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 Page 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


 
 
 
 
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 
 
 
 
 
'
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


 
 
 
 
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 
 
 
 
 
'
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
=
+
 
 
 
 
 
• 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


 
 
 
 
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 
 
 
 
 
'
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
=
+
 
 
 
 
 
• 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 
 
 
 
 
 
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


 
 
 
 
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 
 
 
 
 
'
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
=
+
 
 
 
 
 
• 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 
 
 
 
 
 
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 
 
 
 
 
• 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 Geotechnical Engineering Formulas for Civil Engineering Exam - Foundation Engineering - Civil Engineering (CE)

1. What are some important geotechnical engineering formulas that are commonly asked in civil engineering exams?
Ans. Some important geotechnical engineering formulas that are commonly asked in civil engineering exams include: - Bearing Capacity Formula: This formula is used to calculate the maximum load that can be supported by a foundation soil without causing any failure or excessive settlement. - Consolidation Settlement Formula: This formula is used to estimate the settlement of saturated cohesive soils due to the expulsion of water from the soil pores under load. - Shear Strength Formula: This formula is used to determine the shear strength of soils, which is crucial for designing stable slopes, retaining walls, and foundations. - Earth Pressure Formula: This formula is used to calculate the pressure exerted by soil against retaining structures such as retaining walls and sheet piles. - Lateral Earth Pressure Formula: This formula is used to determine the horizontal pressure exerted by soil against retaining structures, such as basement walls or bridge abutments.
2. How can the bearing capacity of a soil be calculated using geotechnical engineering formulas?
Ans. The bearing capacity of a soil can be calculated using the following geotechnical engineering formulas: - Terzaghi's Bearing Capacity Formula: Q = cNc + γDNq + 0.5γBNγ - Meyerhof's Bearing Capacity Formula: Q = c'Nc + γDNq + 0.5γBNγ - Hansen's Bearing Capacity Formula: Q = c'Nc + γDNq + 0.5γBNγ + 0.4γL In these formulas, Q represents the ultimate bearing capacity of the soil, c is the cohesion of the soil, γ is the unit weight of the soil, Nc, Nq, Nγ, and Nq are bearing capacity factors, and B, D, and L represent the width, depth, and length of the foundation, respectively.
3. How can the settlement of saturated cohesive soils be estimated using geotechnical engineering formulas?
Ans. The settlement of saturated cohesive soils can be estimated using the following geotechnical engineering formula: - Terzaghi's Consolidation Settlement Formula: ΔH = (Cv × γ × H × log10(t2/t1))/ (2.303 × (1 + e0)) In this formula, ΔH represents the settlement of the soil, Cv is the coefficient of consolidation, γ is the unit weight of the soil, H is the thickness of the soil layer, t2 and t1 represent the final and initial time intervals, and e0 is the void ratio of the soil.
4. How can the shear strength of soils be determined using geotechnical engineering formulas?
Ans. The shear strength of soils can be determined using the following geotechnical engineering formulas: - Mohr-Coulomb Shear Strength Formula: τ = c + σn tan(φ) - Terzaghi's Effective Stress Shear Strength Formula: τ = σ' tan(φ') In these formulas, τ represents the shear strength of the soil, c is the cohesion, σn is the normal stress, φ is the angle of internal friction, σ' is the effective normal stress, and φ' is the effective angle of internal friction.
5. How can the lateral earth pressure exerted by soil against retaining structures be calculated using geotechnical engineering formulas?
Ans. The lateral earth pressure exerted by soil against retaining structures can be calculated using the following geotechnical engineering formulas: - Rankine's Earth Pressure Theory: PL = Ka × γ × H - Coulomb's Earth Pressure Theory: PL = Ka × γ × H + Kp × σv In these formulas, PL represents the lateral earth pressure, Ka is the active earth pressure coefficient, Kp is the passive earth pressure coefficient, γ is the unit weight of the soil, H is the height of the retaining structure, and σv is the vertical effective stress.
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