A low-dissipation finite element scheme for scale resolving simulations of turbulent flows

The present work extends the conservative convective scheme proposed by Charnyi et al. (2017) [13], originally formulated for mixed finite elements and tested in laminar flows, to equal order finite elements. A non-incremental fractional-step method is used to stabilise pressure, allowing the use of...

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Detalles Bibliográficos
Autores: Lehmkuhl Barba, Oriol|||0000-0002-2670-1871, Houzeaux, Guillaume|||0000-0002-2592-1426, Owen, Herbert, Chrysokentis, Giorgios, Rodríguez Pérez, Ivette María|||0000-0002-3749-277X
Tipo de recurso: artículo
Fecha de publicación:2019
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:2117/132321
Acceso en línea:https://hdl.handle.net/2117/132321
https://dx.doi.org/10.1016/j.jcp.2019.04.004
Access Level:acceso abierto
Palabra clave:Turbulence--Computer simulation
Eddies
Finite element method
Finite elements
Low-dissipation schemes
Turbulent flows
Large-eddy simulation
Direct numerical simulation
Turbulència -- Simulació numèrica
Remolins (Mecànica de fluids)
Elements finits, Mètode dels
Àrees temàtiques de la UPC::Enginyeria mecànica::Mecànica de fluids
Descripción
Sumario:The present work extends the conservative convective scheme proposed by Charnyi et al. (2017) [13], originally formulated for mixed finite elements and tested in laminar flows, to equal order finite elements. A non-incremental fractional-step method is used to stabilise pressure, allowing the use of finite element pairs that do not satisfy the inf-sup conditions, such as equal order interpolation for the velocity and pressure used in this work. The final scheme preserves momentum and angular momentum at the discrete level; the error in the conservation of kinetic energy introduced by this stabilisation is of O (dt,h^2) in the case of linear finite elements. The low dissipation strategy is tested on a set of relevant turbulent cases. First, by using direct numerical simulation on the inviscid and viscous Taylor-Green vortex problem at Re =1600 and later, coupled with the Vreman (2004) [25]sub-grid stress model for performing large-eddy simulations on a turbulent channel flow at Ret=950, the flow past a sphere at ReD=10^4 and the flow around an Ahmed body at ReH=2 ×10^5. In all cases the performance of the presented formulation is fairly good and it has been capable of reproducing the reference results with good accuracy.