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3. Concrete Dam
• Forces Acting on gravity dam
• Load Combination for design
• Design Method of gravity dam
• Loads on arch dams
• Method of design
• Buttress dam
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Gravity Dam
Loads on concrete dams
Loads can be classified in terms of applicability/relative
importance as primary loads, secondary loads, and exceptional
loads.
• Primary Loads: are identified as those of major importance to all
dams, irrespective of type,
e.g. water and related seepage loads, and self-weight loads.
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Contd
• Secondary Loads: are universally applicable although of lessermagnitude (e.g. sediment load ) or,
– alternatively, are of major importance only to certain types of
dams (e.g. thermal effects within concrete dams).
• Exceptional Loads: are so designed on the basis of limited general
applicability or having a low probability of occurrence
(e.g. tectonic effects, or the inertia loads associated with seismic
activity).
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Contd
• loading diagram on gravity dams
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Contd
Primary Loads
I. Water Load
Hydrostatic distribution of pressure with horizontal resultant force P1
Vertical component of load will also exist in the case of an upstream
face batter
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Contd
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Contd
II. Seepage loads/uplift
The uplift is supposed to act on the whole width of the
foundation
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Contd
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Contd Uplift pressure distribution for perfectly tight cutoff walls
γωh1
γωh2 γωh2
γωh2γωh1 γωh2
γωh1
When flow from u/s to d/s face is allowed With u/s effective cutoff
With d/s effective cutoff With an intermediate cutoff
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Contd
Value of area reduction factor Suggested by
0.25 to 0.40 Henry
1.00 Maurice Levy
0.95 to 1.00 Terzaghi
the value C = 1.00 is recommended
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Contd
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Contd
III. Self weight load
.
For a gravity dam the weight of the structure is the main stabilizingforce, and hence the construction material should be as heavy as
possible
Structure self weight is accounted for in terms of the resultant, W,
which acts through the centroid (center of gravity) of the cross-sectional
area
W = γc * A
Where:γc is the unit weight of concrete
A is the cross-sectional area of the structure
The unit weight of concrete may be assumed to be 24 kN/m3
in theabsence s ecific data from laborator test trials
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Contd
Secondary loads
I. Sediment Load
The gradual accumulation of significant deposits of fine sediment ,
notably silt, against the face of the dam generates a resultant
horizontal force, Ps.
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Contd
II. Hydrodynamic wave
The upper portions of dams are subject to the impact of waves, Pwave.
The dimensions and force of waves depend on the extent of water
surface, the velocity of wind, and other factors
Wave run-up
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Contd
Fetch length ( fetch – continuous area of water over which
the wind blows in a constant direction)
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Contd
As a basis for wave height computation, Hs
(crest to trough), the
Stevenson equation can be used.
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Contd
III. Wind Load
When the dam is full, wind acts only on the downstream side thuscontribute to stability
It may be taken as 100 to 150 kg/m² for
the area exposed to the wind pressure
(Varshney, 1986).
ToeHeel
F'H
FW
FU
F'V
FOD
W
FV
FWA
FWA
FH
Fs
Where:
H = Head water depth
H’ = Tail Water depth
F WA = Wave pressure force
F H = Horizontal hydrostatic force
F S = Silt/sediment pressure force
F EQ = Earthquake/Seismic force
F W = Wind pressure force
F H’ = Tail water hydrostatic force
W = Weight of dam
F OD = Internal pore water pressure
F U = Uplift pressure force [base of dam]
F V = Weight of water above dam [u/s]
F V ’ = Weight of water above dam [d/s]
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Contd
Exceptional Loads
I. Seismic Load
Under reservoir full conditions, the most adverse seismic loadingwill then occur when a ground shock is associated with:
– Horizontal foundation acceleration operating upstream, an
– Vertical foundation acceleration operating downwards.
Earthquake Direction
Direction of vibraion
Reservoire fullReservoir empty
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Contd
The acceleration intensities are expressed by acceleration
coefficients h (Horizontal) and v (vertical) each representing the
ratio of peak ground acceleration
Horizontal and vertical accelerations are not equal, the former
being of greater intensity ( h = (1.5 – 2.0
v ).
Inertia forces
Horizontal Feqh
= ±αh
W
Vertical Feqv = ±αvW
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Contd
Water body
• As analyzed by Westerguard(1993)
where k” = earthquake factor for the water body
''.32
.''
k y H yF
y H k P
whewy
wh y
γ α
γ α
=
=
2
100075.71
816.0"
−=
T
H k Where: T = period of earthquake
γw = in tone/m3
H, y in meters
The force acts at 0.4y from the dam joint being
considered.
