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 Page 1


 
 
1 
 
Short Notes for Soil Mechanics & Foundation Engineering 
Properties of Soils 
Water content 
• 100
W
S
W
w
W
=? 
 W W = Weight of power 
  W S = Weight of solids 
 
Void ratio 
• 
v
s
V
e
V
= 
            V v = Volume of voids 
            V =  Total volume of soil 
 
Degree of Saturation 
• 100
w
v
V
S
V
=? 
V w = Volume of water 
 V v = Volume of voids 
0 = S= 100 
for perfectly dry soil : S = O 
for Fully saturated soil : S = 100% 
 
 
Air Content 
• 1
a
c
v
V
as
V
= = -    V a = Volume of air 
S r + a c = 1 
% Air Void 
• 
Volume of air
% 100 100
Total volume
a
a
V
n
V
= ? = ?
 
 
Unit Weight 
• Bulk unit weight 
sw
s w a
WW W
V V V V
?
+
==
++
 
 
• Dry Unit Weight 
s
d
W
V
? =
 
o Dry unit weight is used as a measure of denseness of soil 
• Saturated unit weight: It is the ratio of total weight of fully saturated soil sample to its total 
volume. 
sat
sat
W
V
? = 
• Submerged unit weight or Buoyant unit weight 
Page 2


 
 
1 
 
Short Notes for Soil Mechanics & Foundation Engineering 
Properties of Soils 
Water content 
• 100
W
S
W
w
W
=? 
 W W = Weight of power 
  W S = Weight of solids 
 
Void ratio 
• 
v
s
V
e
V
= 
            V v = Volume of voids 
            V =  Total volume of soil 
 
Degree of Saturation 
• 100
w
v
V
S
V
=? 
V w = Volume of water 
 V v = Volume of voids 
0 = S= 100 
for perfectly dry soil : S = O 
for Fully saturated soil : S = 100% 
 
 
Air Content 
• 1
a
c
v
V
as
V
= = -    V a = Volume of air 
S r + a c = 1 
% Air Void 
• 
Volume of air
% 100 100
Total volume
a
a
V
n
V
= ? = ?
 
 
Unit Weight 
• Bulk unit weight 
sw
s w a
WW W
V V V V
?
+
==
++
 
 
• Dry Unit Weight 
s
d
W
V
? =
 
o Dry unit weight is used as a measure of denseness of soil 
• Saturated unit weight: It is the ratio of total weight of fully saturated soil sample to its total 
volume. 
sat
sat
W
V
? = 
• Submerged unit weight or Buoyant unit weight 
 
 
2 
 
'
sat w
? ? ? =-
 
sat
? = unit wt. of saturated soil 
? = unit wt. of water 
• Unit wt. of solids:  
s
s
s
W
V
? = 
Specific Gravity 
True/Absolute Special Gravity, G 
• Specific gravity of soil solids (G) is the ratio of the weight of a given volume of solids to the 
weight of an equivalent volume of water at 4 ?. 
.
ss
s w w
W
G
V
?
??
== 
 
• Apparent or mass specific gravity (G m):  
 or  or 
.
d sat
m
ww
W
G
V
? ? ?
??
==
 
where, ? is bulk unit wt. of soil 
? = ? sat for saturated soil mass 
? = ? d for dry soil mass 
G m < G 
 
Relative density (I D) 
• To compare degree of denseness of two soils. 
1
 
D
Shear strength
Compressi t
I
bili y
? ? 
max
max min
% 100
D
ee
I
ee
-
=?
-
 
min
min max
11
    -    
% 100
11
    -    
dd
D
dd
I
??
??
=? 
 
