Large deformation FEMLIP drained analysis of a vertical cut

被引:45
作者
Cuomo, S. [1 ]
Prime, N. [2 ]
Iannone, A. [1 ]
Dufour, F. [2 ]
Cascini, L. [1 ]
Darve, F. [2 ]
机构
[1] Univ Salerno, Dept Civil Engn, Lab Geotech, I-84084 Fisciano, SA, Italy
[2] Univ Grenoble 1, Grenoble INP, Lab Soils Solids Struct Risks 3SR, F-38041 Grenoble 9, France
关键词
FEM; Lagrangian; Large deformation; Modelling; Vertical cut; CONCRETE FLOW; FAILURE; LANDSLIDES; STABILITY;
D O I
10.1007/s11440-012-0179-2
中图分类号
P5 [地质学];
学科分类号
0709 ; 081803 ;
摘要
Understanding and modelling the whole instability mechanisms of a slope are fundamental issues from a scientific and technical viewpoint. To date, small strain Lagrangian approaches have mostly been used in solid mechanics for modelling the failure stage, whereas Eulerian approaches are common in fluid mechanics for propagation analysis. A combination of both approaches allows the stability, failure and propagation stages of a slope to be analysed in a unique mathematical framework. To this end, this paper adopts a finite element method with Lagrangian integration points (FEMLIP), which is currently implemented in the ELLIPSIS code and has been used in geophysics and civil engineering applications. The method combines the robustness of an Eulerian mesh with the flexibility of a set of Lagrangian particles, which allows the history of the material to be taken into account. FEMLIP is first validated with reference to benchmarks with analytical solutions, and is then tested in a large deformation drained analysis of a vertical cut in coarse-grained soils. The results are compared with those provided by the standard engineering methods (1) the limit equilibrium method (LEM) and (2) standard stress-strain elasto-plastic FEM analysis. The comparison shows that FEMLIP is a reliable method for the analysis of both the stability and the instability of a vertical cut, and can be confidently used to analyse more complex problems related to natural slopes.
引用
收藏
页码:125 / 136
页数:12
相关论文
共 32 条
[1]  
[Anonymous], 1937, J BOST SOC CIV
[2]  
[Anonymous], P INT WORKSH FLOWS 2
[3]  
[Anonymous], US GUID GEOSTUDIO 20
[4]  
Barnichon JD, 1998, THESIS U LIEGE, P264
[5]   Geotechnical characterisation of pyroclastic soils involved in huge flowslides [J].
Bilotta, Eduardo ;
Cascini, Leonardo ;
Foresta, Vito ;
Sorbino, Giuseppe .
GEOTECHNICAL AND GEOLOGICAL ENGINEERING, 2005, 23 (04) :365-402
[6]   Slope stability analysis and discontinuous slope failure simulation by elasto-plastic smoothed particle hydrodynamics (SPH) [J].
Bui, H. H. ;
Fukagawa, R. ;
Sako, K. ;
Wells, J. C. .
GEOTECHNIQUE, 2011, 61 (07) :565-574
[7]  
Cascini L., 2008, INT ENV MODELLING SO, P1484
[8]   Typical source areas of May 1998 flow-like mass movements in the Campania region, Southern Italy [J].
Cascini, Leonardo ;
Cuomo, Sabatino ;
Guida, Domenico .
ENGINEERING GEOLOGY, 2008, 96 (3-4) :107-125
[9]   Modeling of Rainfall-Induced Shallow Landslides of the Flow-Type [J].
Cascini, Leonardo ;
Cuomo, Sabatino ;
Pastor, Manuel ;
Sorbin, Giuseppe .
JOURNAL OF GEOTECHNICAL AND GEOENVIRONMENTAL ENGINEERING, 2010, 136 (01) :85-98
[10]   Unstable behaviour of sand and its implication for slope instability [J].
Chu, J ;
Leroueil, S ;
Leong, WK .
CANADIAN GEOTECHNICAL JOURNAL, 2003, 40 (05) :873-885