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Contd
• For inclined upstream face of dam
• where φ is the angle the face makes with the vertical.
• The resultant vertical hydrodynamic load, Fewv, effective above an
upstream face batter or flare may be accounted for by applicationof the appropriate seismic coefficient to vertical water load. It is
considered to act through the centroid of the area.
Fewv = ±αv Fv
φ γ α cos.'' y H k P wh y =
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Contd
• Load Combinations
– A concrete dam should be designed with regard to the most
rigorous adverse groupings or combinations of loads, which have
a reasonable probability of simultaneous occurrence.
– Three nominated load combinations are sufficient for almost all
circumstances.
– In ascending order of severity they may be designated as normal,
unusual, and extreme load combinations, denoted as NLC, ULC
and ELC, respectively
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Contd
• Load Combinations
• Load combination A (construction condition or empty reservoir
condition): Dam completed but no water in the reservoir and no tail
water.
• Load combination B (Normal operating condition): Full reservoir
elevation (or top of gates at crest), normal dry weather tail water,
normal uplift, ice and uplift (if applicable)
• Load combination C (Flood Discharge condition): Reservoir at
maximum flood pool elevation, all gates open, tail water at flood
elevation, normal uplift, and silt (if applicable)
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Contd
• Load combination D - Combination A, with earthquake.
• Load combination E - Combination A, with earthquake but no ice
• Load Combination F - Combination C, but with extreme uplift (drain
inoperative)
• Load Combination G - Combination E, but with extreme uplift (drain
inoperative)
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Contd
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ContdGRAVITY DAM DESIGN AND ANALYSIS
The essential conditions to structural equilibrium and basicstability requirements for a gravity dam for all conditions of loading
are
Safe against overturning at any horizontal plane within thestructure, at the base, or at a plane below the base.
Safe against sliding on any horizontal or near-horizontal planes
within the structure, at the base, or on any rock seam in the
foundation.
The allowable stresses in both the concrete or in the foundation
material shall not be exceeded.
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ContdContd
The essential conditions to structural equilibrium and so to stability
can be summarized as:
Assumptions inherent in preliminary analyses using gravity method
(USBR) are as follows:The concrete (or masonry) is homogeneous, isotropic and
uniformly eastic .
All loads are carried by gravity action of vertical parallel-sidedcantilevers with no mutual support between adjacent cantilevers
(monoliths).
No differential movements affecting the dam or foundation occur
as a result of the water load from the reservoir.
∑∑ == 0VH ∑ = 0 M
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ContdContd
Overturning Stability
Factor of safety against overturning, F0, in terms of moments about
the downstream toe of the dam:
It may be noted that M-ve is inclusive of the moments generated by
uplift load
F0 > 1.25 may be acceptable, but F0 ≥ 1.5 is desirable
∑∑
−
+=ve
ve
0M
MF
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Contd
∑∑=
V M Locationt sul tanRe
Overturning stability is considered satisfactory if the resultantintersects the base within the kern, and allowable stresses are not
exceeded
For earthquake loads, the resultant may fall anywhere within the
base, but the allowable concrete or foundation pressure must not be
exceeded
The resultant location along the base is computed from
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Contd
Sliding Stability
Resistance to sliding any plane above the base of a dam is a function
of the shearing strength of concrete, or of the construction lift joint
The sliding stability is based on a factor of safety, Fs , as a measure of
determining the resistance of the structure against sliding
Estimated using one or other of three definitions:
•Sliding factor, Fss,•Shear friction factor, FSF,
•Limit equilibrium factor, FLF.
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Contd
Sliding Stability
d
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Contd
The resistance to sliding or shearing, which can be mobilized across a
plane, is expressed through the parameters cohesion, c, and frictional
resistance, tanΦ.
Sliding Factor, FSS
FSS is expressed as a function of the resistance to simple sliding
over the plane considered
∑∑=
V
HFSS
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C d
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Contd
Shear-friction factor, FSF
•FSF is the ratio of the total resistance to shear and sliding
which can be mobilized on a plane to the total horizontal load .
• S is the maximum shear resistance, which can be mobilized.
∑
=
H
SFSF
( ) ( )∑ α+φ+αφ−α= tanVtantan1cos
cAS h
where Ah is the area of plane of contact or sliding
C d
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Contd
For the case of a horizontal plane (α =0), the above equation is
simplified to
And hence∑ φ+= tanVcAS h
∑
∑
φ
H
tanVcAF
h
SF
Sliding and shearing resistance: shear-friction factor
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C td
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Contd
This is effected by modifying the equations accordingly as,
( ) ∑+= HPSF pSF
( ) ( )α+φ+
αφ−α= tanW
tantan1cos
AcP w
AB
p
.
