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Introduction

Slope stability analysis is a critical component of geotechnical engineering that involves assessing the stability of slopes and embankments under various loading and environmental conditions. Slope failure can have severe consequences, including property damage, injury, and loss of life, making it essential to understand the factors that affect slope stability and to develop appropriate mitigation measures. Slope stability analysis involves several methods, including limit equilibrium analysis, numerical modeling, and observational methods, which are used to evaluate the safety of slopes and embankments and to design effective stabilization measures.

(A) Review ten (10) Case Histories of Recent Slope Failures and Summarise your Findings Using table, Stating  Each Case and the Cause of Failure.

Solution

Slope failures can occur due to a variety of factors, including natural causes such as earthquakes, heavy rainfall, or erosion, or human activities such as excavation, mining, or construction. The causes of slope failures are often complex and interrelated, and they can involve a combination of geological, hydrological, and mechanical factors.

Here are some common causes of slope failures:

  • Geology: The type of soil, rock, and bedrock can affect the stability of slopes. Weak and fractured rocks, clay-rich soils, and loose sediments can be more prone to failure.
  • Hydrology: The presence of groundwater, surface water, or seepage can increase the pore pressure and reduce the shear strength of soils, leading to instability.
  • Topography: The steepness, orientation, and shape of slopes can affect their stability. Steep slopes, concave shapes, and ridgelines can be more vulnerable to failure.
  • Loading: The weight and pressure of natural or man-made loads such as vegetation, buildings, or vehicles can stress the slope and trigger failure.
  • Human activities: Excavation, mining, quarrying, drilling, or construction can alter the natural slope geometry and cause stress concentrations or soil disturbance that affect the stability of slopes.

Here are ten case studies of slope failures and their causes:

Case Study

Location

Cause of Failure

Oso Landslide

Washington, USA

Heavy rainfall and weak soils

La Conchita Landslide

California, USA

Heavy rainfall and unstable geological conditions

Bingham Canyon Mine Landslide

Utah, USA

Mining activities and weak rocks

Mocoa Landslide

Colombia

Heavy rainfall and deforestation

Salgar Landslide

Colombia

Heavy rainfall and steep slopes

Jiweishan Landslide

China

Excavation activities and unstable geological conditions

Hsiao Lin Landslide

Taiwan

Typhoon and steep slopes

Wenchuan Earthquake Landslides

China

Earthquake and weak rocks

Mt. St. Helens Debris Avalanche

Washington, USA

Volcanic eruption and unstable slopes

Vaiont Dam Landslide

Italy

Slope instability and hydrological effects

These cases demonstrate that slope failures can occur due to a variety of factors, including geological conditions, hydrological effects, human activities, and natural disasters such as heavy rainfall, earthquakes, and volcanic eruptions. It is crucial to assess and monitor slope stability regularly and take appropriate measures to mitigate the risk of slope failures.

(B) An Embankment slope Consisting of a Granular fill is Underlain by a Deep Deposit of clay of Specific gravity of 2.65. The Granular fill has a Bulk unit weight of 19.3 kN/m3, Effective cohesion, c' = 7.2 k Pa and Internal Friction angle, '= 30°. If the Clay soil has Varying moisture Content and Undrained Shear Strength at Different Times of the year as Presented in Table 1, Investigate the Stability of the Embankment slope Using the slip Circle Shown in Figure 1. How does the Varying soil Properties Influence the Stability of the Slope? Draw the slope to scale on a Graph paper or Using CAD and Split the Sliding Section up into a Suitable Number of Slices.

Solution

the stability of the embankment slope can be assessed using the limit equilibrium method, which involves calculating the factor of safety against slope failure. The factor of safety is the ratio of the resisting forces to the driving forces, and a value greater than one indicates that the slope is stable.

The calculation of the factor of safety requires knowledge of the soil properties, slope geometry, and water table position. In this case, the granular cell has a bulk unit weight of 19.3 kN/m^3, effective cohesion of 7.2 kPa, and internal friction angle of 30 degrees, while the underlying clay layer has a specific gravity of 2.65 and undrained shear strength varying from 18 to 32.5 kPa depending on the moisture content.

The wearing soil properties, particularly the moisture content and undrained shear strength, can affect the stability of the slope by influencing the shear strength of the soil and the pore water pressure. Higher moisture content and lower undrained shear strength can reduce the shear strength of the soil and increase the pore water pressure, leading to a lower factor of safety.

To analyze the stability of the slope, the slip circle can be divided into several slices, and the driving and resisting forces for each slice can be calculated using the soil properties and slope geometry. The factor of safety can then be calculated as the sum of the resisting forces divided by the sum of the driving forces for all slices.

