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Slope stability analysis

Figure 1: Rotational failure of slope on circular slip surface

Slope stability analysis is performed to assess the safe design of a human-made or natural slopes (e.g. embankments, road cuts, open-pit mining, excavations, landfills etc.) and the equilibrium conditions.[1][2] Slope stability is the resistance of inclined surface to failure by sliding or collapsing.[3] The main objectives of slope stability analysis are finding endangered areas, investigation of potential failure mechanisms, determination of the slope sensitivity to different triggering mechanisms, designing of optimal slopes with regard to safety, reliability and economics, designing possible remedial measures, e.g. barriers and stabilization.[1][2]

Successful design of the slope requires geological information and site characteristics, e.g. properties of soil/rock mass, slope geometry, groundwater conditions, alternation of materials by faulting, joint or discontinuity systems, movements and tension in joints, earthquake activity etc.[4][5] The presence of water has a detrimental effect on slope stability. Water pressure acting in the pore spaces, fractures or other discontinuities in the materials that make up the pit slope will reduce the strength of those materials.[6] Choice of correct analysis technique depends on both site conditions and the potential mode of failure, with careful consideration being given to the varying strengths, weaknesses and limitations inherent in each methodology.[7]

Before the computer age stability analysis was performed graphically or by using a hand-held calculator. Today engineers have a lot of possibilities to use analysis software, ranges from simple limit equilibrium techniques through to computational limit analysis approaches (e.g. Finite element limit analysis, Discontinuity layout optimization) to complex and sophisticated numerical solutions (finite-/distinct-element codes).[1] The engineer must fully understand limitations of each technique. For example, limit equilibrium is most commonly used and simple solution method, but it can become inadequate if the slope fails by complex mechanisms (e.g. internal deformation and brittle fracture, progressive creep, liquefaction of weaker soil layers, etc.). In these cases more sophisticated numerical modelling techniques should be utilised. Also, even for very simple slopes, the results obtained with typical limit equilibrium methods currently in use (Bishop, Spencer, etc.) may differ considerably. In addition, the use of the risk assessment concept is increasing today. Risk assessment is concerned with both the consequence of slope failure and the probability of failure (both require an understanding of the failure mechanism).[8][9]

Within the last decade (2003) Slope Stability Radar has been developed to remotely scan a rock slope to monitor the spatial deformation of the face. Small movements of a rough wall can be detected with sub-millimeter accuracy by using interferometry techniques.

Limit equilibrium analysisEdit

 
A typical cross-section of a slope used in two-dimensional analyses.

Conventional methods of slope stability analysis can be divided into three groups: kinematic analysis, limit equilibrium analysis, and rock fall simulators.[8] Most slope stability analysis computer programs are based on the limit equilibrium concept for a two- or three-dimensional model.[10][11] Two-dimensional sections are analyzed assuming plane strain conditions. Stability analyses of two-dimensional slope geometries using simple analytical approaches can provide important insights into the initial design and risk assessment of slopes.

Limit equilibrium methods investigate the equilibrium of a soil mass tending to slide down under the influence of gravity. Translational or rotational movement is considered on an assumed or known potential slip surface below the soil or rock mass.[12] In rock slope engineering, methods may be highly significant to simple block failure along distinct discontinuities.[8] All these methods are based on the comparison of forces, moments, or stresses resisting movement of the mass with those that can cause unstable motion (disturbing forces). The output of the analysis is a factor of safety, defined as the ratio of the shear strength (or, alternatively, an equivalent measure of shear resistance or capacity) to the shear stress (or other equivalent measure) required for equilibrium. If the value of factor of safety is less than 1.0, the slope is unstable.

All limit equilibrium methods assume that the shear strengths of the materials along the potential failure surface are governed by linear (Mohr-Coulomb) or non-linear relationships between shear strength and the normal stress on the failure surface.[12] The most commonly used variation is Terzaghi's theory of shear strength which states that

 

where   is the shear strength of the interface,   is the effective stress (  is the total stress normal to the interface and   is the pore water pressure on the interface),   is the effective friction angle, and   is the effective cohesion.