Where
Ww is the weight of the wedge
In the presence of a horizon with low shear resistance, e.g. a thin
clay horizon or clay infill in the discontinuity , it may be advisable to
make the assumption S =0, in the above equation
C td
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Contd
.
USBR recommended values of FSF summarized
C td
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Contd
.Limit equilibrium factor, FLE
This approach follows the conventional soil mechanics logic in
defining the limit equilibrium factor, F LE , as the ratio of shear strength
to mean applied shear stress across the plane
τ
τ= f
LEF
Contd
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Contd
.
For a single plane sliding mode, the above equation will be
Note that for α =0 (horizontal sliding plane) the above expression
simplifies toFLE = FSF
Contd
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Contd
.
The recommended minima for FLE (limit equilibrium factor of safety)
against sliding are
• FLE = 2.0 in normal operation, i.e. with static load maxima applied,and
•FLE = 1.3 under transient load conditions embracing seismic activity.
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Stress Analysis-Gravity Dams
• The basis of the gravity method of stress analysis is the assumption
that the vertical stresses on any horizontal plane vary uniformly as
a straight line, giving a trapezoidal distribution. This is often
referred to as “trapezoidal law.”
• Its validity is questionable near the base of the dam where stress
concentrations arise at the heel and toe due to reentrant corners
formed by the dam faces and the foundation surface.
Contd
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Contd
• The primary stresses determined in a comprehensive analysis by
the gravity method are:
Contd
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Contd
Contd
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Contd
With the trapezoidal law, the vertical stress, σz, may be found by the
following equation, which is the familiar equation for beams withcombined bending and axial load:
Vertical Normal Stress
I
yM
A
V *
h
z
∑∑ ′±=σ
where
∑V = resultant vertical load above the plane considered, exclusive of
uplift,
∑M* = summation of moments determined with respect to the centroidof the plane,
y’ = distance from the neutral axis of the plane to the point where σz is
being determined , and
I = the second moment of area of the plane with respect to its centroid.
Contd
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Contd
•For a regular two-dimensional plane section of unit width parallel to
the dam axis, and with thickness T normal to the axis,
.
3zT
yeV12
T
V ∑∑ ′±=σ
Contd
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Contd
where
e is the eccentricity of the resultant load R, which must
intersect the plane downstream of its centroid for the reservoir
full condition. (The signs are interchanged for reservoir empty
condition of loading)..
Contd
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Contd
For e > T/6, upstream face stress will be negative, i.e. tensile.
.
Requirements for stability
Concrete dam must be free from tensile stress
e ≤ B/6 (law of the middle third)
Contd
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Contd
For e > T/6, upstream face stress will be negative, i.e. tensile.
.
Requirements for stability
Concrete dam must be free from tensile stress
e ≤ B/6 (law of the middle third)
Contd
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Contd
For e > T/6, upstream face stress will be negative, i.e. tensile.
.
Requirements for stability
Concrete dam must be free from tensile stress
e ≤ B/6 (law of the middle third)
Contd
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Contd
.
Vertical Stress
on the base of
a gravity dam
Contd
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• Horizontal shear stresses
Numerically equal and complementary horizontal (τzy) and (τyz)shear stresses are generated at any point as a result of the variationin vertical normal stress over a horizontal plane.
If the angles between the face slopes and the vertical are respectivelyΦu upstream and Φd downstream, and if an external hydrostaticpressure, pw, is assumed to operate at the upstream face, then
Upstream horizontal shear stress
Downstream horizontal shear stress
( ) uzuwu tan p φσ−=τ
d zd d tanφσ=τ
Contd
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Contd
.
Contd
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Contd
.