Relative Compaction 
• Indicate: Degree of denseness of cohesive + cohesionless soil 
 
max
D
c
D
R
?
?
=  
Relative Density 
• Indicate: Degree of denseness of natural cohesionless soil 
Some Important Relationships 
• Relation between ,
d
??  
1
d
w
?
? =
+
 
(ii) 
1
s
V
V
e
=
+
   (iii) 
1
s
W
W
w
=
+
 
Page 3


 
 
1 
 
Short Notes for Soil Mechanics & Foundation Engineering 
Properties of Soils 
Water content 
• 100
W
S
W
w
W
=? 
 W W = Weight of power 
  W S = Weight of solids 
 
Void ratio 
• 
v
s
V
e
V
= 
            V v = Volume of voids 
            V =  Total volume of soil 
 
Degree of Saturation 
• 100
w
v
V
S
V
=? 
V w = Volume of water 
 V v = Volume of voids 
0 = S= 100 
for perfectly dry soil : S = O 
for Fully saturated soil : S = 100% 
 
 
Air Content 
• 1
a
c
v
V
as
V
= = -    V a = Volume of air 
S r + a c = 1 
% Air Void 
• 
Volume of air
% 100 100
Total volume
a
a
V
n
V
= ? = ?
 
 
Unit Weight 
• Bulk unit weight 
sw
s w a
WW W
V V V V
?
+
==
++
 
 
• Dry Unit Weight 
s
d
W
V
? =
 
o Dry unit weight is used as a measure of denseness of soil 
• Saturated unit weight: It is the ratio of total weight of fully saturated soil sample to its total 
volume. 
sat
sat
W
V
? = 
• Submerged unit weight or Buoyant unit weight 
 
 
2 
 
'
sat w
? ? ? =-
 
sat
? = unit wt. of saturated soil 
? = unit wt. of water 
• Unit wt. of solids:  
s
s
s
W
V
? = 
Specific Gravity 
True/Absolute Special Gravity, G 
• Specific gravity of soil solids (G) is the ratio of the weight of a given volume of solids to the 
weight of an equivalent volume of water at 4 ?. 
.
ss
s w w
W
G
V
?
??
== 
 
• Apparent or mass specific gravity (G m):  
 or  or 
.
d sat
m
ww
W
G
V
? ? ?
??
==
 
where, ? is bulk unit wt. of soil 
? = ? sat for saturated soil mass 
? = ? d for dry soil mass 
G m < G 
 
Relative density (I D) 
• To compare degree of denseness of two soils. 
1
 
D
Shear strength
Compressi t
I
bili y
? ? 
max
max min
% 100
D
ee
I
ee
-
=?
-
 
min
min max
11
    -    
% 100
11
    -    
dd
D
dd
I
??
??
=? 
 
Relative Compaction 
• Indicate: Degree of denseness of cohesive + cohesionless soil 
 
max
D
c
D
R
?
?
=  
Relative Density 
• Indicate: Degree of denseness of natural cohesionless soil 
Some Important Relationships 
• Relation between ,
d
??  
1
d
w
?
? =
+
 
(ii) 
1
s
V
V
e
=
+
   (iii) 
1
s
W
W
w
=
+
 
 
 
3 
 
• Relation between e and n 
1
e
n
e
=
+
    or    
1
n
e
n
=
-
 
• Relation between e, w, G and S: 
Se = w. G 
• Bulk unit weight () ? in terms of G, e, w and 
w
? ? , G, e, S r, 
w
? 
()
1
rw
G eS
e
?
?
+
=
+
 
(1 )
(1 )
w
Gw
e
?
?
+
=
+
    {Srxe = wG} 
• Saturated unit weight ( .) sat ? in terms of G, e & 
w
?  
S r = 1 .
1
sat w
Ge
e
??
+ ??
=
??
+
??
 
• Dry unit weight ()
d
? in terms of G, e and 
w
? 
S r = 0 
(1 )
11
1
w w a w
d
G G G
wG
e wG
S
? ? ? ?
?
-
= = =
++
+
 
• Submerged unit weight ( ') ? in terms of G, e and 
w
? 
sat w
? ? ? = - = 
1
'.
1
w
G
e
??
- ??
=
??
+
??
 
