倾斜海滩海堤海啸上升的物理与数值模拟

Ma'ruf Hadi Sutanto
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引用次数: 1

摘要

海啸对陆地的冲击具有巨大的破坏力。对沿海地区海啸上升的过程和特征有必要进行进一步的研究。海堤结构可以减少海啸的上升,这取决于海堤波峰的高度。物理模拟结果表明,海堤可显著降低爬高(𝑅)和淹没(𝑋)。当海堤峰高为7厘米,水深为15厘米时,最大降幅可达55%。在数值模拟的相同场景下,减少的百分比为67.53%。相同情景下的数值模拟结果为6.970 m。海堤作为海啸减灾结构,只有在海啸波相对于海堤高度(H/ sw)较低时才有效。还原率> 25%,H/ sw < 0.856(物理模型),< 0.802(数值模型)。
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Physical and Numerical Modelling of Tsunami Run-up on Seawall at Sloping Beach
Tsunami run-up on land has a large destructive power. Further studies are deemed necessary to understand the process and characteristics of tsunami run-up in coastal areas. Seawall structures can reduce the run-up of a tsunami depending on the height of the seawall crest. Physical modeling shows that seawall may significantly reduce run-up (𝑅) and inundation (𝑋𝑖). The highest reduction up to 55% where the seawall peak height is 7 cm and the water depth is 15 cm. With the same scenario in numerical modeling, the percentage reduction is 67.53%. The highest inundation (Xi) in the scenario without seawall structure is 6.081 m when the initial water depth (d0) equals to 30 cm. The result of the numerical model for the same scenario is 6.970 m. Seawall as tsunami mitigation structure is only effective when the tsunami wave is relatively low compared to the seawall height (H/ sw). Reduction percentage > 25%, with conditions that H/ sw is < 0.856 (physical model) and < 0.802 (numerical model).
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15 weeks
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