Stochastic Modeling of Passive Scalar Transport in Turbulent Channel Flows at High Schmidt Numbers

M. Klein, H. Schmidt
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引用次数: 6

Abstract

High-Schmidt number flow simulations are challenging since the flow has to be resolved down to the Batchelor scale, which yields high resolution requirements. In order to close the gap between the flow regime of applications and that reachable by numerical simulations, we utilize a stochastic modeling approach, the so-called OneDimensional Turbulence (ODT) model. In the present study, ODT is used as stand-alone tool to investigate the turbulent transport of a passive scalar for Schmidt numbers 1 ≤ Sc ≤ 5000 in incompressible, fully-developed turbulent channel flows for Reynolds numbers Reτ ≤ 2000. The applicability of ODT is assessed by comparing the scalar mean and the root mean square fluctuations to those of reference Direct Numerical Simulations (DNS) and Large-Eddy Simulations (LES) up to Sc = 400. Good qualitative but also quantitative agreement is observed between DNS, LES, and ODT, but ODT underestimates the mean scalar concentration in the bulk by a factor of ≈ 3/4. Otherwise, ODT exhibits the correct boundary layer structure and yields the von Kármán constant for the scalar as κθ = 0.23, which corresponds well to the available reference DNS/LES. ODT is then used to simulate the scalar mass transfer coefficient K+ up to very high Schmidt numbers. The power law K ODT ∝ Sc −0.651 is obtained for Sc > 100 where it is also independent of the Reynolds number. This corresponds to the reference laboratory measurements and DNS/LES, which obey K lab ∝ Sc −0.704. The present study shows that ODT can be a versatile tool for robust and accurate modeling of the turbulent scalar transport up to very high Schmidt and Reynolds numbers.
高施密特数湍流通道中被动标量输运的随机模拟
高施密特数流动模拟具有挑战性,因为流动必须被分解到Batchelor尺度,这产生了高分辨率的要求。为了缩小应用程序的流动状态与数值模拟之间的差距,我们利用了一种随机建模方法,即所谓的一维湍流(ODT)模型。在本研究中,使用ODT作为独立工具来研究施密特数1≤Sc≤5000的被动标量在雷诺数Reτ≤2000的不可压缩、完全发育的湍流通道流动中的湍流输运。通过将标量平均值和均方根波动与参考直接数值模拟(DNS)和大涡模拟(LES)在Sc = 400范围内的波动进行比较,评估了ODT的适用性。在DNS, LES和ODT之间观察到良好的定性和定量一致,但ODT低估了块体中的平均标量浓度,约为3/4。否则,ODT表现出正确的边界层结构,标量的von Kármán常数为κθ = 0.23,与现有的参考DNS/LES很好地对应。然后使用ODT来模拟标量传质系数K+直到非常高的施密特数。当Sc > 100时,幂定律K ODT∝Sc−0.651与雷诺数无关。这对应于参考实验室测量和DNS/LES,它们服从K lab∝Sc−0.704。目前的研究表明,ODT可以作为一个通用的工具,对非常高的施密特数和雷诺数的湍流标量输运进行鲁棒和精确的建模。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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