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首页> 外文期刊>American Journal of Civil Engineering and Architecture >Levee Breaching Process of a River and Disaster Risk on Floodplain
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Levee Breaching Process of a River and Disaster Risk on Floodplain

机译:河流堤坝突破过程与洪泛区灾害风险

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摘要

Small-scale laboratory experiments and same scenario numerical analyses were conducted to understand levee breaching phenomena and subsequent disasters risk in floodplain focusing on the effects of the relative height of river bed to the floodplain and the bed materials. In the present study, the area including river, levee and floodplain has been reproduced in both experiment and numerical simulation because not only the behavior of levee but also the phenomena in river and floodplain are intimately related to one another. As a result the followings have been clarified: Higher bed level brings more rapid propagation of the levee breach and widening with more inundation and sediment deposition on the floodplain. River bed degradation in the upstream of the levee breaching point may cause further risk of breach. While as for the effect of bed materials, it has exposed that the finer materials has higher risk not only by more deposition on the floodplain but also by remarkable river bed degradation.
机译:进行了小型实验室实验和相同情景的数值分析,以了解洪水泛滥区的堤防破坏现象和随后的灾害风险,重点是河床相对于洪水泛滥区和河床材料的相对高度的影响。在本研究中,由于不仅堤防的行为与河流与洪泛区的现象之间有着密切的联系,因此在实验和数值模拟中都再现了包括河流,堤防和洪泛区在内的区域。结果,可以弄清以下几点:较高的床位可以使堤防破损更迅速地传播,并随着泛洪平原上更多的洪水和泥沙沉积而加宽。堤防突破口上游的河床退化可能导致进一步的突破风险。至于床层材料的作用,人们已经发现,较细的材料不仅具有更高的风险,不仅因为洪泛区上的沉积更多,而且由于河床的显着降解而造成的。

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