Recent progress in the development of the Elliptic Blending Reynolds-stress model

• Published in: The International journal of heat and fluid flow Vol. 51; pp. 195 - 220
• Main Author: Manceau, Rémi
• Format: Journal Article
• Language: English
• Published: Elsevier Inc 01.02.2015; Elsevier
• Subjects: Blending; Channel flow; Computational fluid dynamics; Engineering Sciences; Fluid flow; Mathematical models; Near-wall turbulence; Reactive fluid environment; Reproduction; Reynolds stress; Rotating flows; Second-moment closure; Turbulence; Turbulence modelling; Turbulent flow; Near-wall turbulence; Rotating flows; Second-moment closure; Turbulence modelling
• ISSN: 0142-727X; 1879-2278; 1879-2278
• DOI: 10.1016/j.ijheatfluidflow.2014.09.002

•Various modifications of the Elliptic Blending Reynolds stress model, proposed during the last decade, are revisited.•Using theoretical arguments and detailed comparison with DNS data, a reference model is formulated.•The model satisfactorily reproduces the effects of spanwise rotation on turbulence, for cases without and with separation. The Elliptic Blending Reynolds Stress Model (EB-RSM), originally proposed by Manceau and Hanjalić (2002) to extend standard, weakly inhomogeneous Reynolds stress models to the near-wall region, has been subject to various modifications by several authors during the last decade, mainly for numerical robustness reasons. The present work revisits all these modifications from the theoretical standpoint and investigates in detail their influence on the reproduction of the physical mechanisms at the origin of the influence of the wall on turbulence. The analysis exploits recent DNS databases for high-Reynolds number channel flows, spanwise rotating channel flows with strong rotation rates, up to complete laminarization, and the separated flow after a sudden expansion without and with system rotation. Theoretical arguments and comparison with DNS results lead to the selection of a recommended formulation for the EB-RSM model. This formulation shows satisfactory predictions for the configurations described above, in particular as regards the modification of the mean flow and turbulent anisotropy on the anticyclonic or pressure side.