• Relation between degree of saturation (s) w and G 
1
(1 )
w
W
S
W
G
?
?
=
+-
 
 
 
• Calibration of Hydrometer 
 
 
• Effective depth is calculated as 
1
1
2
H
e
j
V
H H h
A
??
= + -
??
??
??
 
where, H 1 = distance (cm) between any hydrometer reading and neck. 
h = length of hydrometer bulb 
V H = volume of hydrometer bulb 
Page 4


 
 
1 
 
Short Notes for Soil Mechanics & Foundation Engineering 
Properties of Soils 
Water content 
• 100
W
S
W
w
W
=? 
 W W = Weight of power 
  W S = Weight of solids 
 
Void ratio 
• 
v
s
V
e
V
= 
            V v = Volume of voids 
            V =  Total volume of soil 
 
Degree of Saturation 
• 100
w
v
V
S
V
=? 
V w = Volume of water 
 V v = Volume of voids 
0 = S= 100 
for perfectly dry soil : S = O 
for Fully saturated soil : S = 100% 
 
 
Air Content 
• 1
a
c
v
V
as
V
= = -    V a = Volume of air 
S r + a c = 1 
% Air Void 
• 
Volume of air
% 100 100
Total volume
a
a
V
n
V
= ? = ?
 
 
Unit Weight 
• Bulk unit weight 
sw
s w a
WW W
V V V V
?
+
==
++
 
 
• Dry Unit Weight 
s
d
W
V
? =
 
o Dry unit weight is used as a measure of denseness of soil 
• Saturated unit weight: It is the ratio of total weight of fully saturated soil sample to its total 
volume. 
sat
sat
W
V
? = 
• Submerged unit weight or Buoyant unit weight 
 
 
2 
 
'
sat w
? ? ? =-
 
sat
? = unit wt. of saturated soil 
? = unit wt. of water 
• Unit wt. of solids:  
s
s
s
W
V
? = 
Specific Gravity 
True/Absolute Special Gravity, G 
• Specific gravity of soil solids (G) is the ratio of the weight of a given volume of solids to the 
weight of an equivalent volume of water at 4 ?. 
.
ss
s w w
W
G
V
?
??
== 
 
• Apparent or mass specific gravity (G m):  
 or  or 
.
d sat
m
ww
W
G
V
? ? ?
??
==
 
where, ? is bulk unit wt. of soil 
? = ? sat for saturated soil mass 
? = ? d for dry soil mass 
G m < G 
 
Relative density (I D) 
• To compare degree of denseness of two soils. 
1
 
D
Shear strength
Compressi t
I
bili y
? ? 
max
max min
% 100
D
ee
I
ee
-
=?
-
 
min
min max
11
    -    
% 100
11
    -    
dd
D
dd
I
??
??
=? 
 
Relative Compaction 
• Indicate: Degree of denseness of cohesive + cohesionless soil 
 
max
D
c
D
R
?
?
=  
Relative Density 
• Indicate: Degree of denseness of natural cohesionless soil 
Some Important Relationships 
• Relation between ,
d
??  
1
d
w
?
? =
+
 
(ii) 
1
s
V
V
e
=
+
   (iii) 
1
s
W
W
w
=
+
 
 
 
3 
 
• Relation between e and n 
1
e
n
e
=
+
    or    
1
n
e
n
=
-
 
• Relation between e, w, G and S: 
Se = w. G 
• Bulk unit weight () ? in terms of G, e, w and 
w
? ? , G, e, S r, 
w
? 
()
1
rw
G eS
e
?
?
+
=
+
 
(1 )
(1 )
w
Gw
e
?
?
+
=
+
    {Srxe = wG} 
• Saturated unit weight ( .) sat ? in terms of G, e & 
w
?  
S r = 1 .
1
sat w
Ge
e
??
+ ??
=
??
+
??
 
• Dry unit weight ()
d
? in terms of G, e and 
w
? 
S r = 0 
(1 )
11
1
w w a w
d
G G G
wG
e wG
S
? ? ? ?
?
-
= = =
++
+
 
• Submerged unit weight ( ') ? in terms of G, e and 
w
? 
sat w
? ? ? = - = 
1
'.
1
w
G
e
??
- ??
=
??
+
??
 
