Published June 1991 | Version v1
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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 marche

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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