The methods of slices is the most popular limit equilibrium technique. In this approach, the soil mass is discretized into vertical slices.[11][13] Several versions of the method are in use. These variations can produce different results (factor of safety) because of different assumptions and inter-slice boundary conditions.[12][14]

The location of the interface is typically unknown but can be found using numerical optimization methods.[15] For example, functional slope design considers the critical slip surface to be the location where that has the lowest value of factor of safety from a range of possible surfaces. A wide variety of slope stability software use the limit equilibrium concept with automatic critical slip surface determination.

Typical slope stability software can analyze the stability of generally layered soil slopes, embankments, earth cuts, and anchored sheeting structures. Earthquake effects, external loading, groundwater conditions, stabilization forces (i.e., anchors, geo-reinforcements etc.) can also be included.

Analytical techniques: Method of slicesEdit

 
Schematic of the method of slices showing rotation center.

Many slope stability analysis tools use various versions of the methods of slices such as Bishop simplified, Ordinary method of slices (Swedish circle method/Petterson/Fellenius), Spencer, Sarma etc. Sarma and Spencer are called rigorous methods because they satisfy all three conditions of equilibrium: force equilibrium in horizontal and vertical direction and moment equilibrium condition. Rigorous methods can provide more accurate results than non-rigorous methods. Bishop simplified or Fellenius are non-rigorous methods satisfying only some of the equilibrium conditions and making some simplifying assumptions.[13][14] Some of these approaches are discussed below.

Swedish Slip Circle Method of AnalysisEdit

The Swedish Slip Circle method assumes that the friction angle of the soil or rock is equal to zero, i.e.,  . In other words, when friction angle is considered to be zero, the effective stress term goes to zero, thus equating the shear strength to the cohesion parameter of the given soil. The Swedish slip circle method assumes a circular failure interface, and analyzes stress and strength parameters using circular geometry and statics. The moment caused by the internal driving forces of a slope is compared to the moment caused by forces resisting slope failure. If resisting forces are greater than driving forces, the slope is assumed stable.

Ordinary Method of SlicesEdit

 
Division of the slope mass in the method of slices.

In the method of slices, also called OMS or the Fellenius method, the sliding mass above the failure surface is divided into a number of slices. The forces acting on each slice are obtained by considering the mechanical (force and moment) equilibrium for the slices. Each slice is considered on its own and interactions between slices are neglected because the resultant forces are parallel to the base of each slice. However, Newton's third law is not satisfied by this method because, in general, the resultants on the left and right of a slice do not have the same magnitude and are not collinear.[16]

This allows for a simple static equilibrium calculation, considering only soil weight, along with shear and normal stresses along the failure plane. Both the friction angle and cohesion can be considered for each slice. In the general case of the method of slices, the forces acting on a slice are shown in the figure below. The normal ( ) and shear ( ) forces between adjacent slices constrain each slice and make the problem statically indeterminate when they are included in the computation.

 
Force equilibrium for a slice in the method of slices. The block is assumed to have thickness  . The slices on the left and right exert normal forces   and shear forces  , the weight of the slice causes the force  . These forces are balanced by the pore pressure and reactions of the base  .

For the ordinary method of slices, the resultant vertical and horizontal forces are

 

where   represents a linear factor that determines the increase in horizontal force with the depth of the slice. Solving for   gives

 

Next, the method assumes that each slice can rotate about a center of rotation and that moment balance about this point is also needed for equilibrium. A balance of moments for all the slices taken together gives

 

where   is the slice index,   are the moment arms, and loads on the surface have been ignored. The moment equation can be used to solve for the shear forces at the interface after substituting the expression for the normal force:

 

Using Terzaghi's strength theory and converting the stresses into moments, we have

 

where   is the pore pressure. The factor of safety is the ratio of the maximum moment from Terzaghi's theory to the estimated moment,

 

Modified Bishop’s Method of AnalysisEdit

The Modified Bishop's method[17] is slightly different from the ordinary method of slices in that normal interaction forces between adjacent slices are assumed to be collinear and the resultant interslice shear force is zero. The approach was proposed by Alan W. Bishop of Imperial College. The constraint introduced by the normal forces between slices makes the problem statically indeterminate. As a result, iterative methods have to be used to solve for the factor of safety. The method has been shown to produce factor of safety values within a few percent of the "correct" values.

