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Chapter3

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Compaction
In construction of high way embankments, earth dams and
many other engineering structures, loose soils must be
compacted to improve their strength by increasing their unit
weight.
Compaction – Densification of soil by removing air voids
using mechanic equipment. (for unsaturated soil)
The degree of compaction is measured in terms of its dry
unit weight.
Consolidation is another kind of densification with fluid
flow away. Consolidation is primarily for clayey soils.
Objectives for Compaction
Increasing the bearing capacity of foundations.
Decreasing the undesirable settlement of structures.
Control undesirable volume changes.
Reduction in hydraulic conductivity.
Increasing the stability of slopes.
Effect of Water on Compaction
Water acts as a softening agent
on the soil particles. The soil
particles move into a densely
packed position
Water takes up the spaces that
would have been occupied by
the solid particles.
Same compactive
effort
Optimum
Moisture
Content
Standard Proctor Compaction Test
The standard was originally developed to simulate field
compaction in the lab
Purpose: Find the optimum moisture content at which
the maximum dry unit weight is attained.
Compaction curve
Compaction curve plotted gd vs w.
The peak of the curve is the
maximum compaction at optimum
moisture content.
Zero-air-void Unit Weight
At certain water content, what is
the unit weight to let no air in the
voids
Effect of Compaction Energy
As the compaction effort
increases,
The maximum dry unit weight of
compaction increases
The optimum moisture content
decreases
Effect of soil type
Fine grained soil needs more water to reach optimum; and coarse
grained soil needs less water to reach optimum.
Modified Proctor
Compaction Test
The modified proctor
compaction test was developed
to simulate larger compaction
effort for more serious loads
and bigger equipment.
Mold
Test
Rammer
No. of
layers
Energy of
Blows
compaction (kNper layer
m/m3)
Capacity
(cm3)
Diameter
(mm)
Height
(mm)
Mass
(kg)
Drop
(mm)
Standard
Proctor
943.3
101.6
116.43
2.5
304.8
3
25
591.3
Modified
Proctor
943.3
101.6
116.43
4.54
457
5
25
2696
Empirical Relationship wopt vs PL
Gurtug and Sridharan (2004) proposed correlations for optimum
moisture content, wopt, and maximum dry unit weight, gdmax,
with the plastic limit, PL, of cohesive soils.
wopt(%) = [1.95-0.38(log CE)](PL)
gdmax(kN/m3) = 22.68e0.0183wopt(%)
where CE = compaction energy (kN-m/m3)
For modified Proctor test, CE = 2700 kN-m/m3
wopt(%) ≈ 0.65(PL)
gdmax(kN/m3) ≈ 22.68e0.012(PL)
Relative density
Relative density is commonly used to indicate the in situ
denseness or looseness of granular soil.
where Dr = relative density, usually given as a percentage
e = in situ void ratio of the soil
emax = void ratio of the soil in the loosest state
emin = void ratio of the soil in the densest state
Relative density (%)
Description of soil deposit
0 – 15
Very loose
15 – 50
Loose
50 – 70
Medium
70 – 85
Dense
85 – 100
Very dense
Engineering Classification of Soil
Objective
Classifying soils into groups with similar behaviour, in terms of
simple indices, can provide geotechnical engineers a general
guidance about engineering properties of the soils through the
accumulated experience.
Communicate
between engineers
Simple indices
GSD, LL, PI
Classification
system
Use the
accumulated
experience
Estimate
engineering
properties
Achieve
engineering
purposes
Classification Systems
Two commonly used systems for soil engineers based on
particle distribution and Atterberg limits:
• American Association of State Highway and Transportation
Official (AASHTO) System
• Unified Soil Classification System (USCS)
(preferred by geotechnical engineers)
U.S. Standard Sieve Sizes
Soil particles
Fine grained soil
Gravel, Sand, Silt, Clay
Coarse grained soil
No.10
No.40
Sieve no.
Opening (mm)
4
4.75
10
2.00
20
0.850
40
0.425
60
0.250
100
0.150
200
0.075
No.200
(mm)
No.4 No.10
No.40
No.200
Atterberg Limits
Atterberg limits are the limits of water content used to
define soil behaviour.
