Pore pressure due to capillary rise

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SUMMARY

The discussion centers on the concept of pore pressure due to capillary rise in soil mechanics, specifically questioning why there is no pore pressure at points A and D while it exists at point B. The consensus is that at point A, the soil is above the saturation zone, resulting in no pore water pressure, while at point D, the soil is fully saturated below the water table, eliminating capillary pressure due to the absence of a free surface. The correct understanding of these conditions is critical for soil analysis.

PREREQUISITES
  • Understanding of soil saturation levels and capillary rise
  • Knowledge of pore water pressure concepts in geotechnical engineering
  • Familiarity with soil mechanics terminology
  • Ability to interpret soil profiles and saturation zones
NEXT STEPS
  • Study the principles of capillarity in soils
  • Learn about the effects of soil saturation on pore pressure
  • Explore the relationship between soil texture and capillary rise
  • Investigate methods for measuring pore water pressure in the field
USEFUL FOR

Geotechnical engineers, soil scientists, and students studying soil mechanics who need to understand the dynamics of pore pressure and capillary rise in soil profiles.

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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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.
 
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)
 
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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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 ?
 
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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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 ?
 
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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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 ?
 
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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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