Numerical simulation of complex turbulent Flow over a backward-facing step
Description
A statistical and topological study of a complex turbulent flow over a backward-facing step is realized by means of Direct and Large-Eddy Simulations. Direct simulations are performed in an isothermal and in a stratified two-dimensional case. In the isothermal case coherent structures have been obtained by the numerical simulation in the mixing layer downstream of the step. In a second step a thermal stratification is imposed on this flow. The coherent structures are in this case produced in the immediate vicinity of the step and disappear dowstream for increasing stratification. Afterwards, large-eddy simulations are carried out in the three-dimensional case. The subgrid-scale model is a local adaptation to the physical space of the spectral eddy-viscosity concept. The statistics of turbulence are in good agreement with the experimental data, corresponding to a small step configuration. Furthermore, calculations at higher step configuration show that the eddy structure of the flow presents striking analogies with the plane shear layers, with large billows shed behind the step, and intense longitudinal vortices strained between these billows
Availability note (English)
MF available from INIS under the Report Number.Abstract (French)
Une etude statistique et topologique d'un ecoulement turbulent complexe en aval d'une marche descendante a ete realisee au moyen des techniques de Simulation Directe et de Simulation des Grandes Echelles. Nous avons mis en evidence la formation des structures coherentes qui composent la couche de melange bidimensionnelle. On a aussi etudie l'influence d'une stratification stable sur la couche de melange. Dans ce cas, on montre comment la gravite inhibe la croissance de la couche de melange, et l'apparition d'ondes de gravite internes. La Simulation Directe a ete utilisee dans ce cas. Les ecoulements tridimensionels ont ete etudies a l'aide de la Simulation des Grandes Echelles. Dans ce cas le modele sous-maille est une adaptation locale dans l'espace physique du concept de viscosite turbulente dans l'espace de Fourier. La statistique de la turbulence est validee au moyen des resultats experimentaux correspondants a une marche petite. Des calculs supplementaires sur une marche haute ont permis l'etude topologique des instabilites primaires et secondaires liees a la couche de melange en aval de la marcheFiles
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Additional details
Additional titles
- Original title (French)
- Simulation numerique des grandes echelles d'un ecoulement turbulent decolle en aval d'une marche
Publishing Information
- Imprint Pagination
- 171 p.
- Report number
- FRCEA-TH--344
INIS
- Country of Publication
- France
- Country of Input or Organization
- France
- INIS RN
- 23011553
- Subject category
- S42: ENGINEERING;
- Resource subtype / Literary indicator
- Thesis
- Descriptors DEI
- SIMULATION; THREE-DIMENSIONAL CALCULATIONS; TOPOLOGICAL MAPPING; TURBULENT FLOW; TWO-DIMENSIONAL CALCULATIONS; VORTICES
- Descriptors DEC
- FLUID FLOW; TRANSFORMATIONS