Title: Soil Mechanics A
1Flow Nets
2Flow through a Dam
Phreatic line
Unsaturated Soil
Drainage blanket
Flow of water
z
x
3Graphical representation of solution
1. Equipotentials Lines of constant head,
h(x,z)
Equipotential (EP)
4Graphical representation of solution
2. Flow lines Paths followed by water
particles - tangential to flow
Phreatic line
Flow line (FL)
Equipotential (EP)
5Properties of Equipotentials
Flow line (FL)
Equipotential (EP)
h(x,z) constant
(1a)
6Properties of Equipotentials
Flow line (FL)
Equipotential (EP)
h(x,z) constant
(1a)
(1b)
Thus
7Properties of Equipotentials
Flow line (FL)
Equipotential (EP)
h(x,z) constant
(1a)
(1b)
Thus
(1c)
Equipotenial slope
8Properties of Flow Lines
Geometry
Flow line (FL)
vz
vx
Equipotential (EP)
Kinematics
From the geometry
(2b)
9Properties of Flow Lines
Geometry
Flow line (FL)
vz
vx
Equipotential (EP)
Kinematics
From the geometry
(2b) Now from Darcys law
10Properties of Flow Lines
Geometry
Flow line (FL)
vz
vx
Equipotential (EP)
Kinematics
From the geometry
(2b) Now from Darcys law Hence
(2c)
11Orthogonality of flow and equipotential lines
Flow line (FL)
Equipotential (EP)
On an equipotential
On a flow line
12Orthogonality of flow and equipotential lines
Flow line (FL)
Equipotential (EP)
On an equipotential
On a flow line
(3)
Hence
13Geometric properties of flow nets
h?h
Y
h
Z
FL
h2?h
T
EP
t
X
y
FL
X
z
14Geometric properties of flow nets
From the definition of flow
(4a)
h?h
Y
h
Z
FL
h2?h
T
EP
t
X
y
FL
X
z
15Geometric properties of flow nets
From the definition of flow
(4a)
h?h
Y
h
From Darcys law
Z
FL
h2?h
(4b)
T
EP
t
X
y
FL
X
z
16Geometric properties of flow nets
From the definition of flow
(4a)
h?h
Y
h
From Darcys law
Z
FL
h2?h
(4b)
T
EP
t
Combining (4a)(4b)
X
y
FL
X
(4c)
z
17Geometric properties of flow nets
From the definition of flow
(4a)
h?h
Y
h
From Darcys law
Z
FL
h2?h
(4b)
T
EP
t
Combining (4a)(4b)
X
y
FL
X
(4c)
z
Similarly
(4d)
18Geometric properties of flow nets
From the definition of flow
(4a)
h?h
Y
h
From Darcys law
Z
FL
h2?h
(4b)
T
EP
t
Combining (4a)(4b)
X
y
FL
X
(4c)
z
Similarly
(4d)
19Geometric properties of flow nets
B
EP( h )
C
D
FL
A
d
EP ( h ?h )
b
a
c
20Geometric properties of flow nets
From the definition of flow
B
(6a)
EP( h )
C
D
FL
A
d
EP ( h ?h )
b
a
c
21Geometric properties of flow nets
From the definition of flow
B
(6a)
EP( h )
From Darcys law
C
(6b)
D
FL
A
d
EP ( h ?h )
b
a
c
22Geometric properties of flow nets
From the definition of flow
B
(6a)
EP( h )
From Darcys law
C
(6b)
D
FL
A
d
Combining (6a)(6b)
EP ( h ?h )
b
a
(6c)
c
Similarly
(6d)
23Geometric properties of flow nets
From the definition of flow
B
(6a)
EP( h )
From Darcys law
C
(6b)
D
FL
A
d
Combining (6a)(6b)
EP ( h ?h )
b
a
(6c)
c
Conclusion
Similarly
(6d)
24Geometric properties of flow nets
- When drawing flow nets by hand it is most
convenient to draw them so that - Each flow tube carries the same flow ?Q
- The head drop between adjacent EPs, ?h, is the
same - Then the flow net is comprised of SQUARES
25Geometric properties of flow nets
Demonstration of square rectangles with
inscribed circles
26Drawing Flow Nets
To calculate the flow and pore pressures in the
ground a flow net must be drawn. The flow net
must be comprised of a family of orthogonal lines
(preferably defining a square mesh) that also
satisfy the boundary conditions.
27Common boundary conditions
a. Submerged soil boundary - Equipotential
Water
H-z
H
u
w
h
z
?
?
?
w
z
(7)
Datum
28Common boundary conditions
a. Submerged soil boundary - Equipotential
Water
H-z
H
u
w
h
z
?
?
?
w
z
now
u
H
z
?
?
?