The factor of safety for moment equilibrium in Bishop's method can be expressed as

 

where

 

where, as before,   is the slice index,   is the effective cohesion,   is the effective internal angle of internal friction,   is the width of each slice,  is the weight of each slice, and   is the water pressure at the base of each slice. An iterative method has to be used to solve for   because the factor of safety appears both on the left and right hand sides of the equation.

Lorimer's methodEdit

Lorimer's Method is a technique for evaluating slope stability in cohesive soils. It differs from Bishop's Method in that it uses a clothoid slip surface in place of a circle. This mode of failure was determined experimentally to account for effects of particle cementation. The method was developed in the 1930s by Gerhardt Lorimer (Dec 20, 1894-Oct 19, 1961), a student of geotechnical pioneer Karl von Terzaghi.

Spencer’s MethodEdit

Spencer's Method of analysis[18] requires a computer program capable of cyclic algorithms, but makes slope stability analysis easier. Spencer's algorithm satisfies all equilibria (horizontal, vertical and driving moment) on each slice. The method allows for unconstrained slip plains and can therefore determine the factor of safety along any slip surface. The rigid equilibrium and unconstrained slip surface result in more precise safety factors than, for example, Bishop's Method or the Ordinary Method of Slices.[18]

Sarma methodEdit

The Sarma method,[19] proposed by Sarada K. Sarma of Imperial College is a Limit equilibrium technique used to assess the stability of slopes under seismic conditions. It may also be used for static conditions if the value of the horizontal load is taken as zero. The method can analyse a wide range of slope failures as it may accommodate a multi-wedge failure mechanism and therefore it is not restricted to planar or circular failure surfaces. It may provide information about the factor of safety or about the critical acceleration required to cause collapse.

ComparisonsEdit

The assumptions made by a number of limit equilibrium methods are listed in the table below.[20]

Method Assumption
Ordinary method of cells Interslice forces are neglected
Bishop's simplified/modified [17] Resultant interslice forces are horizontal. There are no interslice shear forces.
Janbu's simplified[21] Resultant interslice forces are horizontal. An empirical correction factor is used to account for interslice shear forces.
Janbu's generalized[21] An assumed line of thrust is used to define the location of the interslice normal force.
Spencer [18] The resultant interslice forces have constant slope throughout the sliding mass. The line of thrust is a degree of freedom.
Chugh[22] Same as Spencer's method but with a constant acceleration force on each slice.
Morgenstern-Price[23] The direction of the resultant interslice forces is defined using an arbitrary function. The fractions of the function value needed for force and moment balance is computed.
Fredlund-Krahn (GLE) [16] Similar to Morgenstern-Price.
Corps of Engineers [24] The resultant interslice force is either parallel to the ground surface or equal to the average slope from the beginning to the end of the slip surface..
Lowe and Karafiath [25] The direction of the resultant interslice force is equal to the average of the ground surface and the slope of the base of each slice.
Sarma [19] The shear strength criterion is applied to the shears on the sides and bottom of each slice. The inclinations of the slice interfaces are varied until a critical criterion is met.

The table below shows the statical equilibrium conditions satisfied by some of the popular limit equilibrium methods.[20]

Method Force balance (vertical) Force balance (horizontal) Moment balance
Ordinary MS Yes No Yes
Bishop's simplified Yes No Yes
Janbu's simplified Yes Yes No
Janbu's generalized Yes Yes Used to compute interslice shear forces
Spencer Yes Yes Yes
Chugh Yes Yes Yes
Morgenstern-Price Yes Yes Yes
Fredlund-Krahn Yes Yes Yes
Corps of Engineers Yes Yes No
Lowe and Karafiath Yes Yes No
Sarma Yes Yes Yes

Rock slope stability analysisEdit

Rock slope stability analysis based on limit equilibrium techniques may consider following modes of failures:

  • Planar failure -> case of rock mass sliding on a single surface (special case of general wedge type of failure); two-dimensional analysis may be used according to the concept of a block resisting on an inclined plane at limit equilibrium[26][27]
  • Polygonal failure -> sliding of a nature rock usually takes place on polygonally-shaped surfaces; calculation is based on a certain assumptions (e.g. sliding on a polygonal surface which is composed from N parts is kinematically possible only in case of development at least (N - 1) internal shear surfaces; rock mass is divided into blocks by internal shear surfaces; blocks are considered to be rigid; no tensile strength is permitted etc.)[27]
  • Wedge failure -> three-dimensional analysis enables modelling of the wedge sliding on two planes in a direction along the line of intersection[27][28]
  • Toppling failure -> long thin rock columns formed by the steeply dipping discontinuities may rotate about a pivot point located at the lowest corner of the block; the sum of the moments causing toppling of a block (i.e. horizontal weight component of the block and the sum of the driving forces from adjacent blocks behind the block under consideration) is compared to the sum of the moments resisting toppling (i.e. vertical weight component of the block and the sum of the resisting forces from adjacent blocks in front of the block under consideration); toppling occur if driving moments exceed resisting moments[29][30]

