A two-layer model for simulating landslide dam over mobile river beds

被引:46
作者
Liu, Wei [1 ,2 ]
He, Siming [1 ,2 ,3 ]
机构
[1] Chinese Acad Sci, Key Lab Mt Hazards & Surface Proc, Chengdu, Peoples R China
[2] Chinese Acad Sci, Inst Mt Hazards & Environm IMHE, 9,Block 4,Renminnanlu Rd, Chengdu, Peoples R China
[3] CAS Ctr Excellence Tibetan Plateau Earth Sci, Chengdu, Peoples R China
基金
中国国家自然科学基金;
关键词
Two-layer model; Landslide dam; Erosion; Excess pore-water pressure; Roe-type scheme; SHALLOW-WATER EQUATIONS; CATASTROPHIC LANDSLIDES; NUMERICAL-SOLUTION; GRANULAR MASSES; FLOW; FAILURE;
D O I
10.1007/s10346-015-0585-2
中图分类号
P5 [地质学];
学科分类号
0709 ; 081803 ;
摘要
Landslides can block mountainous streams and form landslide dams to threaten downstream residents. It is necessary for reliable methods to predict landslide dam dynamic for risk assessment. In this paper, we present a two-layer model of Savage-Hutter type to simulate the dynamic evolution of landslide dam which take account of the erosion of river bed. The two-layer shallow water system is derived by depth-averaging the incompressible Navier-Stokes equations with the hydrostatic assumption integrated of the erosion model of river bed. The effect of excess pore water pressure is considered in the erosion process. A high order accuracy scheme based on Roe-type solver is used to discretize the present model. Finally, several numerical tests are performed to verify the stability of the algorithm and reliability of the model. Numerical results indicate that the erosion effect enhances the huge destructiveness of landslide and increase the possibility of river blocked by landslides. The impact of excess pore water pressure on erosion process should be considered.
引用
收藏
页码:565 / 576
页数:12
相关论文
共 48 条
[1]  
Abbott MichaelB., 1979, Computational Hydraulics: Elements of the Theory of Free Surface Flows, P326
[2]  
[Anonymous], 2002, PROC RIVER FLOW
[3]   Zero mass error using unsteady wetting-drying conditions in shallow flows over dry irregular topography [J].
Brufau, P ;
García-Navarro, P ;
Vázquez-Cendón, ME .
INTERNATIONAL JOURNAL FOR NUMERICAL METHODS IN FLUIDS, 2004, 45 (10) :1047-1082
[4]   A Q-scheme for a class of systems of coupled conservation laws with source term.: Application to a two-layer 1-D shallow water system [J].
Castro, M ;
Macías, J ;
Parés, C .
ESAIM-MATHEMATICAL MODELLING AND NUMERICAL ANALYSIS-MODELISATION MATHEMATIQUE ET ANALYSE NUMERIQUE, 2001, 35 (01) :107-127
[5]   Simulation of the erosion process of landslide dams due to overtopping considering variations in soil erodibility along depth [J].
Chang, D. S. ;
Zhang, L. M. .
NATURAL HAZARDS AND EARTH SYSTEM SCIENCES, 2010, 10 (04) :933-946
[6]   Two-layer shallow water computation of mud flow intrusions into quiescent water [J].
Chen, Su-Chin ;
Peng, Szu-Hsien ;
Capart, Herve .
JOURNAL OF HYDRAULIC RESEARCH, 2007, 45 (01) :13-25
[7]   Two-dimensional numerical model of two-layer shallow water equations for confluence simulation [J].
Chen, Su-Chin ;
Peng, Szu-Hsien .
ADVANCES IN WATER RESOURCES, 2006, 29 (11) :1608-1617
[8]   Numerical modelling of entrainment/deposition in rock and debris-avalanches [J].
Crosta, G. B. ;
Imposimato, S. ;
Roddeman, D. .
ENGINEERING GEOLOGY, 2009, 109 (1-2) :135-145
[9]   The 12 May Wenchuan earthquake-induced landslide lakes: distribution and preliminary risk evaluation [J].
Cui, Peng ;
Zhu, Ying-yan ;
Han, Yong-shun ;
Chen, Xiao-qing ;
Zhuang, Jian-qi .
LANDSLIDES, 2009, 6 (03) :209-223
[10]   Formation and failure of the Tsatichhu landslide dam, Bhutan [J].
Dunning, SA ;
Rosser, NJ ;
Petley, DN ;
Massey, CR .
LANDSLIDES, 2006, 3 (02) :107-113