Time-dependent subgrid scales in residual-based large eddy simulation of turbulent channel flow

被引:35
作者
Gamnitzer, Peter [1 ]
Gravemeier, Volker [1 ,2 ]
Wall, Wolfgang A. [1 ]
机构
[1] Tech Univ Munich, Inst Computat Mech, D-85747 Garching, Germany
[2] Tech Univ Munich, Emmy Noether Res Grp Computat Multiscale Methods, D-85747 Garching, Germany
关键词
Large eddy simulation; Residual-based variational multiscale method; Time-dependent subscales; Turbulent channel flow; FINITE-ELEMENT-METHOD; VARIATIONAL MULTISCALE METHOD; INCOMPRESSIBLE-FLOW; NUMERICAL DISSIPATION; APPROXIMATION; FORMULATION; PROJECTION; BUBBLES; STEP;
D O I
10.1016/j.cma.2009.07.009
中图分类号
T [工业技术];
学科分类号
08 ;
摘要
The present study investigates the effect of taking into account the time dependency of the fine (subgrid) scales in a residual-based variational multiscale approach for large eddy simulation. The residual-based variational multiscale method with time-dependent (dynamic) subgrid scales is presented, and the impact of the time dependency is studied for the well-known test case of turbulent channel flow. Results are presented from computations for various values of the Reynolds number, namely Re-tau = 180, Re-tau = 395 and Re-tau = 590, and several time-step sizes. A generalized-alpha time-integration scheme is employed. Results from our numerical experiments with dynamic subgrid scales are compared to results obtained with an approximation not explicitly taking the time-dependency of the subgrid scales into account. For all Re-tau values and time-step sizes under consideration, results for resolved quantities computed by both approaches are very similar. This statement applies to both, mean streamwise velocity and root-mean-square velocity fluctuations. However, it provides a model for the subgrid-scales not depending on the time-step size and enabling a more robust representation of unresolved scales. Thus we conclude that the time-dependent subgrid-scale approximation is not capable of producing more accurate results for this type of flow if the time-step size is chosen within an optimal range. However, we expect it to be more advantageous for more complex problems, since our results indicate that it provides a more reliable representation of unresolved scales. (C) 2009 Elsevier B.V. All rights reserved.
引用
收藏
页码:819 / 827
页数:9
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