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ENCE 3610 Soil Mechanics Lecture 13 Slope Stability

Overview of Slope Stability Types of Slope Failure Slope failure is one of the most important types of failure in geotechnical engineering As opposed to other types of failure (especially settlement,) slope failures are generally catastrophic Slope failures in Sweden in early 1900 s led to development of one of the first analytic methods of geotechnical analysis rotational failure analysis using slip circle and method of slices Falls (rock falls) generally by surface rock Topples rotation of rock away from a vertically inclined joint or fissure Slides Rotational slides the classic mode of slope failure, rotational failure along a circular (or nearly so) surface Translational slides failure along a planar surface Spreads like translational slide, except material separates and moves apart as it moves downward Flows material comes down in nearly liquid form includes avalanches

Aspects of Slope Stability Analysis Limit equilibrium analysis Evaluate the slope as if it were about to fail and determine the shear strength along the surface Computed stresses are compared to the shear strength to determine the factor of safety Same concept used in bearing capacity analysis of shallow and deep foundations Effective Stress vs. Total Stress Analyses Generally, effective stress analysis is used in slope stability Total stress analysis used when excess pore water pressures are present Critical failure surface Validity of analysis depends upon choosing correct failure surface (surface of lowest factor of safety) Trial and error problem; computer program makes search much more effective

Plasticity Theory: Upper and Lower Bound

Vertical Slope in Cohesive Soils Lower Bound Solution

Vertical Slope in Cohesive Soils Upper Bound Solution

Critical Height and Slope Stability Number Critical Height Critical height is found between upper and lower bounds Slope Stability Number Rearranging and redefining the coefficient γh N o= c Adding a factor of safety γh N o=f s c 2c 4c γ <h cr < γ Values have also been determined between these two Obviously the lower bound is the most conservative

Planar Failure Surfaces Most slope stability analyses (including circular) are two dimensional, i.e, they assume the slope is infinitely long with the same profile Infinite Slope Analysis Failure surface is under the slope and also parallel to it Usually one when a weak layer is above a hard (bedrock) layer Planar failure analysis Failure surface is under the slope but not parallel to it

General Case of Planar Slope Failure

Infinite Slope Only valid for purely cohesionless soils Only valid for the case where the slope and the failure surface are parallel Only valid when water table is not significant Result independent of unit weight Slope stability degraded in the case when water is flowing down the slope or in a purely horizontal direction (earth dams)

Soil With Steady-State Seepage

Infinite Slope Example Given Infinite Slope, H =15, α = 20 deg. Soil, = 10 deg., c = 500 psf, = 110 pcf, saturated w/seepage Find Factor of safety for translational failure Solution Substituting into the equation below, FS = 1.15

Methods of Failure Analysis for Rotational Failure Friction Circle Method Methods of Slices Fellenius Method Chart Solutions (Ordinary Method) Taylor s Stability Bishop Method Number (Simplified) Janbu Charts (DM 7.01) Spencer A good way for Morganstern-Price GLE preliminary The classic way to calculations analyse slope stability, Non-circular failure surfaces Vertical Slopes but computationally intensive by hand Finite Element Methods

Limit Equilibrium Method (Method of Slices)

Limit Equalibrium and Circular Slope Failure

Fellenius Method

Bishop s Method

Slope Stability Charts (Janbu)

Example of Chart Solution Given: Slope cu = 40 kpa γ = 17.5 kn/m3 β = 60 Find Maximum depth of excavation without slope failure Radius of critical circle when factor of safety is unity Distance from crown of slope to slip circle at top of slope

Example of Chart Solution Solution From chart, Stability Number No = 5.2 Assume FS = 1 (for maximum possible height) Solving for H, H = cno/ (γfs) = (40)(5.2)/((17.5) (1)) = 11.89 m Note that, from portion of chart used, we have a toe circle

Example of Chart Solution Solution H = 11.89 m From x-abcissa curve, xo = 0 From y-abcissa curve, yo = 1.5H = (1.5)(11.89) = 17.8m To find the distance of the slip circle at the top of the slope, construct a triangle: Horizontal Leg = 17.8 11.89 = 5.9 m Hypotenuse = radius of circle = 17.8 m Vertical leg = 16.8 m Width of slope = H cot β = (11.89)(cot 60 ) = 6.86 Distance from slope crest to slip circle = 16.8 6.86 = 9.9 m

Limit Equilibrium Method (Method of Slices)

Modified Bishop's Method

Modified Bishop Method Same as Fellenius Method except that it includes normal forces along sides of slices Problem becomes statically indeterminate as a result of this and requires an iterative solution Results tend to result in higher factors of safety than the Fellenius method

Example Using Bishop's Method

Use of Computer Software Automates many of the processes that are required for slope analysis Eliminates the need for iterative solutions Enables running multiple cases and varying parameters without difficulty

Other Types of Rotational Analysis Spencer Assumes forces on the sides of the slices are parallel Solves for both moment and force equation on slices Morganstern-Price Imposes normal and shear forces on the sides of the slices Includes water pressure effects Both methods require equilibrium of forces on each slice Morganstern Rapid Drawdown Method

Solutions to Slope Stability Problems

Other Solutions Lightweight fill Retaining Walls Especially useful when space for a slope is limited Tieback anchors and soil nailing Improvement of drainage Geogrids and Mechanically Stabilized Earth (MSE) walls

Pile Stabilised Slopes

Questions?