Contd
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Contd
• Horizontal normal stresses
The differences in shear forces are balanced by the normal stresses
on the vertical planes
The boundary values for σy at either face are given by the following:
– for the upstream face,
– for the downstream face,( ) u
2
wzuwyu tan p p φ−σ+=σ
d
2
zd yd tan φσ=σ
Contd
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Contd
• Principal stresses
The principal stresses are the maximum and minimum normal
stresses at a point
Principal stresses σ1 and σ3 may be determined from knowledge of σzand σy
– For major principal stress
– For minor principal stress,
max
yz
12
τ+σ+σ
=σ
max
yz
32
τ−σ+σ=σ
2yz
max
2
τ
σ
=
Contd
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Contd
max
yz
12
τ+σ+σ
=σ
max
yz
32
τ−σ+σ=σ
2yz
max
2
τ
σ
=
Contd
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Contd
As there is no shear stress at and parallel to the face, that is one of
the planes of principal stress, the boundary values of σ1 and σ3 are
then determined as follows:
-For upstream face
-For downstream ace , assuming no tail water
) u2
wu2
zuu1 tan ptan1 φ−φ+σ=σ
wu3 p=σ
d
2
zd d 1 tan1 φ+σ=σ
0d 3 =σ
Contd
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Contd
• Permissible stresses and cracking
The compressive stresses generated in a gravity dam by
primary loads are very low
A factor of safety, Fc, with respect to the specified minimumcompressive strength for the concrete, is nevertheless
prescribed; is a common but seldom critical criterion.cσ
3≥cF
Table: Permissible compressive stresses (after USBR, 1976)
Contd
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Horizontal cracking is sometimes assumed to occur at the up stream
face if (computed without uplift) falls below a predetermined
minimum value:
zuσ
t
t wd
zuF
Z K
'
'
min
'σ γ σ
−=
Contd
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• Cracked Base Analysis
For a horizontal crack a direct solution may be obtained bythe following equation:
Where:
B = total base width
b = base width in compression
Mo = sum of moments at the toe excluding uplift
V = sum of vertical forces excluding uplift
p = unit uplift pressure at heel
Contd
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A resulting negative value for
b indicates an overturning
condition with the resultant
falling downstream of the toe
After the width b is found, themaximum base pressure can be
determined, and then the overturning
and sliding stabilities can be
evaluated.
Contd
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• Uplift Pressure Distribution
Case-1: Uplift distribution with drainage gallery
Contd
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Case-2: Uplift distribution with foundation drains near upstream
face
Contd
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• Case-3: Uplift distribution cracked base with drainage, zero
compression zone not extending beyond drains
Contd
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• Case-4: Uplift distribution cracked base with drainage, zero
compression zone extending beyond drains
Buttress Dam
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• Buttress dams consists of principal structural elements:
A sloping upstream deck that supports the water
The buttress or vertical walls that support the deck and transmit
the load
• According to the structure of the dam deck, buttress dams classified
as:
Buttress dams with a massive head
Buttress dams with a flat slab deck
Buttress dams with thin curved multiple arch deck
Contd
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Buttress dams with a massive head
– Round head buttress dam – Diamond head buttress dams
– T-head buttress dams
Contd
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• Buttress dams with a flat slab deck
– Simple or Amburson slab buttress
– Fixed or continuous deck slab buttress Cantilever deck slab
buttress dam:
Contd
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Contd
• Longitudinal beams are used for stiffing and bracing the buttresses
• Foundation slab below the entire dam, provided with drainage
openings for eliminating the uplift pressure
• The stability against sliding is ensured with the weight of water on
the inclined deck and on the amount of the decrease in the uplift
pressure
Contd
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Contd
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Contd
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• The distance l between the buttresses and the angle of inclination of
the dam barrier can be determined from the condition for sliding
stability of dam
α
( )
s
PK
K
bd c f U W GGW
..2
1
+−++=
Contd
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• Example
#The profile of the major monolith of a buttress dam is illustrated in the
figure. The stability of the dam is to be reviewed in relation to:
Normal Load Condition (NLC): Water load(to design flood level + self
weight + uplift(no pressure relief drain)
Static stability : Overturning, Fo>1.5; sliding (shear friction factor),FSF >2.4.
Concrete characteristics: Unit weight 23KN/m3 , Unit shear
resistance , C = 500KN/m2 , angle of shearing resistance (internal
friction) = 350
C γ
C φ
Contd
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1. Analyze the static stability of the buttress unit with respect to plane
X–X under NLC and in relation to the defined criteria for Fo and F
SF.
2. Concern is felt with regard to stability under possible seismic loading.
Dynamic stability criteria are specified as Fo = 2.0; FSF =3.2, and will be
met by prestressing as shown. Determine the prestress load required in
each inclined tendon.
Contd
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• Solution
1.
– All calculations relating to stability refer to the monolith as a
complete unit.
– Uplift is considered to act only under the buttress head, and
– The profile is subdivided into the elements A, B and C, identified
in figure for convenience
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The load–moment table (all moments are relative to toe) is as follows:
Contd
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2. The load–moment table (all moments are relative to toe) is as
follows:
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Arch Dam
• An arch dam is a curved dam that carries a major part of its waterload horizontally to the abutments by arch action
• Arch (or arch unit) refers to a portion of the dam bounded by two
horizontal planes, 1 foot (1 meter) apart.
