Effect of dike line adjustment on the tidal bore in the Qiantang Estuary, China

IF 3.4 3区 工程技术 Q1 MECHANICS
Jian Zeng (曾剑), Gang Chen (陈刚), Cun-hong Pan (潘存鸿), Zhi-yong Zhang (张芝永)
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引用次数: 12

Abstract

In this paper, the effect of the dike line adjustment on the Qiantang Tidal Bore (QTB) is studied by physcial experiments. A lab-scale physical model of the Qiantang Estuary is built and the tidal bore is generated. With this model, the formation and pro-pagation processes of the tidal bore are simulated with or without the dike line adjustment. It is shown that the adjusted dike line changes the direction of the reflected tidal bore. The height of the tidal bore increases in the upstream region where the dike line is contracted. In the tested bent and forking regimes, the bore height at the upstream station is increased by 0.10 m and 0.04 m, respectively. Furthermore, the crossing bore still exists near the Daquekou station and the location slightly moves by about 3 km to the downstream region.

钱塘江口堤线调整对潮涌的影响
本文通过物理实验研究了堤线调整对钱塘潮涌的影响。建立了钱塘江口的室内物理模型,并进行了潮涌的模拟。利用该模型,模拟了在进行堤线调整和不进行堤线调整的情况下潮孔的形成和发展过程。结果表明,调整后的堤线改变了反射潮涌的方向。在堤线收缩的上游地区,潮孔高度增加。在弯曲和分叉试验工况下,上游站钻孔高度分别增加0.10 m和0.04 m。此外,大溪口站附近仍有过孔存在,位置向下游移动了约3 km。
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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来源期刊
CiteScore
5.90
自引率
0.00%
发文量
1240
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