Increasing moisture content
V
ol
u
m
e,
V
Solid
Semisolid
Plastic
Liquid
S = 100%
Plasticity Index
PI = LL-PL
SL
Shrinkage Limit
PL
Plastic Limit
LL
Liquid Limit
Moisture
content, w %
AASHTO Classification System
This system was developed in 1929 as the Public Road
Administration classification system. Afterwards, there are
several revisions. The present version is primarily based on
the version in 1945.
1. Grain size
No.10
No.40
No.200
(mm)
If boulders are encountered, they are excluded from the portion of the soil sample
from which classification is made. However, the percentage of such material is
recorded.
2. Plasticity
The term silty is applied when the fine fractions of the soil have a plasticity index
of 10 or less. The term clayey is applied when the fine fractions have a plasticity
index of 11 or more.
Classification for Granular Materials
(Proceeding from left to right against the columns)
By process of elimination, the first group from the left into
which the test data fit is the correct classification.
Classification for Silt-clay Materials
(Proceeding from left to right against the columns)
By process of elimination, the first group from the left into
which the test data fit is the correct classification.
Range of LL and PI for soils in groups A-2, A-4, A-5, A-6 and A-7
1.
2.
3.
4.
Group Index, GI
The first term is determined by the LL
GI = (F200-35)[0.2+0.005(LL-40)]
+0.01(F200-15)(PI-10)
The second term is determined by the PI
For Group A-2-6 and A-2-7
GI = 0.01(F200-15)(PI-10)
where F200 = percentage passing
through the No. 200 sieve
If equation gives a negative value then GI = 0
The calculated GI is rounded off to the nearest whole number
There is no upper limit for GI
The GI of soils belong to groups A-1-a, A-1-b, A-2-4, A-2-5, and
A-3 is always 0.
The quality of performance of a soil as a subgrade
material is inversely proportional to the GI
Summary AASHTO
●
●
●
8 major groups: A-1 – A-7 (with several subgroups) and
organic soils A-8
The required tests are sieve analysis and Atterberg limits.
The group index, an empirical formula, is used to further
evaluate soils within a group (subgroups).
A-1 – A-3
Granular Materials
≤ 35% pass No. 200 sieve
Using LL and PI separates silty
materials from clayey materials
(only for A2 group)
A-4 – A-7
Silt-clay Materials
> 35% pass No. 200 sieve
Using LL and PI separates silty
materials from clayey materials
●
The original purpose of this classification system is used for
Example 3.1 Passing No. 10 sieve =100%
LL = 30, PI =10
No. 40 sieve = 80%
No. 200 sieve = 58%
A-4 – A-7
GI = (F200-35)[0.2+0.005(LL-40)]+0.01(F200-15)(PI-10)
= (58-35)[0.2+0.005(30-40)]+0.01(58-15)(10-10)
= 3.45 ≈ 3
A-4(3)
Example 3.2
Passing No. 200 sieve = 95%
LL = 60, PI =40
A-4 – A-7
GI = (F200-35)[0.2+0.005(LL-40)]+0.01(F200-15)(PI-10)
40 > 60-30
= (95-35)[0.2+0.005(60-40)]+0.01(95-15)(40-10)
= 42
A-7-6(42)
Unified Soil Classification System
This system was first developed by Casagrande in 1942 for
use in the airfield construction work during World War II.
In cooperation with the U.S. Bureau of Reclamation, this
system was revised in 1952. At present, it is used widely by
engineers.
Grain size
(mm)
No.4 No.10
No.40
No.200
Two broad categories
1. Coarse-grained soils that are gravelly and sandy in nature with less
than 50% passing through the No. 200 sieve.
2. Fine-grained soils are with 50% or more passing through the No. 200
sieve.
