首页> 外文会议>International Conference on Coastal Dynamics >DEPTH OF SAND ACTIVATION ON PROTECTED AND NON-PROTECTED NOURISHED BEACHES: A LABORATORY STUDY IN A LARGE-SCALE WAVE FLUME
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DEPTH OF SAND ACTIVATION ON PROTECTED AND NON-PROTECTED NOURISHED BEACHES: A LABORATORY STUDY IN A LARGE-SCALE WAVE FLUME

机译:受保护和非保护营养海滩的沙子激活深度:大规模波浪的实验室研究

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The depth of sand activation on a beach under the action of waves is a key parameter for many scientific and applied projects in coastal engineering. Although there is a good literature on field studies, the work presented here represents the first laboratory study of its kind. Two nourished beaches from the Venice barrier-island system (Pellestrina and Cavallino) were reconstructed in a large wave flume and sediment activation was studies using trenches filled with colored sand. The results confirm the control by Significative Wave Height (Hs) and Peak Wave Period (Ts). The spatially averaged Sediment Mixing Depth (Zm) resulted to be respectively 20% of Hs and 8% of Tp. In the case of the beach protected by a breakwater (Pellestrina) wave steepness resulted to be an additional indicator, possibly because of variable transmission rates over the structure.
机译:海滩上的沙滩上的沙子激活深度是沿海工程中许多科学和应用项目的关键参数。虽然在田间研究中存在良好的文学,但这里提出的工作代表了对其种类的第一个实验室研究。从威尼斯屏障 - 岛屿系统(Pellestrina和Cavallino)的两个营养海滩被重建在大波浪水槽中,沉积物激活是使用填充有色沙子的沟渠的研究。结果通过有效波高(HS)和峰波周期(TS)确认控制。空间平均沉积物混合深度(Zm)导致分别为HS和8%TP的20%。在海滩受到防波堤(Pellestrina)的情况下,波陡峭导致额外的指示器,可能是因为结构上的可变传输速率。

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