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1
Shallow Foundation
Settlement
2
Total Settlement
Total settlement
scet SSSS ++=
Se = immediate settlement (elastic deformation)
Sc = primary consolidation settlement (due to
dissipation of excess pore water pressure)
Ss = secondary consolidation settlement (due to
adjustment of soil fabric)
3
Immediate Settlement: Occurs immediately after the
construction. This is computed using elasticity theory
(Important for Granular soil)
Primary Consolidation: Due to gradual dissipation of pore
pressure induced by external loading and consequently
expulsion of water from the soil mass, hence volume
change. (Important for Inorganic clays)
Secondary Consolidation: Occurs at constant effective
stress with volume change due to rearrangement of
particles. (Important for Organic soils)
________________________________________________
For any of the above mentioned settlement calculations,
we first need vertical stress increase in soil mass due to
net load applied on the foundation
4
5
6
Elastic Settlement
7
Stress Due to a Concentrated Load
8
Stress due to a Circularly Loaded
Area
9
Distribution of Stress
(from a vertical line load)
10
Stress below a Rectangular Area
11
Stress Influence Chart
12
2:1 method
Approximate methods
13
Approximate methods
14
Types of elastic settlement in foundation
15
16
Elastic settlement Based on the
Theory of Elasticity
17
If the foundation is perfectly flexible then,
the elastic settlement (Se) may be
If = depth factor (Fox, 1948)
α = factor that depends upon the location of foundation where
settlement is being calculated
18
19
20
21
22
F1 and F2 versus H/B ( After Steinbrenner, 1934)
23
If = depth factor (Fox, 1948)
24
α = factor that depends upon the location of
foundation where settlement is being
calculated
α = 4, settlement at the center of foundation
α = 1, settlement at the corner of foundation
25
26
A rigid foundation 1 mX 2m is shown in Fig. Calculate the elastic settlement at the
center of the foundation.
27
(a) Initial condition (b) At the moment of load
Consolidation Process
Valve closed
S=0
∆σ∆σ∆σ∆σ’=0
∆∆∆∆u=0
Valve closed
S=0
∆σ∆σ∆σ∆σ’=0
∆∆∆∆u=P/A
PA
28
Valve opened
Consolidation Process (Continued)
(c) At a time, t
S=δδδδ(t)
∆σ∆σ∆σ∆σ’=kδδδδ(t)
∆∆∆∆u=P/A-kδδδδ(t)
P
δδδδ(t)
Valve opened
S=δδδδp
∆σ∆σ∆σ∆σ’=kδδδδp=P/A
∆∆∆∆u=0
P
δδδδp
(d) At completion of
consolidation
29
Load
Dial gauge
Oedometer
Consolidation Test
30
Consolidation Curve
Time (log scale)
Deformation
Stage I: Initial compression
Stage II: Primary
consolidation
Stage III: Secondary
consolidation
tp
31
Over-Consolidation Ratio
A
Current ground surface
Highest ground surface
in the past
γγγγ z
h
Preconsolidation stress (pressure) - the maximum effective
stress the soil has experienced in the past
pc (or σσσσp’) = γγγγ(h+z)
OCR = pc/σσσσz’
OCR > 1 Overconsolidated soil
OCR = 1 Normally-consolidated soil
OCR < 1 Under-consolidated soil
32
Pressure, p (log scale)
VoidRatio,e
pc
a b
c
d
e
f
g
αααα
αααα
Determination of Preconsolidation
Stress from Lab Results
33
Pressure, p (log scale)
VoidRatio,e
e0
Field consolidation curve
Lab consolidation curve
Remolded specimen
Consolidation curveDisturbance
increases
0.42e0
Effect of Soil Disturbance
34
Pressure, p (log scale)
VoidRatio,e
e0
Virgin consolidation curve
Lab consolidation curve
0.42e0
Cc
pc=σσσσz’
e - logp Curve for Normally
Consolidated Soil
Cc = Compression index
35
Pressure, p (log scale)
VoidRatio,e
e0
Virgin consolidation curve
Lab consolidation curve
0.42e0
Cc
pcσσσσz’
Cr
Lab rebound curve
e - logp Curve for
Overconsolidated Soil
Cr = Recompression index
36
VoidRatio,e
ep
∆∆∆∆e
Time, t (log scale)
t1 t2
Cαααα=∆∆∆∆e/log(t2/t1)
e - logt Curve for
Secondary Consolidation
37
Typical Compression Indices
Cc = 0.1 to 0.8 and Cc = 0.009(LL-10)
Cr = Cc/5 to Cc/10
Cαααα/Cc = 0.01 to 0.07
For soils
38
Stress, σσσσ’ (log scale)
VoidRatio,e
pc = σσσσz’
∆σ∆σ∆σ∆σ
Primary Consolidation Settlement
of Normally Consolidated Soil








