基于堤防易损性指数和洪水风险综合模拟的堤防破坏点估算

Kosuke Tabata, S. Fukuoka
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引用次数: 0

摘要

为了检验洪水风险管理措施,必须尽可能准确地估计堤防决口点、淹没流量线和流域淹没水运动。本文的目的是在2015年大洪水期间,日本基努河因溢流和堤防决口而遭受40 km2范围内淹没的情况下进行上述系列研究。首先,建立了洪水与淹没相结合的模拟模型。根据观测到的基努河水面剖面的时间变化,通过洪水流量分析,估算了基努河因溢流和决口引起的洪涝流量曲线。洪水是用二维模型计算的。淹没分析模型的网格采用5 m大小的规则网格生成,以表达DSM (Digital Surface model)获得的微地形。曼宁粗糙度系数根据土地利用情况和淹没深度给出。从相机图像中读取的淹没到达时间和实际淹没水在流域内的扩散情况证实了所建立的模型的有效性。其次,对基努河堤防脆弱性指数t*的适用性进行了检验。最后,根据t*的值进行了实际溃坝和假设溃坝条件下的淹没流量分析。结果表明,基努河流域决口位置和决口时间的差异对淹没水量和淹没面积的运动有影响。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
ESTIMATION OF LEVEE FAILURE POINTS BASED ON LEVEE VULNERABILITY INDEX AND FLOOD RISK ANALYSIS BY INTEGRATING SIMULATION OF FLOOD FLOW AND INUNDATION
ABSTRACT To examine the flood risk management measures, it is important to estimate the levee breach points, inundation discharge hydrograph and motion of the inundation water in the basin as precisely as possible. The purpose of this paper is to conduct the above series of studies on the Kinu River (Japan) suffered from inundation in the range of 40 km2 due to overflowing and levee breach during the 2015 large flood. First, a simulation model integrating flood flow and inundation is developed. The inundation discharge hydrographs due to the overflowing and levee breach are estimated by the flood flow analysis based on observed temporal changes in water surface profiles in the Kinu River. The inundation is calculated by a two-dimensional model. The mesh of the inundation analysis model is generated by regular grid with 5 m size in order to express the microtopography obtained by DSM (Digital Surface Model). Manning’s roughness coefficients are given according to the situation of the land use and inundation depth. It is confirmed that the developed model is useful by the inundation arrival time read from camera images and the spread of the actual inundation water in the basin. Next, the suitability of the levee vulnerability index t* which has been derived by the authors is examined for the levees of the Kinu River. Finally, the inundation flow analysis is conducted under the actual and hypothetical levee breach conditions based on the value of t*. It is concluded that the difference in the location and time of the levee breach influences on the motion of the inundation water and inundation areas in the Kinu River basin.
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