Effects of the foot evolution on the behaviour of slow-moving landslides

被引:30
作者
Ferrari, A. [2 ]
Ledesma, A. [1 ]
Gonzalez, D. A. [1 ]
Corominas, J. [1 ]
机构
[1] Tech Univ Catalonia, UPC, Dept Geotech Engn & Geosci, E-08034 Barcelona, Spain
[2] Ecole Polytech Fed Lausanne, Lab Soil Mech, CH-1015 Lausanne, Switzerland
关键词
Translational slide; Block model; Toe erosion; Motion analysis; Viscosity; DISPLACEMENTS; FAILURE; MODEL;
D O I
10.1016/j.enggeo.2010.11.001
中图分类号
P5 [地质学];
学科分类号
0709 ; 081803 ;
摘要
The paper presents a time-dependent 2D numerical model which has been developed with the purpose of highlighting the effects of the slope foot evolution on the behaviour of slow-moving landslides. The model allows to quantitatively analyse how foot mass variations can influence the stability and the movement rates of the landslide. The landslide body is modelled as composed of two rigid blocks sliding on two different planes and interacting through a common boundary, which position is assumed fixed during the analysis. A finite difference approach is used to discretize the time. For each time increment, changes in model parameters are allowed, including variations in shearing resistances, groundwater level and block masses (in order to simulate foot erosion). During each iteration, the overall stability of the system is checked computing the safety factor, assuming that the percentage of mobilized shear strength is the same for the three surfaces. If the system is not stable or if it is not at rest, the velocity of the system is computed solving the momentum equations for the two blocks taking into account destabilising and resisting forces, the mechanical interaction between the blocks and viscous components. Computed velocities are iteratively used to compute mass accumulation at the foot, which in turn results in a change of the stability condition of the system. Examples are provided in order to highlight the roles of the model parameters. Finally, the application to a real landslide (Vallcebre, Spain) is presented which shows the advantage of considering the foot mass in the analysis of the displacement trends and the possibility to take into account the foot erosion in the long-term behaviour of the slope. (C) 2010 Elsevier B.V. All rights reserved.
引用
收藏
页码:217 / 228
页数:12
相关论文
共 16 条
[1]   Aznalcollar dam failure. Part 3: Dynamics of the motion [J].
Alonso, EE ;
Gens, A .
GEOTECHNIQUE, 2006, 56 (03) :203-210
[2]   A visco-plastic model for slope analysis applied to a mudslide in Cortina d'Ampezzo, Italy [J].
Angeli, MG ;
Gasparetto, P ;
Menotti, RM ;
Pasuto, A ;
Silvano, S .
QUARTERLY JOURNAL OF ENGINEERING GEOLOGY, 1996, 29 :233-240
[3]  
[Anonymous], 1932, Bergsturz und menschenleben
[4]  
Bertini T., 1984, IV International Symposium on Landslides [Canadian Geotechnical Society]., P367
[5]  
BERTINI T, 1986, P 16 CONV NAZ GEOT B, P91
[6]   Prediction of ground displacements and velocities from groundwater level changes at the Vallcebre landslide (Eastern Pyrenees, Spain) [J].
Corominas, J ;
Moya, J ;
Ledesma, A ;
Lloret, A ;
Gili, JA .
LANDSLIDES, 2005, 2 (02) :83-96
[7]   Measurement of landslide displacements using a wire extensometer [J].
Corominas, J ;
Moya, J ;
Lloret, A ;
Gili, JA ;
Angeli, MG ;
Pasuto, A ;
Silvano, S .
ENGINEERING GEOLOGY, 2000, 55 (03) :149-166
[8]  
Ferrari A, 2009, CMES-COMP MODEL ENG, V52, P217
[9]   The viscous component in slow moving landslides: A practical case [J].
Gonzalez, D. A. ;
Ledesma, A. ;
Corominas, J. .
LANDSLIDES AND ENGINEERED SLOPES: FROM THE PAST TO THE FUTURE, VOLS 1 AND 2, 2008, :237-+
[10]   A MODEL FOR THE RUNOUT ANALYSIS OF RAPID FLOW SLIDES, DEBRIS FLOWS, AND AVALANCHES [J].
HUNGR, O .
CANADIAN GEOTECHNICAL JOURNAL, 1995, 32 (04) :610-623