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Transcript of SOIL MECHANICS (BCE 3303) Seepage and Flownet Lecture Mdm Nur Syazwani LINTON UNIVERSITY COLLEGE...
![Page 1: SOIL MECHANICS (BCE 3303) Seepage and Flownet Lecture Mdm Nur Syazwani LINTON UNIVERSITY COLLEGE SCHOOL OF CIVIL ENGINEERING.](https://reader036.fdocuments.us/reader036/viewer/2022062300/56649e115503460f94afdeb3/html5/thumbnails/1.jpg)
SOIL MECHANICSSOIL MECHANICS(BCE 3303)(BCE 3303)
Seepage and FlownetSeepage and Flownet
Lecture
Mdm Nur SyazwaniMdm Nur Syazwani
LINTON UNIVERSITY COLLEGELINTON UNIVERSITY COLLEGESCHOOL OF CIVIL ENGINEERINGSCHOOL OF CIVIL ENGINEERING
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INTRODUCTION
DAMWater
Seepage
Vx
Vz
Water
Vx
Vz
Two-dimensional flow
PERMEABLE SOIL
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INTRODUCTION
• Pore spaces between soil particles are interconnected and water is free to flow within the soil mass
• Flow of water through soils is called seepage. • Seepage takes place when there is difference in
water levels on the two sides of the structure• The vertical and horizontal velocity components
vary from point to point within the cross-section of the soil mass
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• If we know the permeability of the soil, how do we compute the discharge through the soil?
• How do we compute the pore water pressures at various locations in the flow region or assess the uplift loading on the bottom of the concrete dam?
• Is there any problem with hydraulic gradient being too high within the soil?
To address all these, let’s look at some fundamentals in flow……
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FLOW THROUGH SOILS
• Bernoulli’s equation for steady flow of non-viscous incompressible flow:
Total head =
• When water flow through soil, the seepage velocity is often very small and negligible, Bernoulli’s equation becomes:
g
vz
g
p
w 2
2
Pressure HeadElevation Head
Velocity Head
zg
p
w
Total head =
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DARCY’S LAW
• In saturated condition, 1-D flow is governed by Darcy’s Law:
• The quantity flowing is therefore given by:
L
hkkiv
Flow Velocity
Permeability of SoilHydraulic Gradient
Difference in Total Head
Flow Path Length
AkiAvq Area through which flow is taking place
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TWO-DIMENSIONAL FLOW
Seepage taking place around water retaining structure (sheet pile, dams etc.) and embankments is 2-D i.e. vx & vz vary from point to point
A Flow Net is a graphical solution to the Laplace equation for two-dimensional flow in a homogenous and isotropic (kh = kv) soil mass
Two sets of derived orthogonal curves :
a)Equipotential Lines
b)Flow Lines
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FLOW NET(GRAPHICAL PROPERTIES)
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FLOW NET(GRAPHICAL PROPERTIES)
a) Flow lines and Equipotential lines are perpendicular
b) Grids are curvilinear squares, where diagonals cross at right angles
c) Impermeable boundary is a flow line
d) The quantity of seepage,
(flow interval)
(equipotential drop)
e) At any point,
Total head = Elevation Head + Pressure Head
d
f
N
NkHq
pet hhh
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FLOW NET (CONSTRUCTION RULES)
a) Draw to scale the cross sections of the structure, water elevations, and aquifer profiles
b) Establish boundary conditions, and draw one or two flow lines and equipotential lines near the boundaries
c) Sketch intermediate flow lines and equipotential lines by smooth curves adhering to right-angle intersections and square grids. Where flow direction is a straight line, flow lines are an equal distance apart and parallel
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FLOW NET (CONSTRUCTION RULES)
d) Continue sketching until a problem develops. Each problem will indicate changes to be made in the entire net. Successive trials will result in a reasonably consistent flow net