Limit analysisEdit

A more rigorous approach to slope stability analysis is limit analysis. Unlike limit equilibrium analysis which makes ad-hoc though often reasonable assumptions, limit analysis is based on rigorous plasticity theory. This enables, among other things, the computation of upper and lower bounds on the true factor of safety.

Programs based on limit analysis include:

  • OptumG2 (2014-) General purpose software for geotechnical applications (also includes elastoplasticity, seepage, consolidation, staged construction, tunneling, and other relevant geotechnical analysis types).
  • LimitState:GEO (2008-) General purpose geotechnical software application based on Discontinuity layout optimization for plane strain problems including slope stability.

Stereographic and kinematic analysisEdit

Kinematic analysis examines which modes of failure can possibly occur in the rock mass. Analysis requires the detailed evaluation of rock mass structure and the geometry of existing discontinuities contributing to block instability.[31][32] Stereographic representation (stereonets) of the planes and lines is used.[33] Stereonets are useful for analyzing discontinuous rock blocks.[34] Program DIPS[35] allows for visualization structural data using stereonets, determination of the kinematic feasibility of rock mass and statistical analysis of the discontinuity properties.[31][35]

Rockfall simulatorsEdit

Rock slope stability analysis may design protective measures near or around structures endangered by the falling blocks. Rockfall simulators determine travel paths and trajectories of unstable blocks separated from a rock slope face. Analytical solution method described by Hungr & Evans[36] assumes rock block as a point with mass and velocity moving on a ballistic trajectory with regard to potential contact with slope surface. Calculation requires two restitution coefficients that depend on fragment shape, slope surface roughness, momentum and deformational properties and on the chance of certain conditions in a given impact.[37]

Program ROCFALL[38] provides a statistical analysis of trajectory of falling blocks. Method rely on velocity changes as a rock blocks roll, slide or bounce on various materials. Energy, velocity, bounce height and location of rock endpoints are determined and may be analyzed statistically. The program can assist in determining remedial measures by computing kinetic energy and location of impact on a barrier. This can help determine the capacity, size and location of barriers.[38]

Numerical methods of analysisEdit

Numerical modelling techniques provide an approximate solution to problems which otherwise cannot be solved by conventional methods, e.g. complex geometry, material anisotropy, non-linear behaviour, in situ stresses. Numerical analysis allows for material deformation and failure, modelling of pore pressures, creep deformation, dynamic loading, assessing effects of parameter variations etc. However, numerical modelling is restricted by some limitations. For example, input parameters are not usually measured and availability of these data is generally poor. User also should be aware of boundary effects, meshing errors, hardware memory and time restrictions. Numerical methods used for slope stability analysis can be divided into three main groups: continuum, discontinuum and hybrid modelling.[39]


Continuum modellingEdit

 
Figure 3: Finite element mesh

Modelling of the continuum is suitable for the analysis of soil slopes, massive intact rock or heavily jointed rock masses. This approach includes the finite-difference and finite element methods that discretize the whole mass to finite number of elements with the help of generated mesh (Fig. 3). In finite-difference method (FDM) differential equilibrium equations (i.e. strain-displacement and stress-strain relations) are solved. finite element method (FEM) uses the approximations to the connectivity of elements, continuity of displacements and stresses between elements. Most of numerical codes allows modelling of discrete fractures, e.g. bedding planes, faults. Several constitutive models are usually available, e.g. elasticity, elasto-plasticity, strain-softening, elasto-viscoplasticity etc.[39]

