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Effect of backward-facing step heights in vegetation-step model on reducing the velocity of a tsunami inundation and increasing the energy dissipation efficiency 被引量:1
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作者 Wen-xin Huai Xiao-hua Zhang +2 位作者 Dan Li Zhong-hua Yang Yi-dan Ai 《Journal of Hydrodynamics》 SCIE EI CSCD 2024年第5期803-816,共14页
A coastal forest combined with a backward-facing step is an efficient facility to reduce tsunami damage to residential areas behind sea embankments.This study establishes a generalized model,and experimentally explore... A coastal forest combined with a backward-facing step is an efficient facility to reduce tsunami damage to residential areas behind sea embankments.This study establishes a generalized model,and experimentally explores the water level changes upstream of the vegetation-step mitigation model as well as its energy dissipation effect under different initial Froude numbers,step heights,and vegetation conditions.The results show that the relative backwater rise increases with the growth of vegetation density,patch length and initial Froude number,representing a slowing down of the tsunami inundation.As for energy dissipation,it is mainly caused by the additional resistance of the vegetation and the hydraulic jump.And the vegetation condition not only affects the energy dissipation due to stem-scale turbulence within the patch,but also changes the hydraulic jump process of water falling from the step in cooperation with the step height.As a result,the energy dissipation efficiency always increases with the growth of vegetation density,vegetation patch length and step height.With the criterion that the energy dissipation efficiency and its growth rate can hardly change with vegetation parameters,this study innovatively defines the threshold slope and gives the principle of judging the most cost-effective vegetation conditions at different step heights.These results are expected to provide an important reference for the design of composite tsunami mitigation facilities. 展开更多
关键词 vegetation-step model step height backwater rise energy dissipation
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