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Large-scale turbulent structure of uniform shallow free-surface flows

机译:均匀的浅自由表面流的大型湍流结构

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The hydrodynamics of super- and sub-critical shallow uniform free-surface flows are assessed using laboratory experiments aimed at identifying and quantifying flow structure at scales larger than the flow depth. In particular, we provide information on probability distributions of horizontal velocity components, their correlation functions, velocity spectra, and structure functions for the near-water-surface flow region. The data suggest that for the high Froude number flows the structure of the near-surface layer resembles that of two-dimensional turbulence with an inverse energy cascade. In contrast, although large-scale velocity fluctuations were also present in low Froude number flow its behaviour was different, with a direct energy cascade. Based on our results and some published data we suggest a physical explanation for the observed behaviours. The experiments support Jirka's [Jirka GH (2001) J Hydraul Res 39(6):567-573] hypothesis that secondary instabilities of the base flow may generate large-scale two-dimensional eddies, even in the absence of transverse gradients in the time-averaged flow properties.
机译:使用实验室实验评估超临界和亚临界浅均匀自由表面流体的流体力学,该实验旨在识别和量化大于流动深度的尺度的流动结构。特别是,我们提供了有关水平速度分量的概率分布,它们的相关函数,速度谱以及近水面流域结构函数的信息。数据表明,对于较高的弗洛德数流,近表面层的结构类似于具有逆能量级联的二维湍流。相反,尽管在低Froude数流中也存在大规模速度波动,但其行为却有所不同,具有直接能量级联。根据我们的结果和一些公开的数据,我们建议对观察到的行为进行物理解释。实验支持Jirka [Jirka GH(2001)J Hydraul Res 39(6):567-573]的假设,即即使当时没有横向梯度,基流的次要不稳定性也可能产生大规模的二维涡流。平均流量特性。

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