σ
σ∆+σ
+
= '
z
'
z
o
c
c log
e
HC
S
1 H = Thickness of soil layer
39
Primary Consolidation Settlement
of Overconsolidated Soil
Stress, σσσσ’ (log scale)
VoidRatio,e
σσσσz’
∆σ∆σ∆σ∆σ pc
σσσσ
Cr
1
Stress, σσσσ’ (log scale)
VoidRatio,e
σσσσz’
∆σ∆σ∆σ∆σ
pc
Cr
1
Cc
1








σ
σ∆+σ
+
= '
z
'
z
o
r
c log
e
HC
S
1 






 σ∆+σ
+
+
+
=
c
'
zc
o
r
c
p
log
e
HC
)OCRlog(
e
HC
S
011
40
Rate of Consolidation
For U<60%
2
v
100
U
4
T 




π
=
( )U10093307811Tv −−= log.. For U>60%
2
dr
v
v
H
tC
T =
Clay
Sand
H
Hdr
41
42
43
Elastic settlement Based on the
Theory of Elasticity
44
Elastic Settlement of Rectangular
footings
45
Elastic Settlement on Saturated
Clay
46
47
Multi-layer systems
48
49
50
Elastic Settlement
51
Elastic Settlement
52
Elastic Settlement
53
Elastic Settlement
54
Elastic Settlement Using the Strain Influence
Factor: [Schmertman Method (1978)]
55
Elastic Settlement Using the Strain Influence
Factor: [Schmertman Method (1978)]
56
Elastic Settlement Using the Strain Influence Factor:
[Schmertman Method (1978)]
57
Elastic Settlement Using the Strain Influence Factor:
[Schmertman Method (1978)]
58
Elastic Settlement Using the Strain Influence Factor:
[Schmertman & Hartman Method (1978)]
59
60
Procedure for Schmertman Method (1978)
61
Procedure for Schmertman Method (1978)
62
Procedure for Schmertman Method (1978)
63
Procedure for Schmertman Method (1978)
64
Notes on Schmertmann Method
65
Notes Cont…
66
Notes Cont…
67
Elastic Settlement Using the Strain Influence
Factor: [Schmertman Method (1978)]
68
69
70
71
72
73
74
75
76
Primary Consolidation
• Expulsion of water from soils accompanied by
increase in effective stress and strength
• Amount can be reasonably estimated based
on lab data, but rate is often poorly estimated
77
Consolidation Settlement
• This method makes use of the results of the conventional
oedometer test where the consolidation parameters of the soil
are measured.
• To compute the stress changes within the soil mass. The
stress changes are computed using a Boussinesqtype
approach assuming elasticity.
• The important parameter for consolidation settlement
calculation is the net effective stress change in the soil.
• Usually the settlements are calculated for the soil divided into
a number of sub-layers and the final total settlement is the
sum of individual sub-layer settlements
78
Consolidation Settlement
79
Consolidation Settlement
80
Consolidation Settlement
81
Consolidation Settlement
82
Consolidation Settlement
83
Consolidation Settlement
84
Consolidation Settlement
85
Average Vertical Stress Increases
Due to a Rectangularly Loaded Area
86
Average Vertical Stress Increases
Due to a Rectangularly Loaded Area
87
Average Vertical Stress Increases
in a given layer
88
Secondary Consolidation
• At the end of primary settlement, settlement
may continue to develop due to the plastic
deformation (creep) of the soil.
• The stage of consolidation is called secondary
consolidation.
89
Secondary Compression Index
90
Field Load Test
• Ultimate load, allowable
load, and settlement can
be determined from a
field load test (ASTM D-
1194-72).
• The test plates are either
square (12”or 18”) or
circular (12” to 30”)
91
Allowable Bearing Capacity for
Sandy Soil based on Settlement
92
Allowable Bearing Capacity for
Sandy Soil based on Settlement
93
Reliability of Settlement
Computations
• The predication is quite satisfactorily in
general.
• The predication is better for inorganic,
insensitive clays than for others.
• The time rate of consolidation settlement
is not well-predicted.
94
95
Average Vertical Stress Increases
Due to a Rectangularly Loaded Area
96
Average Vertical Stress Increases
Due to a Rectangularly Loaded Area
97
Average Vertical Stress Increases
in a given layer

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