Numerical study of the stability of breakwater built on a sloped porous seabed under tsunami loading

被引:29
作者
Ye Jianhong [1 ,3 ]
Jeng Dongsheng [2 ,3 ]
Wang Ren [1 ]
Zhu Changqi [1 ]
机构
[1] Chinese Acad Sci, State Key Lab Geomech & Geotech Engn, Inst Rock & Soil Mech, Wuhan 430071, Peoples R China
[2] Griffith Univ, Griffith Sch Engn, Gold Coast, Qld 4222, Australia
[3] Univ Dundee, Div Civil Engn, Dundee DD1 4HN, Scotland
基金
英国工程与自然科学研究理事会;
关键词
Earthquake; Tsunami; Breakwater; Porous seabed; Shear failure; Liquefaction; Japanese; 311; earthquake; SOLITARY WAVE; BREAKING; LIQUEFACTION; MODEL;
D O I
10.1016/j.apm.2013.05.006
中图分类号
T [工业技术];
学科分类号
08 ;
摘要
Strong earthquake induced huge tsunami has occurred for three times in Pacific ocean in recent ten years; for example, the tsunami triggered by the Sumatra earthquake in 2004, Chile earthquake in 2010 and Tohoku earthquake (Japan) in 2011. Tsunami carrying huge energy always would bring high risks to the population living near to coastline. Breakwater is widely used to dissipate the wave energy, and protect coastline and ports. However, they are vulnerable when being attacked by tsunami wave. At present, the interaction mechanism between tsunami, breakwater and its seabed foundation is not fully understood. In this study, the dynamics and stability of a breakwater under the attacking of tsunami wave is investigated by adopting an integrated model PORO-WSSI 2D, in which the VARANS equation for wave motion, and the Blot's dynamic equation for soil are used. Based on the numerical results, it is found that offshore breakwater interacts intensively with tsunami wave when it overtopping and overflowing over a breakwater. The impact force on the lateral side of breakwater applied by tsunami wave is huge. The shear failure is likely to occur in the seabed foundation of breakwater. The liquefaction is unlikely to occur due to the fact that there is basically no upward seepage force in seabed foundation in the process of tsunami wave passing through the breakwater. (C) 2013 Elsevier Inc. All rights reserved.
引用
收藏
页码:9575 / 9590
页数:16
相关论文
共 28 条
[1]  
[Anonymous], J FLUIDS STRUCT
[2]  
[Anonymous], J WATERWAY PORT COAS
[4]   General theory of three-dimensional consolidation [J].
Biot, MA .
JOURNAL OF APPLIED PHYSICS, 1941, 12 (02) :155-164
[5]   Effect of a submerged bay-mouth breakwater on tsunami behavior analyzed by 2D/3D hybrid model simulation [J].
Fujima, Koji .
NATURAL HAZARDS, 2006, 39 (02) :179-193
[6]   CHARACTERISTICS OF SOLITARY WAVE BREAKING INDUCED BY BREAKWATERS [J].
GRILLI, ST ;
LOSADA, MA ;
MARTIN, F .
JOURNAL OF WATERWAY PORT COASTAL AND OCEAN ENGINEERING-ASCE, 1994, 120 (01) :74-92
[7]   Tsunami-like solitary waves impinging and overtopping an impermeable seawall: Experiment and RANS modeling [J].
Hsiao, Shih-Chun ;
Lin, Ting-Chieh .
COASTAL ENGINEERING, 2010, 57 (01) :1-18
[8]   On the evolution and run-up of breaking solitary waves on a mild sloping beach [J].
Hsiao, Shih-Chun ;
Hsu, Tai-Wen ;
Lin, Ting-Chieh ;
Chang, Yu-Hsuan .
COASTAL ENGINEERING, 2008, 55 (12) :975-988
[9]   WAVE-INDUCED SOIL RESPONSE IN AN UNSATURATED ANISOTROPIC SEABED OF FINITE THICKNESS [J].
HSU, JRC ;
JENG, DS .
INTERNATIONAL JOURNAL FOR NUMERICAL AND ANALYTICAL METHODS IN GEOMECHANICS, 1994, 18 (11) :785-807
[10]   A numerical model for wave motions and turbulence flows in front of a composite breakwater [J].
Hsu, TJ ;
Sakakiyama, T ;
Liu, PLF .
COASTAL ENGINEERING, 2002, 46 (01) :25-50