Title: Effective Stress
1Effective Stress
2Soil loaded by an applied weight W
Soil loaded by water weighing W
W
W
3Soil loaded by an applied weight W
Soil loaded by water weighing W
W
W
Compression
No deformation
4Definition of Total and Effective Stress
(1)
5Definition of Total and Effective Stress
(1)
Effective vertical stress
(2)
6Definition of Total and Effective Stress
(1)
Effective vertical stress
(2)
7Definition of Total and Effective Stress
(1)
Effective vertical stress
(2)
8Effective Stress
Fig 2 Two Pieces of Rock in Contact
9Effective Stress
Effective Force
(3a)
U uw ( A - Ac )
10Effective Stress
Effective Force
(3a)
U uw ( A - Ac )
Frictional Failure
11Effective Stress
Effective Force
(3a)
U uw ( A - Ac )
Frictional Failure
Failure in terms of stress
(3b)
12Calculation of Effective Stress
Surcharge q
d1
Layer 1
Layer 2
d2
z
Layer 3
d3
Fig 3 Soil Profile
13Calculation of Total Vertical Stress
Elevation
q
Force on base Force on top Weight of soil
d1
d2
z
Plan
A
14Calculation of Total Vertical Stress
Elevation
q
Force on base Force on top Weight of soil
A ?v A q A ?1 d1 A ?2 d2
A ?3 ( z - d1 - d2 )
d1
d2
z
Plan
A
15Calculation of Total Vertical Stress
Elevation
q
Force on base Force on top Weight of soil
A ?v A q A ?1 d1 A ?2 d2
A ?3 ( z - d1 - d2 )
?v q ?1 d1 ?2 d2 ?3 ( z - d1 -
d2 )
d1
d2
z
(4)
Plan
A
16Calculation of pore water pressure
Water table
H
(5)
P
Fig 4 Soil with a static water table
17Calculation of pore water pressure
Water table
H
(5)
P
Fig 4 Soil with a static water table
- The water table is the level of the water
surface in a borehole.
18Calculation of pore water pressure
Water table
H
(5)
P
Fig 4 Soil with a static water table
- The water table is the level of the water
surface in a borehole. - It is the level at which the pore water
pressure uw 0
19Example determining the effective stress
Step 1 Draw ground profile showing soil
stratigraphy and water table
Dry
2 m
3m
Saturated
Fig 5 Soil Stratigraphy
20Example
Step 2 Calculation of relevant bulk unit
weights
Vve Vs 0.7m3
Voids
Vs 1m3
Solid
Distribution by Volume
21Example
Step 2 Calculation of relevant bulk unit
weights
Vve Vs 0.7m3
W 0
Voids
Vs 1m3
Solid
Distribution by weight for the dry soil
Distribution by Volume
22Example
Step 2 Calculation of relevant bulk unit
weights
Vve Vs 0.7m3
W 0
Voids
Vs 1m3
Solid
Distribution by weight for the dry soil
Distribution by Volume
Distribution by weight for the saturated soil
23Example
Step 2 Calculation of relevant bulk unit
weights
Vve Vs 0.7m3
Ww0
Voids
Vs 1m3
Solid
Distribution by weight for the dry soil
Distribution by Volume
Distribution by weight for the saturated soil
?
kN
G
26
46
.
3
s
w
?
kN
m
?
?
?
15
56
.
/
dry
3
m
e
?
1
70
1
.
24Example
Step 2 Calculation of relevant bulk unit
weights
Vve Vs 0.7m3
Ww0
Voids
Vs 1m3
Solid
Distribution by weight for the dry soil
Distribution by Volume
Distribution by weight for the saturated soil
25Example
Step 3 Calculate total stress
2 m
3m
26Example
Step 3 Calculate total stress
2 m
Step 4 Calculate pore water pressure
3m
27Example
Step 3 Calculate total stress
2 m
Step 4 Calculate pore water pressure
3m
Step 5 Calculate effective stress
28Vertical stress and pore pressure variation
0
50
100
150
kPa
0m
2m
4m
Total Stress
(5m)
pore water pressure
6m
Effective stress
Depth
8m
29Stresses acting on a soil element
z
z
y
x
x
Fig 7 Definition of Stress Components
30Principle of Effective Stress
Effective stress relations for general stress
states
(10)
31Example
1 m
Initial GWL
3 m
Lowered GWL
z
Clay
Rock aquifer
32Example
1 m
Initial GWL
3 m
Lowered GWL
z
Clay
Rock aquifer
33Example
- Effective stress increases - soil compresses -
ground surface settles - Effective stress decreases- soil swells - ground
surface heaves. The following problems may then
occur - surface flooding
- flooding of basements built when GWL lowered
- uplift of buildings
- failure of retaining structures
- failures due to reductions in bearing capacity
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