Discontinuum modellingEdit

Discontinuum approach is useful for rock slopes controlled by discontinuity behaviour. Rock mass is considered as an aggregation of distinct, interacting blocks subjected to external loads and assumed to undergo motion with time. This methodology is collectively called the discrete-element method (DEM). Discontinuum modelling allows for sliding between the blocks or particles. The DEM is based on solution of dynamic equation of equilibrium for each block repeatedly until the boundary conditions and laws of contact and motion are satisfied. Discontinuum modelling belongs to the most commonly applied numerical approach to rock slope analysis and following variations of the DEM exist:[39]

The distinct-element approach describes mechanical behaviour of both, the discontinuities and the solid material. This methodology is based on a force-displacement law (specifying the interaction between the deformable rock blocks) and a law of motion (determining displacements caused in the blocks by out-of-balance forces). Joints are treated as [boundary conditions. Deformable blocks are discretized into internal constant-strain elements.[39]

Discontinuum program UDEC[40] (Universal distinct element code) is suitable for high jointed rock slopes subjected to static or dynamic loading. Two-dimensional analysis of translational failure mechanism allows for simulating large displacements, modelling deformation or material yielding.[40] Three-dimensional discontinuum code 3DEC[41] contains modelling of multiple intersecting discontinuities and therefore it is suitable for analysis of wedge instabilities or influence of rock support (e.g. rockbolts, cables).[39]

In discontinuous deformation analysis (DDA) displacements are unknowns and equilibrium equations are then solved analogous to finite element method. Each unit of finite element type mesh represents an isolated block bounded by discontinuities. Advantage of this methodology is possibility to model large deformations, rigid body movements, coupling or failure states between rock blocks.[39]

Discontinuous rock mass can be modelled with the help of distinct-element methodology in the form of particle flow code, e.g. program PFC2D/3D.[42][43] Spherical particles interact through frictional sliding contacts. Simulation of joint bounded blocks may be realized through specified bond strengths. Law of motion is repeatedly applied to each particle and force-displacement law to each contact. Particle flow methodology enables modelling of granular flow, fracture of intact rock, transitional block movements, dynamic response to blasting or seismicity, deformation between particles caused by shear or tensile forces. These codes also allow to model subsequent failure processes of rock slope, e.g. simulation of rock[39]

Hybrid/coupled modellingEdit

Hybrid codes involve the coupling of various methodologies to maximize their key advantages, e.g. limit equilibrium analysis combined with finite element groundwater flow and stress analysis ; coupled particle flow and finite-difference analyses. Hybrid techniques allows investigation of piping slope failures and the influence of high groundwater pressures on the failure of weak rock slope. Coupled finite-/distinct-element codes provide for the modelling of both intact rock behaviour and the development and behaviour of fractures.[39]

[44]

Rock mass classificationEdit

Various rock mass classification systems exist for the design of slopes and to assess the stability of slopes. The systems are based on empirical relations between rock mass parameters and various slope parameters such as height and slope dip.

The Q-slope method for rock slope engineering and rock mass classification developed by Barton and Bar[45] expresses the quality of the rock mass for assessing slope stability using the Q-slope value, from which long-term stable, reinforcement-free slope angles can be derived.