• Relation between degree of saturation (s) w and G 
1
(1 )
w
W
S
W
G
?
?
=
+-
 
 
 
• Calibration of Hydrometer 
 
 
• Effective depth is calculated as 
1
1
2
H
e
j
V
H H h
A
??
= + -
??
??
??
 
where, H 1 = distance (cm) between any hydrometer reading and neck. 
h = length of hydrometer bulb 
V H = volume of hydrometer bulb 
 
 
4 
 
 
Plasticity Index (I p):  
• It is the range of moisture content over which a soil exhibits plasticity. 
I p = W L - W p 
W L = water content at LL 
W p = water content at PL 
 
I p (%) Soil Description 
0 
1 to 5 
5 to 10 
10 to 20 
20 to 40 
> 40 
Non plastic 
Slight plastic 
Low plastic 
Medium plastic 
Highly plastic 
Very highly plastic 
 
Relative Consistency or Consistency – index (I c):  
LN
C
p
WW
I
I
-
= 
 
 
   0 
     
 1
C
N L C
NP
For W W I
For W I W
=
=
? ? = ?
?
?=
?
 
 
Liquidity Index (I L) 
NP
L
P
WW
I
I
-
= 
For a soil in plastic state I L varies from 0 to 1. 
 
Consist. Description I C I L 
Liquid 
Plastic 
 
 
 
 
Semi-
solid 
 
Solid 
Liquid 
Very soft  
soft 
medium 
stiff  
stiff 
Very stiff 
OR Hard 
 
Hard OR 
very hard 
<0 
0-0.25 
0.25-0.5 
0.50-0.75 
0.75-1.00 
 
 
>1 
 
 
>1 
>1 
0.75-1.00 
0.50-0.75 
0.25-0.50 
0.0-0.25 
 
 
< 0 
 
 
< 0 
 
Flow Index (I f) 
12
21
log10( / )
f
WW
I
NN
-
= 
 
 
Toughness Index (I t) 
P
T
F
I
I
I
= 
• For most of the soils:  0 < I T < 3 
Page 5


 
 
1 
 
Short Notes for Soil Mechanics & Foundation Engineering 
Properties of Soils 
Water content 
• 100
W
S
W
w
W
=? 
 W W = Weight of power 
  W S = Weight of solids 
 
Void ratio 
• 
v
s
V
e
V
= 
            V v = Volume of voids 
            V =  Total volume of soil 
 
Degree of Saturation 
• 100
w
v
V
S
V
=? 
V w = Volume of water 
 V v = Volume of voids 
0 = S= 100 
for perfectly dry soil : S = O 
for Fully saturated soil : S = 100% 
 
 
Air Content 
• 1
a
c
v
V
as
V
= = -    V a = Volume of air 
S r + a c = 1 
% Air Void 
• 
Volume of air
% 100 100
Total volume
a
a
V
n
V
= ? = ?
 
 
Unit Weight 
• Bulk unit weight 
sw
s w a
WW W
V V V V
?
+
==
++
 
 
• Dry Unit Weight 
s
d
W
V
? =
 
o Dry unit weight is used as a measure of denseness of soil 
• Saturated unit weight: It is the ratio of total weight of fully saturated soil sample to its total 
volume. 
sat
sat
W
V
? = 
• Submerged unit weight or Buoyant unit weight 
 
 
2 
 
'
sat w
? ? ? =-
 
sat
? = unit wt. of saturated soil 
? = unit wt. of water 
• Unit wt. of solids:  
s
s
s
W
V
? = 
Specific Gravity 
True/Absolute Special Gravity, G 
• Specific gravity of soil solids (G) is the ratio of the weight of a given volume of solids to the 
weight of an equivalent volume of water at 4 ?. 
.
ss
s w w
W
G
V
?
??
== 
 
• Apparent or mass specific gravity (G m):  
 or  or 
.
d sat
m
ww
W
G
V
? ? ?
??
==
 
where, ? is bulk unit wt. of soil 
? = ? sat for saturated soil mass 
? = ? d for dry soil mass 
G m < G 
 
Relative density (I D) 
• To compare degree of denseness of two soils. 
1
 
D
Shear strength
Compressi t
I
bili y
? ? 
max
max min
% 100
D
ee
I
ee
-
=?
-
 
min
min max
11
    -    
% 100
11
    -    
dd
D
dd
I
??
??
=? 
 
