Pregunta
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  1. A soi-layer is fully saturated with a unit weight of and a water table
    located 1 m below the surface.
    Calculate the total stress ( ), pore water pressure (u), and effective stress ( ) at
    depths of:
    a) 1 m
    b) 3 m
    c) 5 m

Ask by Peterson Hampton. in Rwanda
Jan 10,2025

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At 1 m depth:
  • Total Stress (σ): 20 kPa
  • Pore Water Pressure (u): 0 kPa
  • Effective Stress (σ′): 20 kPa
At 3 m depth:
  • Total Stress (σ): 60 kPa
  • Pore Water Pressure (u): 20 kPa
  • Effective Stress (σ′): 40 kPa
At 5 m depth:
  • Total Stress (σ): 100 kPa
  • Pore Water Pressure (u): 40 kPa
  • Effective Stress (σ′): 60 kPa

Solución

To determine the total stress (σ), pore water pressure (u), and effective stress (σ′) at various depths within the soil layer, we’ll follow a systematic approach based on soil mechanics principles.

Given Data:

  • Unit Weight of Fully Saturated Soil (γ): 20 kN/m³
  • Water Table Depth: 1 m below the surface
  • Unit Weight of Water (γ₍w₎): Typically, γ₍w₎ = 10 kN/m³

Key Concepts:

  1. Total Stress (σ):
    • Definition: The total stress at a depth is the weight of the soil (and water, if present) above that point.
    • Formula:
  2. Pore Water Pressure (u):
    • Definition: The pressure exerted by water within the pores of the soil.
    • Formula:
  3. Effective Stress (σ′):
    • Definition: The stress carried by the soil skeleton, crucial for assessing soil stability.
    • Formula:

Calculations for Each Depth:

a) Depth = 1 m

  • Total Stress (σ):
  • Pore Water Pressure (u):
    • Since Water Table Depth,
  • Effective Stress (σ′):

b) Depth = 3 m

  • Total Stress (σ):
  • Pore Water Pressure (u):
  • Effective Stress (σ′):

c) Depth = 5 m

  • Total Stress (σ):
  • Pore Water Pressure (u):
  • Effective Stress (σ′):

Summary of Results:

Depth (m) Total Stress σ (kPa) Pore Water Pressure u (kPa) Effective Stress σ′ (kPa)
1 20 0 20
3 60 20 40
5 100 40 60

Conclusion:

At each specified depth, the total stress increases linearly with depth, while the pore water pressure starts to contribute only below the water table (1 m). Consequently, the effective stress, which is crucial for understanding soil behavior under load, increases with depth but at a slower rate due to the influence of pore water pressure.

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Mind Expander

At a depth of 1 m, which is at the water table, the total stress ( ) is calculated as the unit weight of the soil times the depth, so . The pore water pressure ( ) at this depth is 0, since it’s at the water table. The effective stress ( ) is then .
At a depth of 3 m, total stress is . The pore water pressure ( ) can be calculated as the unit weight of water (≈ 10 kN/m³) times the depth below the water table, so at 2 m (3 m - 1 m), . The effective stress is .
At a depth of 5 m, total stress is . For the pore water pressure, at 4 m below the water table (5 m - 1 m), . Thus, the effective stress is .
In summary:
  • At 1 m:
  • At 3 m:
  • At 5 m:

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