See alsoEdit

ReferencesEdit

  1. ^ a b c Eberhardt 2003, p. 4
  2. ^ a b Abramson 2002, p. 2
  3. ^ Kliche 1999, p. 2
  4. ^ USArmyCorps 2003, pp. 1–2
  5. ^ Abramson 2002, p. 1
  6. ^ Beale, Geoff; Read, John, eds. (2014). Guidelines for Evaluating Water in Pit Slope Stability. CSIRO Publishing. ISBN 9780643108356.
  7. ^ Stead 2001, p. 615
  8. ^ a b c Eberhardt 2003, p. 6
  9. ^ Cardenas, IC (2019). "On the use of Bayesian networks as a meta-modelling approach to analyse uncertainties in slope stability analysis". Georisk: Assessment and Management of Risk for Engineered Systems and Geohazards. 13 (1): 53–65. doi:10.1080/17499518.2018.1498524.
  10. ^ Abramson 2002, p. 329
  11. ^ a b Abramson 2002, p. 363
  12. ^ a b c USArmyCorps 2003, p. 2
  13. ^ a b Zhu 2003, pp. 377–395
  14. ^ a b Abramson 2002, pp. 363–367
  15. ^ USArmyCorps 2003, p. 5
  16. ^ a b Fredlund, DG; Krahn, J (1977), "Comparison of slope stability methods of analysis", Canadian Geotechnical Journal, 14 (3): 429–439, doi:10.1139/t77-045
  17. ^ a b Bishop, A. W. (1955). "The use of the Slip Circle in the Stability Analysis of Slopes". Géotechnique. 5: 7–17. doi:10.1680/geot.1955.5.1.7.
  18. ^ a b c Spencer, E. (1967). "A Method of analysis of the Stability of Embankments Assuming Parallel Inter-Slice Forces". Géotechnique. 17: 11–26. doi:10.1680/geot.1967.17.1.11.
  19. ^ a b Sarma, S. K. (1975). "Seismic stability of earth dams and embankments". Géotechnique. 25 (4): 743–761. doi:10.1680/geot.1975.25.4.743.
  20. ^ a b Fredlund, D.G. (1984), "Analytical methods for slope stability analysis" (PDF), Proceedings of the Fourth International Symposium on Landslides, State-of-the-Art: 229–250
  21. ^ a b Janbu, Nilmar (1973), RC Hirschfeld and SJ Poulos (eds.), "Slope stability computations", In Embankment-dam Engineering, Jon Wiley and Sons Inc., NY: 40PCS1 maint: uses editors parameter (link)
  22. ^ Chugh, Ashok K (1982), "Slope stability analysis for earthquakes", International Journal for Numerical and Analytical Methods in Geomechanics, 6 (3): 307–322, Bibcode:1982IJNAM...6..307C, doi:10.1002/nag.1610060304
  23. ^ Morgenstern, N. R.; Price, V. Eo (1965), "The analysis of the stability of general slip surfaces", Geotechnique, 15 (1): 79–93, doi:10.1680/geot.1965.15.1.79
  24. ^ "Slope Stability" (PDF). US Army Corps of Engineers. Retrieved 15 April 2015.
  25. ^ Lowe, John; Karafiath, Leslie (1960), "Stability of earth dams upon drawdown", In Proc. 1st. Pan American Conference on Soil Mechanics and Foundation Engineering, México, 2: 537–552
  26. ^ Kliche 1999, pp. 125–137
  27. ^ a b c Kovari 1978, pp. 103–124
  28. ^ Kliche 1999, pp. 153–169
  29. ^ Kliche 1999, p. 15
  30. ^ Kliche 1999, pp. 139–152
  31. ^ a b Eberhardt 2003, p. 7
  32. ^ Kliche 1999, p. 111
  33. ^ Kliche 1999, pp. 111–123
  34. ^ Kliche 1999, pp. 43–65
  35. ^ a b "DIPS – Graphical and Statistical Analysis of Orientation Data", Rocscience.com, Toronto, Canada: Rocscience, retrieved 21 July 2009
  36. ^ Hungr 1988, pp. 685–690
  37. ^ Eberhardt 2003, pp. 15–17
  38. ^ a b "ROCFALL – Statistical Analysis of Rockfalls", Rocscience.com, Toronto, Canada: Rocscience, retrieved 21 July 2009
  39. ^ a b c d e f g h Eberhardt 2003, pp. 17–38
  40. ^ a b "UDEC - Universal Distinct Element Code", Itascacg.com, Minneapolis, USA: Itasca, retrieved 27 July 2009
  41. ^ "3DEC - Three Dimensional Distinct Element Code", Itascacg.com, Minneapolis, USA: Itasca, retrieved 27 July 2009
  42. ^ "PFC2D - Particle Flow Code in Two Dimensions", Itascacg.com, Minneapolis, USA: Itasca, retrieved 27 July 2009
  43. ^ "PFC3D - Particle Flow Code in Three Dimensions", Itascacg.com, Minneapolis, USA: Itasca, retrieved 27 July 2009
  44. ^ Van der Meij, R. (25 May 2010). "A Genetic Algorithm for Solving Slope Stability Problems: From Bishop to a Free Slip Plane". Numerical Methods in Geotechnical Engineering. 4: 345–350. ISBN 9780203842362.
  45. ^ Bar, N.; Barton, N.R. (2017). "The Q-slope Method for Rock Slope Engineering". Rock Mechanics & Rock Engineering, Vol 50, Springer, Vienna, https://doi.org/10.1007/s00603-017-1305-0.

BibliographyEdit

External linksEdit