Relative Compaction 
• Indicate: Degree of denseness of cohesive + cohesionless soil 
 
max
D
c
D
R
?
?
=  
Relative Density 
• Indicate: Degree of denseness of natural cohesionless soil 
Some Important Relationships 
• Relation between ,
d
??  
1
d
w
?
? =
+
 
(ii) 
1
s
V
V
e
=
+
   (iii) 
1
s
W
W
w
=
+
 
 
 
3 
 
• Relation between e and n 
1
e
n
e
=
+
    or    
1
n
e
n
=
-
 
• Relation between e, w, G and S: 
Se = w. G 
• Bulk unit weight () ? in terms of G, e, w and 
w
? ? , G, e, S r, 
w
? 
()
1
rw
G eS
e
?
?
+
=
+
 
(1 )
(1 )
w
Gw
e
?
?
+
=
+
    {Srxe = wG} 
• Saturated unit weight ( .) sat ? in terms of G, e & 
w
?  
S r = 1 .
1
sat w
Ge
e
??
+ ??
=
??
+
??
 
• Dry unit weight ()
d
? in terms of G, e and 
w
? 
S r = 0 
(1 )
11
1
w w a w
d
G G G
wG
e wG
S
? ? ? ?
?
-
= = =
++
+
 
• Submerged unit weight ( ') ? in terms of G, e and 
w
? 
sat w
? ? ? = - = 
1
'.
1
w
G
e
??
- ??
=
??
+
??
 
• Relation between degree of saturation (s) w and G 
1
(1 )
w
W
S
W
G
?
?
=
+-
 
 
 
• Calibration of Hydrometer 
 
 
• Effective depth is calculated as 
1
1
2
H
e
j
V
H H h
A
??
= + -
??
??
??
 
where, H 1 = distance (cm) between any hydrometer reading and neck. 
h = length of hydrometer bulb 
V H = volume of hydrometer bulb 
 
 
4 
 
 
Plasticity Index (I p):  
• It is the range of moisture content over which a soil exhibits plasticity. 
I p = W L - W p 
W L = water content at LL 
W p = water content at PL 
 
I p (%) Soil Description 
0 
1 to 5 
5 to 10 
10 to 20 
20 to 40 
> 40 
Non plastic 
Slight plastic 
Low plastic 
Medium plastic 
Highly plastic 
Very highly plastic 
 
Relative Consistency or Consistency – index (I c):  
LN
C
p
WW
I
I
-
= 
 
 
   0 
     
 1
C
N L C
NP
For W W I
For W I W
=
=
? ? = ?
?
?=
?
 
 
Liquidity Index (I L) 
NP
L
P
WW
I
I
-
= 
For a soil in plastic state I L varies from 0 to 1. 
 
Consist. Description I C I L 
Liquid 
Plastic 
 
 
 
 
Semi-
solid 
 
Solid 
Liquid 
Very soft  
soft 
medium 
stiff  
stiff 
Very stiff 
OR Hard 
 
Hard OR 
very hard 
<0 
0-0.25 
0.25-0.5 
0.50-0.75 
0.75-1.00 
 
 
>1 
 
 
>1 
>1 
0.75-1.00 
0.50-0.75 
0.25-0.50 
0.0-0.25 
 
 
< 0 
 
 
< 0 
 
Flow Index (I f) 
12
21
log10( / )
f
WW
I
NN
-
= 
 
 
Toughness Index (I t) 
P
T
F
I
I
I
= 
• For most of the soils:  0 < I T < 3 
 
 
5 
 
• When I T < 1, the soil is friable (easily crushed) at the plastic limit. 
 