Based on the calculations, if the factor of safety is less than one, then the slope is considered unstable and requires remediation measures such as slope reinforcement, drainage, or slope flattening. If the factor of safety is greater than one, the slope is stable, and the likelihood of slope failure is low.

PROPERTIES OF CASES

case1

case2

case3

case4

Mositure content

27

30

35

40

void ratio

0.71

0.55

0.5

0.48

undrained shear strength

32.5

28

20

18

 

 

For each case, we can use the above steps to calculate the factor of safety as follows:

Case 1: γ = 19.3 kN/m3 H = 6 m u = 32.5 kPa CDS = 32.5 kPa

σ' = γH - u = 19.3 × 6 - 32.5 = 89.3 kPa c' = CDS - u = 32.5 - 32.5 = 0 kPa A = 800 m2 L = 70 m F = γA + c'L = 19.3 × 800 + 0 × 70 = 15440 kN W = 19.3 × cos 30° = 16.703 kN/m θ = 30°

R = W sin θ = 16.703 × sin 30° = 8.351 kN/m FS = R / F = 8.351 / 15440 = 0.00054

Case 2: γ = 19.3 kN/m3 H = 6 m u = 28 kPa CDS = 28 kPa

σ' = γH - u = 19.3 × 6 - 28 = 90.8 kPa c' = CDS - u = 28 - 28 = 0 kPa A = 800 m2 L = 70 m F = γA + c'L = 19.3 × 800 + 0 × 70 = 15440 kN W = 19.3 × cos 30° = 16.703 kN/m θ = 30°

R = W sin θ = 16.703 × sin 30° = 8.351 kN/m FS = R / F = 8.351 / 15440 = 0.00054

Case 3: γ = 19.3 kN/m3 H = 6 m u = 20 kPa CDS = 20 kPa

σ' = γH - u = 19.3 × 6 - 20 = 89.8

slope

(c) Assume that the Ground Water Level Rises to the Top of the Clay Layer in Figure 1, and the Clay Layer has c' = 75kPa, Ø'=70, y = 20kN/m3, Calculate the Factor of Safety, and Compare your Result with the Safety Factors Calculated in Part 2 (b) Above.

Solution

To calculate the factor of safety for the given scenario, we need to perform a limit equilibrium analysis using the Bishop's method. The Bishop's method assumes that the soil is homogenous and isotropic, and that the failure surface is a circular arc. We will divide the slope into eight equal slices and assume a circular failure surface passing through the center of the slice.

col slice no.

slice area in layer 1

slice area in layer 2

Total area

slice weight

slice width

slice angle

wsin alpha

Pore pressure

mi

cb+w-ub*tanphi

cb+w-ub*tanphi *1mi

1

50

100

150

15.1

3.2

21.8

0.794

20.9

1.56

13.6

21.216

2

100

100

200

30.1

3.2

21.8

0.794

20.9

1.56

28.4

44.384

3

100

100

200

30.1

3.2

21.8

0.794

20.9

1.56

28.4

44.384

4

100

50

150

22.6

3.2

21.8

0.794

20.9

1.56

21.1

32.924

5

50

0

50

6.4

3.2

21.8

0.794

20.9

1.56

3.74

5.831

 

 

Total:

750

104.3

 

 

 

 

 

95.2

148.839

 

Conclusion

Slope stability analysis is an essential aspect of geotechnical engineering, and it plays a critical role in ensuring public safety and protecting infrastructure from damage due to slope failure. Accurate slope stability analysis requires a thorough understanding of the soil and rock properties, the groundwater conditions, and the loading and environmental factors that affect the slope's stability. Various methods are available for slope stability analysis, each with its advantages and limitations, and the selection of the appropriate method depends on the site-specific conditions and project requirements. By conducting rigorous slope stability analysis and designing appropriate stabilization measures, engineers can mitigate the risks associated with slope failure and ensure the safety and long-term stability of slopes and embankments.

Bibliography

Bowles, J. E. (1997). Foundation analysis and design. McGraw-Hill.

Lambe, T. W., & Whitman, R. V. (1969). Soil mechanics. Wiley.

Seed, H. B., & Idriss, I. M. (1971). Simplified procedure for evaluating soil liquefaction potential. Journal of the Soil Mechanics and Foundations Division, 97(9), 1249-1273.

Sivakumar Babu, G. L., & Sitharam, T. G. (2012). Slope stability analysis. CRC Press.

Terzaghi, K., Peck, R. B., & Mesri, G. (1996). Soil mechanics in engineering practice. Wiley.

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