Table 3.2
Group Symbol
Soil symbols:
● G : Gravel
● S : Sand
● M : Silt
● C : Clay
● O : Organic
● Pt : Peat
Plasticity symbols:
● H : High plasticity (LL ≥ 50)
● L : Low plasticity (LL < 50)
Gradation symbols:
● W : Well graded
● P : Poor graded
1 < Cc < 3 and Cu ≥ 4
(for gravels)
1 < Cc < 3 and Cu ≥ 6
(for sands)
Prefix
Examples:
● SW : Well-graded sand
● SC : Clayey sand
● SM : Silty sand
● MH : Elastic silt
Typical USCS:
SM – Silty sand with gravel
Group symbol
Group name
Classification
The coarse-grained soils are designated by group symbols such as
GW, GP, GM, GC, SW, SP, SM and SC. For proper classification, the
following factors are to be considered:
1. Percent passing through the No. 200 sieve
2. Percent of coarse fraction passing through the No. 4 sieve
3. Cu and Cc (for soils with 0-5% passing through the No. 200
sieve)
4. LL and PI of that portion of soil passing through the No. 40 sieve
(for soils with 5% or more passing through the No. 200 sieve)
When the percent passing through the No. 200 sieve is between 5 and
12% dual symbols, such as GW-GM, GP-GM, GW-GC, GP-GC, SWSM, SW-SC, SP-SM and SP-SC are needed.
Fine-grained soil classifications with symbols ML, CL, OL,
MH, CH, and OH are obtained by plotting the LL and PI of
soil on the plasticity chart.
The A-line generally separates
the more claylike soils from silty
soils, and the organics from the
inorganics.
The U-line indicates the upper
bound for general soils
7
4
Dual Symbols
For the following three conditions, a dual symbol should be used.
1. Coarse-grained soils with 5-12% passing through the No. 200
sieve. The first symbol indicates whether the coarse fraction is
well or poorly graded. The second symbol describes the
contained fine fraction. For example, SP-SM, poorly graded
sand with silt.
2. Soils with limits within the shaded area of the plasticity chart.
(PI between 4 and 7, and LL between about 12 and 25). It is
hard to distinguish between the silty and clayey soil. CL-ML:
Silty clay, SC-CM: Silty, clayey sand.
3. Soil contain similar fine and coarse-grained fractions. For
example, GM-ML.
Organic Soils
Highly organic soils – Peat (Group symbol, Pt)
A sample composed primarily of vegetable tissue in various
stages of decomposition and has a fibrous to amorphous
texture, a dark-brown to black colour, and an organic odor
should be designated as a highly organic soil and shall be
classified as peat, Pt.
Organic clay or silt (Group symbol, OL or OH)
“The soil’s liquid limit (LL) after oven drying is less than
75% of its liquid limit before oven drying.” If the above
statement is true, then the first symbol is O.
The second symbol is obtained by locating the values of PI
and LL (not oven dried) in the plasticity chart.
Coarse-grained
A
Soils
Group symbol
Group name
Group
symbol
Fine-grained
Soils
Group name
Summary USCS
Example 3.3
Passing No. 10 sieve =100%
No. 40 sieve = 80%
No. 200 sieve = 58%
LL = 30, PI =10
A fine-grained soil
CL
7
4
Example 3.4
Soil A LL = 30, PL = 22
1. About 8% of the soil pass through
No. 200 sieve. Hence this is a
coarse-grained soil and, since this
is within 5 to 12%, dual symbols
needed to be used.
2. 100% of the soil pass through No.
4. Hence this is a sandy soil.
3. Cu = 1.59 < 6, Cc = 1.25 > 1 poorly
graded
4. LL = 30, PI = 30-22 = 8, it plots
above the A-line. Hence this is a
clayey soil.
SP-SC – Poorly-graded sand with clay (or silty clay)
Example 3.4 (cont.)
Soil B
LL = 26, PL = 20
1. About 61% of the soil pass through
No. 200 sieve. Hence this is a finegrained soil.
2. LL = 26, PI = 26-20 = 6, it falls
inside the shaded area of the
plasticity chart .
CL-ML – Sandy silty clay
Homeworks
3.1) The sieve analysis of ten soils and the liquid and plastic limits of the fraction
passing through the No. 40 sieve are given below. Classify the soils by the AASHTO
classification system and give the group indexes.
Soil no.
1
2
3
4
5
6
7
8
9
10
Sieve Analysis % Finer
No. 10
No. 40
No. 200
Liquid
limit
98
100
100
85
92
97
100
94
83
100
80
92
88
55
75
60
55
80
48
92
50
80
65
45
62
30
8
63
20
86
38
56
37
28
43
25
40
20
70
Plastic
limit
29
23
22
20
28
16
NP
21
15
38
3.2) Classify soils 1 through 6 given in Problem 3.1 by the Unified classification
system.
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