Modelling the impact of dam failure scenarios on flood inundation using SPH

被引:41
作者
Prakash, Mahesh [1 ]
Rothauge, Kai [2 ]
Cleary, Paul W. [1 ]
机构
[1] CSIRO Math Informat & Stat, Clayton, Vic 3169, Australia
[2] Univ British Columbia, Inst Appl Math, Vancouver, BC V6T 1Z2, Canada
关键词
Smoothed particle hydrodynamics; Dam-break; St. Francis dam; Flood inundation; Dam wall fragments; Disaster scenario modelling; SMOOTHED PARTICLE HYDRODYNAMICS; SIMULATION; BREAK; VOLUME; FLOWS; COMPLEX; FRONTS;
D O I
10.1016/j.apm.2014.03.011
中图分类号
T [工业技术];
学科分类号
08 ;
摘要
Flooding resulting from collapse of a dam is a highly destructive event. It is important to accurately predict the flow behaviour so that potential mitigation strategies can be investigated for disaster management planning. The meshless SPH method has previously been able to model this class of extreme flow events. In this paper, we extend the method to include modelling of dam wall fragments. Collisions between dam wall fragments, between fragments and terrain and full two-way coupling between fragments and the free surface water flow is included. This gives a method that can specifically investigate the impact of the dam wall failure scenario on the subsequent inundation. The historical St. Francis dam failure is used to demonstrate the impact of including the dam fragments. It also provides a means of quantitatively investigating their effect in terms of arrival time and water height at a downstream power station. The scenario with multiple independently timed failures of different parts of the wall (which closely matches the historical failure) gives excellent agreement with the observed data and gives the best match of all failure scenarios. Traditionally such modelling is performed by solving the two dimensional shallow water equations which is not able to capture the three dimensional nature of the flow in earlier stages of dam flooding. We specifically investigate the three dimensional nature of flow structures and formation of multiple downstream hydraulic jumps. These strongly influence water height and therefore control the extent of flooding of tributary valleys. (C) 2014 Elsevier Inc. All rights reserved.
引用
收藏
页码:5515 / 5534
页数:20
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