大涡模拟的混合模式:单层和双层最小耗散- bardina模式

L. B. Streher, M. H. Silvis, P. Cifani, R. Verstappen
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引用次数: 2

摘要

利用大涡模拟预测湍流的行为需要对亚网格尺度应力张量进行建模。这个张量可以用混合模型来近似,混合模型结合了功能模型的耗散性质和结构模型近似非平衡效应的能力。然而,现有的混合模型是基于模型的线性组合,缺乏数学动机。因此,我们提出了一个数学基础来混合(功能的)涡流黏度模型和(结构的)Bardina模型。用这种方法得到了混合各向异性最小耗散(AMD) -Bardina模型。为了获得符合物理条件的壁面流动模型,我们进一步将该混合模型发展为两层方法:近壁面区域用AMD-Bardina模型参数化,而外壁面区域用Bardina模型计算。对原始和双层AMD-Bardina模型在不同雷诺数下的湍流通道流动进行了测试,与单独使用AMD和Bardina模型的计算相比,混合模型的预测结果得到了改进。用两层AMD-Bardina模型获得的结果特别显著:一阶和二阶统计量都得到了非常好的预测,甚至捕获了通道中心平均速度的变化。由此,获得了一种非常有前途的中、高雷诺数湍流通道大涡模拟模型。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Mixed modeling for large-eddy simulation: The single-layer and two-layer minimum-dissipation-Bardina models
Predicting the behavior of turbulent flows using large-eddy simulation requires modeling of the subgrid-scale stress tensor. This tensor can be approximated using mixed models, which combine the dissipative nature of functional models with the capability of structural models to approximate out-of-equilibrium effects. The currently existing mixed models, however, are based on ad hoc linear combinations of models and lack mathematical motivation. We, therefore, propose a mathematical basis to mix (functional) eddy-viscosity models with the (structural) Bardina model. With this methodology we obtain the mixed anisotropic minimum-dissipation (AMD) -Bardina model. In order to also obtain a physics-conforming model for wall-bounded flows, we further develop this mixed model into a two-layer approach: the near-wall region is parameterized with the AMD-Bardina model, whereas the outer region is computed with the Bardina model. The original and two-layer AMD-Bardina models are tested in turbulent channel flows at various Reynolds numbers, and improved predictions are obtained when the mixed models are applied in comparison to the computations with the AMD and Bardina models alone. The results obtained with the two-layer AMD-Bardina model are particularly remarkable: both first- and second-order statistics are extremely well predicted and even the inflection of the mean velocity in the channel center is captured. Hence, a very promising model is obtained for large-eddy simulations of turbulent channel flows at moderate and high Reynolds numbers.
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