Pore pressure due to capillary rise

In summary, the conversation discusses the presence of pore pressure due to capillary rise at different points in the soil. The author believes that there should also be pore pressure at points A and D, while the other person argues that there is no capillary pressure at those points because they are either above or below the water table. The conversation also clarifies that point B is the top of the region containing water in some of the pores, hence why there is capillary pressure there.
  • #1
tzx9633

Homework Statement


Why there's no pore pressure due to capillary rise at point A and point D ? There's only pore pressure due to capillary rise at B ..

Homework Equations

The Attempt at a Solution


i think the author is wrong . There's should be also ore pressure due to capillary rise at A and D . Because the capillary rise can occur anywhere in the soil .
 

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  • #2
tzx9633 said:

Homework Statement


Why there's no pore pressure due to capillary rise at point A and point D ? There's only pore pressure due to capillary rise at B ..

Homework Equations

The Attempt at a Solution


i think the author is wrong . There's should be also ore pressure due to capillary rise at A and D . Because the capillary rise can occur anywhere in the soil .
Can you please define the variables in your equations.
 
  • #3
Chestermiller said:
Can you please define the variables in your equations.
Huh , what do you mean ?

It's the pore water pressure due to capillary rise , u = -s(yw)(H2)
 
  • #4
There is no water in the pores at A; it is above the saturation zone. At D, the pores are all fully saturated, because it is below the water table, and there is no capillary pressure there because there is no free surface (between air and water) in this zone. So the author is correct.
 
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  • #5
Chestermiller said:
there is no capillary pressure there because there is no free surface (between air and water) in this zone. So the author is correct.
Having said that there's capillary rise at B , means that there is free surface (between air and water) in this zone ?

I didnt see there's air at B , can you explain further ?
 
  • #6
tzx9633 said:
Having said that there's capillary rise at B , means that there is free surface (between air and water) in this zone ?
Sure.
I didnt see there's air at B , can you explain further ?
What do the words "50% saturated" mean to you?
 
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  • #7
Chestermiller said:
Sure.

What do the words "50% saturated" mean to you?
ok , noted . Why there is no pore pressure due to capillary rise at C ?
 
  • #8
tzx9633 said:
ok , noted . Why there is no pore pressure due to capillary rise at C ?
At C and below, the pores are completely full of water.
 
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  • #9
Chestermiller said:
There is no water in the pores at A; it is above the saturation zone. At D, the pores are all fully saturated, because it is below the water table, and there is no capillary pressure there because there is no free surface (between air and water) in this zone. So the author is correct.
How do you know that there's no water at A ? How do you know that there's water at B ?
 
  • #10
tzx9633 said:
How do you know that there's no water at A ? How do you know that there's water at B ?
The figure implies that, between A and B, there is dry sand and between B and C, there is partially saturated sand. So, B is the top of the region containing water in some of the pores.
 
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1. What is pore pressure due to capillary rise?

Pore pressure due to capillary rise refers to the upward force exerted by the movement of water through small pores in a material, such as soil or rock. This pressure can cause changes in the stability and behavior of the material, and is important to consider in engineering and geology.

2. How does capillary rise affect soil stability?

Capillary rise can significantly impact soil stability by increasing pore pressure and reducing the effective stress within the material. This can lead to decreased shear strength and potential failure of the soil, especially in areas with high saturation and low permeability.

3. What factors influence the magnitude of pore pressure due to capillary rise?

The magnitude of pore pressure due to capillary rise is influenced by several factors, including the pore size and distribution within the material, the moisture content, and the surface tension of the water. The type of material and its porosity also play a role in determining the amount of pore pressure generated.

4. How is pore pressure due to capillary rise measured?

Pore pressure due to capillary rise can be measured using various techniques, such as tensiometers, pressure transducers, or suction probes. These instruments measure the tension or pressure of the water within the material and can provide valuable data for understanding the behavior of the material under different conditions.

5. What are the implications of pore pressure due to capillary rise in engineering projects?

Pore pressure due to capillary rise must be carefully considered in engineering projects, particularly in areas with high groundwater levels or low-permeability soils. It can affect the stability and strength of the material, leading to potential failure or settlement. Proper drainage and soil compaction techniques can help mitigate the effects of capillary rise on engineering projects.

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