (UPC)
Repositorio:UPCommons. Portal del coneixement obert de la UPC
Idioma:inglés
OAI Identifier:oai:upcommons.upc.edu:2117/441268
Acceso en línea:https://hdl.handle.net/2117/441268
https://dx.doi.org/10.1063/5.0261021
Access Level:acceso abierto
Palabra clave:Molecular dynamics
Elastic waves
Mathematical crystallography
Polymer chemistry
Finitely extensible nonlinear elastic
Non Newtonian fluids
Viscoelastic flows
Flow instabilities
Fluid flows
Hydrodynamics
Àrees temàtiques de la UPC::Física::Física de fluids::Flux de fluids
Àrees temàtiques de la UPC::Aeronàutica i espai::Aerodinàmica
Descripción
Sumario:We report direct numerical simulations of elastic turbulence in shear-driven flow of a dilute polymer solution within a three-dimensional straight channel. Most existing approaches in the literature employ the Oldroyd-B model or its advanced version, the finite extensible nonlinear elastic model introduced by Peterlin (FENE-P model), for simulation of polymer hydrodynamics, with their limitations of being continuum models. To overcome such restriction, we explicitly model the dilute polymer solution utilizing a classical bead-spring representation for each polymer chain and, therefore, also accounting for spatial variations in polymer concentration. We show that the viscoelastic instability forms in elastic waves and eventually chaotic flow, which persists above the transition with increasing Weissenberg number further into viscoelastic turbulence.