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Shear strength
 Shear strength is a term used in soil mechanics to describe the magnitude of
the shear stress that a soil can sustain.
 The shear resistance of soil is a result of friction and interlocking of particles,
and possibly cementation or bonding at particle contacts.
 Shear failure occurs when the stresses B/W the particles are such that they
slide or roll past each other
Types of shear failure
 General shear failure
 Local shear failure
 Punching shear failure
shear failure
Shear Strength in Soils parameters
 Soil derives its shear strength from two sources:
 Cohesion (C)
 Frictional resistance (ϕ)
Cohesion (C)
 The attraction between the molecules of the same material is called cohesion.
 Cohesion (C), is a measure of the forces that cement particles of soils
 Dry sand is cohesion less.
 Addition of water in the dry and induces, a little cohesion in it.
 Clayey soil has maximum cohesion
 The cohesion of soil depends on:
 1. Fineness of clay particles
 2.Amount of clay
 3.Water content of soil
Internal Friction(ϕ)
Internal friction
 The frictional resistance between the individual soil particles at their contact
point is known as internal friction.
Angle of Internal friction : Ф
 It represents the frictional resistance between the soil particles, which is
directly proportional to the normal stress
Cohesion less soil (Ф- Soil)
 These are the soils which do not have cohesion.
(C=0)
 These soils derive the shear strength from the
intergranular friction.
 These soils are also called frictional soils.
 Examples: Sands and gravels.
 Equation for strength
is, S= σ . Tan Ф
Mohr-Coulomb Failure Criteria
 This theory states that a material fails because of a critical combination of
normal stress and shear stress, and not from their either maximum normal
or shear stress alone.
 The relationship between normal stress and shear is given as
 s = c¢ +s ¢ tanf ¢
 angle of internal friction
 c cohesion
 s shear strength
Shear
Strength,S
Normal Stress, n =  =  h
C
 = 
Mohr-Coulomb Failure
Criterion
Mohr-Coulomb Failure Criterion
’f
f
’
Shear strength consists of two
components: cohesive and frictional.

'
c’
’f tan ’
c’
 f  c''f tan'
Mohr-Coulomb Failure Criterion
(in terms of total stresses)

f is the maximum shear stress the soil can take without
failure, under normal stress of .

c
 f  c  tan

f

f is the maximum shear stress the soil can take without
failure, under normal effective stress of ’.
Mohr-Coulomb Failure Criterion
(in terms of effective stresses)

’
c’
 f  c' 'tan'
’
Effective
cohesion Effective
friction angle
f
’
 '
  u
u = pore water
pressure
4
MOHR CIRCLE OF STRESS

’
'
' '
1 3
2
m
1 3
2
'
'
'
3
 1
'

PP = Pole w.r.t.plane

’
’
’ ’
' 

Major principal stress: σ1
Minor principal stress: σ3
Mean principal stress: σm
Maximum shear stress: τmax
max ’ 
2 2
   
 
2

2
2
 1 3
  1 3

Equation of Mohr Circle
Compare it’s formulation with equation of circle
MOHR CIRCLE AND FAILURE ENVALOPE
Failure surface
X X
Y
Y
Soil elements at different locations
Y ~ stable
X ~ failure


’
  ctan
f
MOHR CIRCLE AND FAILURE ENVALOPE
Y h
h
Mohr circle before
external loading
v
 +
Soil element does not fail if the Mohr circleis
contained within the envelope
GL

v
v

MOHR CIRCLE AND FAILURE ENVALOPE
Y
h
GL
As loading progresses, Mohr
circle becomes larger…
.. and finally failure occurs
when Mohr circle touches
the envelope

v
h
v
MOHR CIRCLE IN TERMS OF TOTAL AND
FFECTIVE STRESSES
X
h’
X
u
u
= +
h’
u
v
v’ h
X
v v’
h

 or ’
If X is on
failure
Failure envelope in
terms of total stresses

c’ c
Failure envelope in terms
of effective stresses
’
Effective Stresses Total Stresses
MOHR-COULOMB FAILURE CRITERION WITH
MOHR CIRCLE OF STRESS
Shear Strength Parameters and types.pptx
Shear Strength Parameters and types.pptx

