0
GEOTECHNICAL ENGINEERING - II
Engr. Nauman Ijaz

LATERAL EARTH PRESSURE

Chapter # 04
UNIVERSITY OF SOUTH ASIA
LATERAL EARTH
PRESSURE
Lateral Earth pressure is an important
parameter for the design of bridge abutment,
different types...
GRAVITY RETAINING
WALL
CANTILEVER WALL
COUNTERFORT OR BUTTRESS
RETAINING WALL
SHEET PILES
BRIDGE ABUTMENT
LATERAL EARTH PRESSURE
AND WALL MOVEMENT
Lateral earth pressure are the direct
result of horizontal stresses in the soil.
...
COEFFICIENT OF LATERAL
EARTH PRESSURE “K”
It is defined as the;
“Ratio of the horizontal effective stress to the
vertical ...
1.
2.
3.

K is important because it is an indicator
of the lateral earth pressures acting on
retaining wall.
For purpose o...
Two classic Earth pressure theories has
been put forward in the eighteen and
nineteen centuries by Coulomb and Rankine
res...
Consider an element of soil at depth z
below the ground surface level (GSL) as
shown in the figure.
The vertical stress du...
Figure # (a)
Figure # (b)
When confined (as in general case
below GSL due to the pressure of
surrounding soil), this vertical
stress,(σz) will tend ...
The ratio of σx to σz is termed as the co-efficient
of earth pressure at rest and denoted by Ko.
Thus;
Ko = σx / σz = σ3 /...
Φ’
= Effective angle of internal friction.
OCR = Over-consolidation Ratio.
For normally consolidated soils, the equation(b...
TYPICAL VALUES OF Ko
SOIL TYPE

Ko

LOOSE SAND

0.59

DENSE ASND

0.36

NORMALLY CONSOLIDATED CLAY

0.56 – 0.80

PRECONSOL...
ACTIVE CASE
Consider the figure (b), if the wall moves
away from the backfill the soil expands and
the confining stress, σ...
This condition of wall movement is
said to generate an active stress
condition and the ratio σx / σz is
defined as the act...
PASSIVE CASE
When the wall moves towards the backfill,
and against the soil mass, the soil will be
subjected to lateral co...
where,
Kp = the coefficient of Passive Earth
pressure.
Thus soil can exist in any condition ranging
from the active, throu...
DIAGRAMTIC RELATIONSHIP
BETWEEN THE LATERAL STRAIN AND
LATERAL EARTH PRESSURE
RANKINE THEORY (1857)
In original form the theory was
developed for purely non-cohesive
soils (i.e. c = 0), but subsequent...
ASSUMPTIONS
1.

2.
3.
4.
5.

Soil is non-cohesive (c = 0) dry, isotropic
and homogenous.
Backfill is horizontal.
Wall is v...
Soil Element : Rankine Theory
Vertical Stress = σ’z = γz

Major Principal stress.

At failure Horizontal stress , σ’x

Minor Principal Stress.
From ∆OAB,
SinΦ = AB/OB = ½(σz – σx)
½(σz + σx)
SinΦ(σz + σx) = (σz – σx)
σz (1 – SinΦ) = σx (1 + SinΦ)
Ka = σx / σz = (1 ...
Similarly, passive earth pressure,
Kp = tan² (45 – Φ/2) and,
σp = γz tan² (45 + Φ/2)

m.irfan B-15952
Upcoming SlideShare
Loading in...5
×

Geotech. Engg. Ch#04 lateral earth pressure

1,851

Published on

Published in: Education, Technology, Business
0 Comments
2 Likes
Statistics
Notes
  • Be the first to comment

No Downloads
Views
Total Views
1,851
On Slideshare
0
From Embeds
0
Number of Embeds
0
Actions
Shares
0
Downloads
175
Comments
0
Likes
2
Embeds 0
No embeds

No notes for slide

Transcript of "Geotech. Engg. Ch#04 lateral earth pressure"