(
)
(7)
w
w
Datum
29Common boundary conditions
a. Submerged soil boundary - Equipotential
Water
H-z
H
u
w
h
z
?
?
?
w
z
now
u
H
z
?
?
?
(
)
(7)
w
w
Datum
so
H
z
?
?
(
)
w
h
z
H
?
?
?
?
w
30Common boundary conditions
b. Impermeable soil boundary - Flow Line
Permeable Soil
vn0
Flow Line
vt
Impermeable Material
31Common boundary conditions
c. Line of constant pore pressure - eg. phreatic
surface
Head is given by
32Common boundary conditions
c. Line of constant pore pressure - eg. phreatic
surface
Head is given by and thus
33Common boundary conditions
c. Line of constant pore pressure - eg. phreatic
surface
Head is given by and thus now if pore pressure
is constant
34Common boundary conditions
c. Line of constant pore pressure - eg. phreatic
surface
Head is given by and thus now if pore pressure
is constant and hence
(8)
35Common boundary conditions
c. Line of constant pore pressure - eg. phreatic
surface
36Procedure for drawing flow nets
- Mark all boundary conditions
- Draw a coarse net which is consistent with the
boundary conditions and which has orthogonal
equipotentials and flow lines. (It is usually
easier to visualise the pattern of flow so start
by drawing the flow lines). - Modify the mesh so that it meets the conditions
outlined above and so that rectangles between
adjacent flow lines and equipotentials are
square. - Refine the flow net by repeating the previous
step.
37Example Suction Caisson Installation
38Value of head on equipotentials
(9)
Phreatic line
15 m
Datum
h 15m
h 0
h 3m
h 12m
h 6m
h 9m
39Calculation of flow
Phreatic line
15 m
h 15m
h 0
h 3m
h 12m
h 6m
h 9m
For a single Flow tube of width 1m ?Q k
?h (10a)
40Calculation of flow
Phreatic line
15 m
h 15m
h 0
h 3m
h 12m
h 6m
h 9m
For a single Flow tube of width 1m ?Q k
?h (10a)
For k 10-5 m/s and a width of 1m ?Q
10-5 x 3 m3/sec/m (10b)
41Calculation of flow
Phreatic line
15 m
h 15m
h 0
h 3m
h 12m
h 6m
h 9m
For a single Flow tube of width 1m ?Q k
?h (10a)
For k 10-5 m/s and a width of 1m ?Q
10-5 x 3 m3/sec/m (10b)
For 5 such flow tubes Q
5 x 10-5 x 3 m3/sec/m (10c)
42Calculation of flow
Phreatic line
15 m
h 15m
h 0
h 3m
h 12m
h 6m
h 9m
For a single Flow tube of width 1m ?Q k
?h (10a)
For k 10-5 m/s and a width of 1m ?Q
10-5 x 3 m3/sec/m (10b)
For 5 such flow tubes Q
5 x 10-5 x 3 m3/sec/m (10c)
For a 25m wide dam Q
25 x 5 x 10-5 x 3 m3/sec (10d)
43Calculation of flow
Phreatic line
15 m
h 15m
h 0
h 3m
h 12m
h 6m
h 9m
For a single Flow tube of width 1m ?Q k
?h (10a)
For k 10-5 m/s and a width of 1m ?Q
10-5 x 3 m3/sec/m (10b)
For 5 such flow tubes Q
5 x 10-5 x 3 m3/sec/m (10c)
For a 25m wide dam Q
25 x 5 x 10-5 x 3 m3/sec (10d)
(10e)
Note that per metre width
44Calculation of pore pressure
Phreatic line
15 m
h 15m
h 0
5m
P
h 3m
h 12m
h 6m
h 9m
5m
P
(11a)
Pore pressure from
45Calculation of pore pressure
Phreatic line
15 m
h 15m
h 0
5m
P
h 3m
h 12m
h 6m
h 9m
5m
P
(11a)
Pore pressure from
At P, using dam base as datum
(11b)
46Example Calculating Pore Pressures
20 m
10 m
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Step 1 Choose a convenient datum. In this
example the sea floor has been chosen Then H1
40 m H2 1 m. The increment of head, ?h
39/9 4.333 m
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A
B
C
D
E
Step 2 Calculate the head at points along the
base of the vessel. For convenience these are
chosen to be where the EPs meet the vessel (B
to E) and at the vessel centerline (A). Hence
calculate the pore water pressures. At B
Head H1 - 5 ?h H2 4 ?h 18.33 m Pore
pressure at B
18.33 ?w 179.8 kPa
50Step 3 Calculate the upthrust (Force/m) due to
pore pressures
3218 kN/m Without pumping Upthrust 20 ? 1
? 9.81 196 kN/m Upthrust due to Pumping
3218 196 3022 kN/m
51S
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