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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
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
’
ctan
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