  1. 1. GEOTECHNICAL ENGINEERING - II Engr. Nauman Ijaz LATERAL EARTH PRESSURE Chapter # 04 UNIVERSITY OF SOUTH ASIA
  2. 2. LATERAL EARTH PRESSURE Lateral Earth pressure is an important parameter for the design of bridge abutment, different types of retaining walls (Such as gravity retaining walls, cantilever walls, counterforts or buttresses), sheet piles and other retaining structures.
  3. 3. GRAVITY RETAINING WALL
  4. 4. CANTILEVER WALL
  5. 5. COUNTERFORT OR BUTTRESS RETAINING WALL
  6. 6. SHEET PILES
  7. 7. BRIDGE ABUTMENT
  8. 8. LATERAL EARTH PRESSURE AND WALL MOVEMENT Lateral earth pressure are the direct result of horizontal stresses in the soil. In order to understand the lateral earth pressure we have to define the Coefficient of lateral earth pressure, K.
  9. 9. COEFFICIENT OF LATERAL EARTH PRESSURE “K” It is defined as the; “Ratio of the horizontal effective stress to the vertical effective stress at any point in a soil.” K = σ’x / σ’z K = Coefficient of lateral earth pressure. σ’x = Horizontal effective stresses. σ’z = Vertical effective stresses.
  10. 10. 1. 2. 3. K is important because it is an indicator of the lateral earth pressures acting on retaining wall. For purpose of describing lateral earth pressures, geotechnical engineers have defined three important soil conditions; At – rest Condition The Active Condition Passive condition
  11. 11. Two classic Earth pressure theories has been put forward in the eighteen and nineteen centuries by Coulomb and Rankine respectively. 1) Rankine (1857) Earth Pressure Theory 2) Coulomb’s(1776) Earth Pressure Theory These two theories are still in use in their original form and in some modified forms to calculate the earth pressure.
  12. 12. Consider an element of soil at depth z below the ground surface level (GSL) as shown in the figure. The vertical stress due to the self weight of soil, σ’z (also known as overburden pressure or gravitational stress) is given by; σ’z = γz Where; γ = unit weight of in-situ soil
  13. 13. Figure # (a)
  14. 14. Figure # (b)
  15. 15. When confined (as in general case below GSL due to the pressure of surrounding soil), this vertical stress,(σz) will tend to cause the expansion of soil element and in doing so a secondary lateral pressure is generated. These vertical (σz) and horizontal (σx) stresses are the major and minor principal stresses in this particular case respectively.
  16. 16. The ratio of σx to σz is termed as the co-efficient of earth pressure at rest and denoted by Ko. Thus; Ko = σx / σz = σ3 / σ1………..(a) Ko value in general is variable and depends upon t soil type and its history of deposition Numerous relations have been derived for its evaluation, but the following relationships given by Jaky (1948) is commonly used; Ko = 1 – SinΦ’ under root(OCR)……(b)
  17. 17. Φ’ = Effective angle of internal friction. OCR = Over-consolidation Ratio. For normally consolidated soils, the equation(b) is reduced to; Ko = 1 – SinΦ’
  18. 18. TYPICAL VALUES OF Ko SOIL TYPE Ko LOOSE SAND 0.59 DENSE ASND 0.36 NORMALLY CONSOLIDATED CLAY 0.56 – 0.80 PRECONSOLIDATED CLAY >1
  19. 19. ACTIVE CASE Consider the figure (b), if the wall moves away from the backfill the soil expands and the confining stress, σx gradually decreases. If the movement is sufficiently large the σx will decrease to minimum value and the state of equilibrium will then attained. As σz > σx in this case, σz is the major principal stress and σx is the minor principal stress.
  20. 20. This condition of wall movement is said to generate an active stress condition and the ratio σx / σz is defined as the active earth pressure co-efficient, Ka. Thus: Ka = σx / σz = σ3 / σ1
  21. 21. PASSIVE CASE When the wall moves towards the backfill, and against the soil mass, the soil will be subjected to lateral compression. Under this condition, σx is the principal stress and σz becomes the minor principal stress. this condition is known as Passive Earth Pressure condition and ratio is given by; Kp = σx / σz = σ1 / σ3
  22. 22. where, Kp = the coefficient of Passive Earth pressure. Thus soil can exist in any condition ranging from the active, through the at rest to the passive state.
  23. 23. DIAGRAMTIC RELATIONSHIP BETWEEN THE LATERAL STRAIN AND LATERAL EARTH PRESSURE
  24. 24. RANKINE THEORY (1857) In original form the theory was developed for purely non-cohesive soils (i.e. c = 0), but subsequently Bell (1915) extended this theory to c-Φ soil as well.
  25. 25. ASSUMPTIONS 1. 2. 3. 4. 5. Soil is non-cohesive (c = 0) dry, isotropic and homogenous. Backfill is horizontal. Wall is vertical, Wall friction is neglected. Failure is a plain strain problem. Consider a unit length of an infinitely long wall.
  26. 26. Soil Element : Rankine Theory
  27. 27. Vertical Stress = σ’z = γz Major Principal stress. At failure Horizontal stress , σ’x Minor Principal Stress.
  28. 28. From ∆OAB, SinΦ = AB/OB = ½(σz – σx) ½(σz + σx) SinΦ(σz + σx) = (σz – σx) σz (1 – SinΦ) = σx (1 + SinΦ) Ka = σx / σz = (1 – SinΦ) = tan² (45 – Φ/2) (1 + SinΦ) and σx = active earth pressure = σz Ka σa = γz tan² (45 – Φ/2)
  29. 29. Similarly, passive earth pressure, Kp = tan² (45 – Φ/2) and, σp = γz tan² (45 + Φ/2) m.irfan B-15952
  1. A particular slide catching your eye?

    Clipping is a handy way to collect important slides you want to go back to later.

×