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Physical modelling of breaking tidal bores: comparison with prototype data

机译:破潮洞的物理模型:与原型数据的比较

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A tidal bore is a hydraulic jump in translation, propagating upstream as the tide turns to rising and the flood flow advances in a funnel-shaped river mouth under spring tide conditions. This study focused on the unsteady turbulence induced by a breaking tidal bore. Detailed free-surface and velocity measurements were conducted with a high temporal resolution using non-intrusive free-surface measurement probes and acoustic Doppler velocimetry sampled at 200 Hz. The laboratory data were systematically compared with an earlier series of field measurements conducted in the breaking bore of the Selune River (France). Key findings include the agreement, in terms of dimensionless instantaneous free-surface and velocity data, between laboratory and field observations as well as the existence of a transient recirculation region near the bed.
机译:潮汐孔是水力平移,在潮汐条件下,随着潮汐转向上升,洪水在上游呈漏斗状的河口传播。这项研究的重点是潮汐孔破裂引起的不稳定湍流。使用非侵入式自由表面测量探头和以200 Hz采样的声学多普勒测速仪,可以在高时间分辨率下进行详细的自由表面和速度测量。系统地将实验室数据与在塞鲁内河(法国)的破洞处进行的一系列较早的现场测量进行了比较。主要发现包括在实验室和野外观测之间就无因次瞬时自由表面和速度数据达成一致,以及在床附近存在一个瞬态再循环区域。

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