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Shear Strength Parameters and types.pptx

  • 1.
  • 2. Shear strength  Shear strength is a term used in soil mechanics to describe the magnitude of the shear stress that a soil can sustain.  The shear resistance of soil is a result of friction and interlocking of particles, and possibly cementation or bonding at particle contacts.  Shear failure occurs when the stresses B/W the particles are such that they slide or roll past each other
  • 3. Types of shear failure  General shear failure  Local shear failure  Punching shear failure
  • 5. Shear Strength in Soils parameters  Soil derives its shear strength from two sources:  Cohesion (C)  Frictional resistance (ϕ)
  • 6. Cohesion (C)  The attraction between the molecules of the same material is called cohesion.  Cohesion (C), is a measure of the forces that cement particles of soils  Dry sand is cohesion less.  Addition of water in the dry and induces, a little cohesion in it.  Clayey soil has maximum cohesion  The cohesion of soil depends on:  1. Fineness of clay particles  2.Amount of clay  3.Water content of soil
  • 7. Internal Friction(ϕ) Internal friction  The frictional resistance between the individual soil particles at their contact point is known as internal friction. Angle of Internal friction : Ф  It represents the frictional resistance between the soil particles, which is directly proportional to the normal stress
  • 8. Cohesion less soil (Ф- Soil)  These are the soils which do not have cohesion. (C=0)  These soils derive the shear strength from the intergranular friction.  These soils are also called frictional soils.  Examples: Sands and gravels.  Equation for strength is, S= σ . Tan Ф
  • 9. Mohr-Coulomb Failure Criteria  This theory states that a material fails because of a critical combination of normal stress and shear stress, and not from their either maximum normal or shear stress alone.  The relationship between normal stress and shear is given as  s = c¢ +s ¢ tanf ¢  angle of internal friction  c cohesion  s shear strength
  • 10. Shear Strength,S Normal Stress, n =  =  h C  =  Mohr-Coulomb Failure Criterion
  • 11. Mohr-Coulomb Failure Criterion ’f f ’ Shear strength consists of two components: cohesive and frictional.  ' c’ ’f tan ’ c’  f  c''f tan'
  • 12. Mohr-Coulomb Failure Criterion (in terms of total stresses)  f is the maximum shear stress the soil can take without failure, under normal stress of .  c  f  c  tan  f 
  • 13. f is the maximum shear stress the soil can take without failure, under normal effective stress of ’. Mohr-Coulomb Failure Criterion (in terms of effective stresses)  ’ c’  f  c' 'tan' ’ Effective cohesion Effective friction angle f ’  '   u u = pore water pressure
  • 14. 4 MOHR CIRCLE OF STRESS  ’ ' ' ' 1 3 2 m 1 3 2 ' ' ' 3  1 '  PP = Pole w.r.t.plane  ’ ’ ’ ’ '   Major principal stress: σ1 Minor principal stress: σ3 Mean principal stress: σm Maximum shear stress: τmax max ’  2 2       2  2 2  1 3   1 3  Equation of Mohr Circle Compare it’s formulation with equation of circle
  • 15. MOHR CIRCLE AND FAILURE ENVALOPE Failure surface X X Y Y Soil elements at different locations Y ~ stable X ~ failure   ’   ctan f
  • 16. MOHR CIRCLE AND FAILURE ENVALOPE Y h h Mohr circle before external loading v  + Soil element does not fail if the Mohr circleis contained within the envelope GL  v v 
  • 17. MOHR CIRCLE AND FAILURE ENVALOPE Y h GL As loading progresses, Mohr circle becomes larger… .. and finally failure occurs when Mohr circle touches the envelope  v h v
  • 18. MOHR CIRCLE IN TERMS OF TOTAL AND FFECTIVE STRESSES X h’ X u u = + h’ u v v’ h X v v’ h   or ’ If X is on failure Failure envelope in terms of total stresses  c’ c Failure envelope in terms of effective stresses ’ Effective Stresses Total Stresses
  • 19. MOHR-COULOMB FAILURE CRITERION WITH MOHR CIRCLE OF STRESS