e) In most cases, 5 to 10 flow lines are usually sufficient. Depending on the number of flow lines selected, the number of equipotential lines will automatically be fixed by geometry and grid layout
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INSTABILITY (‘PIPING’)
• ‘Piping’ effect – an unstable condition cause by the vertical component of seepage pressure (upward direction) exceeds the weight of the soil (downward direction)
• Piping failure can lead to the collapse of a water-retaining structure
• Factor of safety against piping = Downward Weight
Upward Seepage Force
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Example 1
Impermeable Stratum
Sand
8m
3.5m0.5m
Water Level
Water Level
k = 6.5 x 10-4 m/s
e = 0.68
G = 2.6214m
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Example 1
Impermeable Stratum
8m
3.5m0.5m
Water Level
Water Level
14m
k = 6.5 x 10-4 m/s
e = 0.68
G = 2.62
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Example 1 – Sheet Piles
Impermeable Stratum
8m
3.5m0.5m
Water Level
Water Level
14m
k = 6.5 x 10-4 m/s
e = 0.68
G = 2.62
A
Impermeable Stratum
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Solution 1a:
Flow Interval, Nf = 4.3Equipotential Drop, Nd = 11
The quantity of seepage beneath the sheet pile,
= 2744.18 l/h per m
3600100011
3.43105.6 4
d
f
N
NkHq
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Solution 1b:
Taking the impermeable stratum as datum,
hT @ upstream = 17.5mhT @ downstream = 14.5m
hT loss = 0.273m (per square)
11
3
dN
H
Point ht (m) he hp u (kPa)
A 17.5 17.5 0 0
B 17.5 - (2 x 0.273) = 16.954 10 6.954 68.22
C(TOE) 17.5 - (5 x 0.273) = 16.135 6 10.135 99.42
D 17.5 - (8 x 0.273) = 15.316 8 7.316 71.77
E 17.5 - (10 x 0.273) = 14.77 12 2.77 27.17
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Solution 1c:Check again piping:
19.27 kN/m3
Effective weight of soil,
302.72 kN/m run
Upward seepage force,
397.68 kN/m run Piping failure will occur due to the upward seepage force is (397.68
kN/m) larger than the effective weight of the soil (302.72 kN/m)
81.968.01
68.062.2
1 ws
sat e
eG
2
8881.927.19W
2
842.99
2
DuF TOE
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Example 1 (continued)
Impermeable Stratum
11m
3.5m0.5m
Water Level
Water Level
14m
k = 6.5 x 10-4 m/s
e = 0.68
G = 2.62
Increase the sheet pile to a depth of 11m
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Flow Interval, Nf = 6.3Equipotential Drop, Nd = 16
Flow Interval, Nf = 4.5Equipotential Drop, Nd = 16
3600100016
3.63105.6 4
d
f
N
NkHq 36001000
16
5.43105.6 4
d
f
N
NkHq
2764.13 l/h per m 1974.38 l/h per m
hT loss = 0.1875 (per square)
16
3
dN
H
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Point ht (m) he hp u (kPa)
Point ht (m) he hp u (kPa)
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Example 2
A river has a water depth of 3m above the clayey sand base. The clayey sand layer is 14m thick which in turn overlies impermeable rock.
Laboratory tests indicate that the average permeability of the clayey sand is 4 x 10-3 m/s. The void ratio of the clayey sand is 0.6 and the specific gravity of the grains is 2.65.
It is required to excavate a 35m long, 5m wide and 6m deep trench across the river. To facilitate this work, a cofferdam is to be constructed by driving 2 lines of sheet piles to a depth of 10m below the clayey sand.
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Example 2 – Cofferdam
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Example 3 – Concrete Dam
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Example
Impermeable Stratum
Sand
12m
5.0m1.0m
Water Level
Water Level
k = 1 x 10-4 m/s
21mγsat = 16.5 kN/m3
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Example
Impermeable Stratum
12m
5.0m1.0m
Water Level
Water Level
k = 1 x 10-4 m/s
21mγsat = 16.5 kN/m3
![Page 36: SOIL MECHANICS (BCE 3303) Seepage and Flownet Lecture Mdm Nur Syazwani LINTON UNIVERSITY COLLEGE SCHOOL OF CIVIL ENGINEERING.](https://reader036.fdocuments.us/reader036/viewer/2022062300/56649e115503460f94afdeb3/html5/thumbnails/36.jpg)
Example
Impermeable Stratum
12m
5.0m1.0m
Water Level
Water Level
k = 1 x 10-4 m/s
21mγsat = 16.5 kN/m3