Numerical Modeling of Large Landslide Stability and Runout

Abstract. Modelling of flow-like landslides is one of the possible approaches that can be used to simulate landslide instability and flow development. Models based on continuum mechanics and associated with a versatile rheological model are usually preferred to predict landslide runout and relevant parameters. A different approach has been used in this research. We have developed a 2-D/3-D finite element code to analyse slope stability and to model runout of mass movements characterised by very large displacements. The idea was to be able to use different material laws already known, tested and verified for granular materials. The implemented materials laws include classical elasto-plasticity, with a linear elastic part and different applicable yield surfaces with associated and non-associated flow rules. The application of Finite Element methods to model landslide run-out, contrasts previous research where typically depth-averaged equivalent-fluid approaches were adopted. The code has been applied to the simulation of large rock avalanches and rapid dry flows in different materials and under different geological and geomorphological conditions.

[1]  H. J. Körner,et al.  Flow mechanisms and resistances in the debris streams of rock slides , 1977 .

[2]  Kyoji Sassa,et al.  Geotechnical model for the motion of landslides , 1988 .

[3]  Nick Barton,et al.  Engineering classification of rock masses for the design of tunnel support , 1974 .

[4]  D. M. Cruden,et al.  Destructive mass movements in high mountains: hazard and management, Geological Survey of Canada Paper 84-16: Book review , 1985 .

[5]  E. T. Brown,et al.  Underground excavations in rock , 1980 .

[6]  Kenneth J. Hsü,et al.  Catastrophic Debris Streams (Sturzstroms) Generated by Rockfalls , 1975 .

[7]  P. Julien,et al.  Two‐Dimensional Water Flood and Mudflow Simulation , 1993 .

[8]  David M. Cruden,et al.  LANDSLIDES: INVESTIGATION AND MITIGATION. CHAPTER 3 - LANDSLIDE TYPES AND PROCESSES , 1996 .

[9]  J. N. Hutchinson A sliding–consolidation model for flow slides , 1986 .

[10]  Oldrich Hungr,et al.  A model for the runout analysis of rapid flow slides, debris flows, and avalanches , 1995 .

[11]  F. Legros,et al.  Pseudotachylyte (Frictionite) at the Base of the Arequipa Volcanic Landslide Deposit (Peru): Implications for Emplacement Mechanisms , 2000, The Journal of Geology.

[12]  Timothy R. H. Davies Spreading of rock avalanche debris by mechanical fluidization , 1982 .

[13]  B. Voight,et al.  Multiple-pulsed debris avalanche emplacement at Mount St. Helens in 1980: Evidence from numerical continuum flow simulations , 1995 .

[14]  N. Barton,et al.  The shear strength of rock joints in theory and practice , 1977 .

[15]  A. Heim Bergsturz und Menschenleben , 1932 .

[16]  J. D. Aitken,et al.  A rock avalanche triggered by the October 1985 North Nahanni earthquake, District of Mackenzie, N.W.T. , 1987 .

[17]  Richard M. Iverson,et al.  Flow of variably fluidized granular masses across three‐dimensional terrain: 2. Numerical predictions and experimental tests , 2001 .

[18]  Giovanni B. Crosta,et al.  Structural constraints on deep-seated slope deformation kinematics , 2001 .

[19]  Alfred S. McEwen,et al.  Dynamics of Mount St. Helens' 1980 pyroclastic flows, rockslide-avalanche, lahars, and blast , 1989 .

[20]  P. Habib,et al.  Production of gaseous pore pressure during rock slides , 1975 .

[21]  Jey K. Jeyapalan,et al.  Investigation of Flow Failures of Tailings Dams , 1983 .

[22]  Adrian E. Scheidegger,et al.  On the prediction of the reach and velocity of catastrophic landslides , 1973 .

[23]  Richard M. Iverson,et al.  Flow of variably fluidized granular masses across three‐dimensional terrain: 1. Coulomb mixture theory , 2001 .

[24]  L. Siebert Large volcanic debris avalanches: Characteristics of source areas, deposits, and associated eruptions , 1984 .

[25]  William G. Pariseau,et al.  Rockslides and Avalanches: Basic Principles, and Perspectives in the Realm of Civil and Mining Operations , 1979 .

[26]  Charles S. Campbell,et al.  Self-Lubrication for Long Runout Landslides , 1989, The Journal of Geology.

[27]  B. Voight,et al.  Lessons from Ontake-san: A comparative analysis of debris avalanche dynamics , 1994 .

[28]  T. H. Erismann,et al.  Flowing, rolling, bouncing, sliding: Synopsis of basic mechanisms , 1986 .

[29]  H Chen,et al.  Numerical simulation of debris flows , 2000 .

[30]  G. Crosta,et al.  Numerical simulation of dry granular flows: From the reproduction of small-scale experiments to the prediction of rock avalanches , 2000 .

[31]  H. J. Melosh,et al.  The physics of very large landslides , 1986 .

[32]  J. Clague,et al.  Destructive mass movements in high mountains: Hazard and management , 1984 .

[33]  F. Legros The mobility of long-runout landslides , 2002 .

[34]  Z. T. Bieniawski,et al.  Engineering Rock Mass Classifications: A Complete Manual for Engineers and Geologists in Mining, Civil, and Petroleum Engineering , 1989 .

[35]  William R. Normark,et al.  Prodigious submarine landslides on the Hawaiian Ridge , 1989 .

[36]  R. L. Shreve,et al.  Leakage and Fluidization in Air-Layer Lubricated Avalanches , 1968 .

[37]  O. Hungr,et al.  The Avalanche Lake rock avalanche, Mackenzie Mountains, Northwest Territories, Canada: description, dating, and dynamics , 1994 .

[38]  Christopher R. J. Kilburn,et al.  Runout lengths of sturzstroms: The control of initial conditions and of fragment dynamics , 1998 .

[39]  Theodor H. Erismann,et al.  Dynamics of rockslides and rockfalls , 2001 .