Pregunta
- 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
located 1 m below the surface.
Calculate the total stress (
depths of:
a) 1 m
b) 3 m
c) 5 m
Ask by Peterson Hampton. in Rwanda
Jan 10,2025
Solución de inteligencia artificial de Upstudy
Respuesta verificada por el tutor
Responder
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:
-
Total Stress (σ):
- Definition: The total stress at a depth
is the weight of the soil (and water, if present) above that point. - Formula:
- Definition: The total stress at a depth
-
Pore Water Pressure (u):
- Definition: The pressure exerted by water within the pores of the soil.
- Formula:
-
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,
- Since
-
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.
Respondido por UpStudy AI y revisado por un tutor profesional
Como
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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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