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Breaking bore: Physical observations of roller characteristics

机译:破孔:辊子特性的物理观察

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In an estuary, a tidal bore is a hydraulic jump in translation generated at the leading edge of the flood tide during the early flood tide under spring macrotidal conditions in a narrow funnelled channel. After formation, the bore is traditionally analysed as a hydraulic jump in translation and its leading edge is characterised by a breaking roller for Fr-1 > 1.3-1.5. Herein new unsteady experiments were conducted to investigate in details the upstream propagation of breaking bore roller. The toe perimeter shape fluctuated rapidly with transverse distance and time. A characteristic transverse wave length of the toe perimeter was observed. Both the standard deviation of toe perimeter location and characteristic transverse wave length were comparable to field observations. The celerity of the roller toe fluctuated rapidly with time and space. The instantaneous longitudinal profile of the roller free-surface showed significant temporal and spatial fluctuations. Although the bore propagation may be analysed in an integral form in first approximation, the rapid fluctuations in roller toe perimeter and free-surface profiles indicated a strongly three-dimensional turbulent flow motion. (C) 2015 Elsevier Ltd. All rights reserved.
机译:在河口,潮汐孔是在春季大潮条件下,在狭窄的漏斗形通道中,在早期洪水期间在洪水潮的前缘产生的水力跃迁。形成孔之后,通常将孔分析为平移中的水力跃迁,并且其前缘的特征是对于Fr-1> 1.3-1.5的折断辊。在此进行了新的非稳态实验,以详细研究破孔辊的上游传播。脚趾周长形状随横向距离和时间而快速波动。观察到脚趾周长的特征性横向波长。脚趾周长位置的标准偏差和特征横波长度都可以与现场观察相媲美。脚趾的速度随时间和空间快速波动。滚子自由表面的瞬时纵向轮廓显示出明显的时间和空间波动。尽管可以近似近似地分析孔的传播,但辊趾周长和自由表面轮廓的快速波动表明存在强烈的三维湍流运动。 (C)2015 Elsevier Ltd.保留所有权利。

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