 
 
• Shrinkage Ratio (SR) 
12
12
100
d
VV
V
SR
ww
-
?
=
-
 
V 1 = Volume of soil mass at water content w 1%. 
V 2 = volume of soil mass at water content w 2%.  
V d = volume of dry soil mass 
? 
1
1
100
()
d
d
s
VV
V
SR
WW
?? -
?
??
??
=
-
 
If w 1 & w 2 are expressed as ratio, 
1 2 1 2
12
12
( ) / ( ) /
,
dw
s
V V V V V
SR But w w
W W W
? --
= - =
-
 
?
1
 .
sd
d w w
W
SR
V
?
??
== 
 
Properties Relations
hip 
Governing 
Parameters 
Plasticity      ? Plasticity Index 
Better 
Foundation 
Material upon 
Remoulding 
     ?  Consistency 
Index 
Compressibility      ? Liquid Limit 
Rate of loss in 
shear strength 
with increase in 
water content 
     ? Flow Index 
Strength of 
Plastic Limit 
     ? Toughness 
Index 
 
 
Compaction of Soil 
 
 
Optimum moisture content 
max
()
1
d imum
optimum
w
?
? =
+
 
max
()
d imum
? = Maximum dry density 
 ? = Density of soil 
optimum
w = Optimum moisture content 
 
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FAQs on Earth Pressure Theories - Foundation Engineering - Civil Engineering (CE)

1. What is earth pressure in civil engineering?
Ans. Earth pressure in civil engineering refers to the force exerted by soil or other materials against a retaining structure, such as a wall or foundation. It is important to understand earth pressure in order to design safe and stable structures.
2. What are the different theories used to calculate earth pressure?
Ans. There are several theories used in civil engineering to calculate earth pressure, including: - Coulomb's Theory: This theory assumes that the soil behaves as a frictional material and the earth pressure depends on the angle of internal friction. - Rankine's Theory: Rankine's theory assumes that the soil is cohesionless and the earth pressure depends on the angle of friction and the angle of repose of the soil. - Terzaghi's Theory: Terzaghi's theory takes into account both the soil cohesion and the angle of internal friction, providing a more accurate calculation of earth pressure. - Brinch Hansen's Theory: Brinch Hansen's theory considers the soil as an elastic-plastic material and incorporates the effects of soil deformation in the calculation of earth pressure. - Coulomb-Mohr Theory: This theory combines Coulomb's theory of soil friction with Mohr's theory of stress to calculate earth pressure, taking into account both the shear strength and normal stress on the soil.
3. How is earth pressure determined during the design of retaining walls?
Ans. During the design of retaining walls, earth pressure is determined by considering factors such as the type of soil, the wall geometry, and the loads acting on the wall. Various methods, such as graphical methods, limit equilibrium methods, and numerical methods, can be used to calculate the earth pressure. The choice of method depends on the complexity of the problem and the desired level of accuracy.
4. What are the factors that influence earth pressure?
Ans. Several factors influence earth pressure, including: - Soil properties: The cohesion and angle of internal friction of the soil play a significant role in determining the earth pressure. - Wall geometry: The shape, height, and inclination of the retaining wall affect the distribution of earth pressure. - Wall stiffness: The stiffness of the wall influences the magnitude and distribution of earth pressure. - Surcharge loads: Additional loads on the soil, such as buildings or vehicles, can increase the earth pressure on the retaining wall. - Groundwater conditions: The presence of groundwater can affect the soil properties and increase the earth pressure.
5. What are the practical applications of understanding earth pressure in civil engineering?
Ans. Understanding earth pressure is crucial in several civil engineering applications, including: - Design of retaining walls: Proper estimation of earth pressure ensures the stability and safety of retaining walls. - Design of basement walls: Knowledge of earth pressure helps in designing basement walls to withstand the lateral forces exerted by the surrounding soil. - Slope stability analysis: Earth pressure calculations are essential in analyzing the stability of slopes and designing appropriate measures to prevent landslides. - Design of deep excavations: Understanding earth pressure is vital for designing deep excavations to prevent soil collapse and ensure the safety of workers. - Design of underground structures: Earth pressure considerations are crucial in designing underground structures such as tunnels, underground parking lots, and underground storage facilities to withstand the lateral forces exerted by the surrounding soil.
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