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Slope stability I EOSC316 Engineering Geoscience.

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Presentation on theme: "Slope stability I EOSC316 Engineering Geoscience."— Presentation transcript:

1 Slope stability I EOSC316 Engineering Geoscience

2 Landslip trigger processes Water Toe removal –Natural –Artificial Head loading Vibration

3 Folkestone Warren, Kent Toe erosion due to extension of harbour wall, 1905 Since 1915 slide –mass concrete toe weights –drainage adits

4 Mt. Huascaran, Peru, 1970 earthquake triggered hit towns of Yungay and Ranrahirca, 18 km away, at around 150 km/hr Yungay completely buried, 66,000 dead

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6 Types of landslide Rock failure –failure plane pre- determined Soil failure –failure plane along line of max stress

7 Rock failure

8 Planar translational slip in rock  = angle of repose (= angle of friction) Factor of safety = shear force at failure / shear force

9 Wedge failure in rock

10 Toppling failure, Masada, Israel

11 Effect of cohesive strength on bench height in rock Shear stress on sliding plane: Failure occurs when: Thus Area of wedge

12 Half dome, YosemiteCarrara marble quarries, Italy

13 Rock failure – remedial measures

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18 Slope failure in ‘unconsolidated’ material

19 Planar versus rotational slip in unconsolidated material Planar slip –frictional –cohesionless –C = 0 Rotational slip –frictional –cohesional –C ≠ 0

20 La Conchita, Santa Barbara, California, Spring 1995

21 Planar translational slip  = angle of repose (= angle of friction) Factor of safety = shear force at failure / shear force

22 Planar slip - analysis

23 Planar slip in soils Cohesionless soils (φ=0) Soils with cohesion (φ≠0)


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