• Cantilever (or cantilever unit) is a portion of the dam contained
between two vertical radial planes, 1 foot (or 1 m) apart.
• Extrados and Intrados: Extrados is the upstream face of arches
and intrados is the downstream face of the arches.
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Contd
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Valley suited for arch dam
• Narrow gorges provide the most natural solution for an arch damconstruction, the usually recommended ratio of crest length to dam
height being 5 or less.
• The overall shape of the site is classified as a narrow-V , wide-V ,narrow-U , or wide-U as shown in Figure
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• Sarkaria proposed a canyon shape factor (C.S.F.), which would
indicate the suitability of a site for arch dam as follows
H
H BCSF
)sec(sec 21 ψ ψ ++=
•The usual values of C.S.F. are 2 to 5; lower value giving thinner sections
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Valley type Bottom width
B
ψ1 ψ2 CSF
U shaped < H < 150 < 150 < 3.1
Narrow V shaped 0 < 350 < 350 < 2.4Wide V-shaped 0 > 350 > 350 > 2.4
Composite U-V
shaped
< 2H > 150 > 150
≅ 4.1
Wide and flatshapes
> 2H ψ1 ψ2 > 4.1
Unclassified Highly irregular valley shape
Classification of valley shapes based on CSF value
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• Arch dams may be grouped into two main divisions:
– Massive arch dam:- the whole span of the dam is covered by asingle curved wall usually vertical or nearly so.
– Multiple arch dam:- series of arches cover the whole span of
the dam, usually inclined and supported on piers or buttresses.
• Massive arch dams are divided into the following types:
– Constant radius arch dams – Constant angle arch dams
– Variable radius arch dams
– Double curvature or Cupola arch dams
– Arch gravity dams
ContdA h t d fil
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• Arch geometry and profile
The horizontal component of arch thrust must be transferred into the
abutment at a safe angle, β, (i.e. one that will not promote abutmentyielding or instability)
At any elevation the arch thrust may be considered to enter theabutment as shown in Figure
In general an abutment entry angle, β, of between 45 and 70° issuggested
Angle between arch thrust and rock contours
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Arch and cupola profiles are based on a number of geometrical
forms, the more important of which are:
Constant-radius profile
Constant-angle profile
Constant radius profile
Has the simplest geometry, combining a vertical U/S face of constant
radius with a uniform radial D/S slope
The downstream face radius varies with elevation and the centralangle, 2θ, reaches a maximum at crest level .
The profile is suited to relatively symmetrical U-shaped valleys.
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Constant Radius profile
ContdC l fil
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Constant-angle profile
Also known as variable-radius arch dam; usually have extradosand intrados curves of gradually decreasing radii as the depth
below the crest increases
This is to keep the central angle as large and as nearly constant aspossible, so as to secure maximum arch efficiency at all elevations.
They are often of double curvature. Frequently adapted to narrow
steep-sided V-shaped valleys
It is economical type of profile using about 70% concrete as
compared to a constant radius arch dam
Contd
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Constant Angle profile
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Cupola profile:
Has a particularly complex geometry and profile, with constantly
varying horizontal and vertical radii to either face.
ContdC C til
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• Crown Cantilever:
The crown cantilever is defined as the maximum height vertical
cantilever and is usually located in the streambed
• Single Curvature :
Single-curvature arch dams are curved in plan only . Vertical
sections, or cantilevers, have vertical or straight sloped faces.
• Double Curvature :
Double-curvature arch dams means the dam is curved in plan and
elevation
This type of dam utilizes the concrete weight to greater advantage
than single-curvature arch dams
Contd
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Contd
L d h d
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Loads on arch dam
• The forces acting on arch dam are the same as that of gravity dams
– Uplift forces are less important (not significant)
– Internal stresses caused by temperature changes and yielding
of abutments are very important
– The principal dead load is the concrete weight
– The principal live load is the reservoir water pressure
– An arch dam transfers loads to the abutments and foundations
both by cantilever action and through horizontal arches
Contd
L d h d
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Loads on arch dam
• The forces acting on arch dam are the same as that of gravity dams
– Uplift forces are less important (not significant)
– Internal stresses caused by temperature changes and yielding
of abutments are very important
– The principal dead load is the concrete weight
– The principal live load is the reservoir water pressure
– An arch dam transfers loads to the abutments and foundations
both by cantilever action and through horizontal arches
Contd
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• Methods of design of massive arch dams
a. Thin cylinder theory
b. Thick cylinder theory
c. The elastic theory
d. Other advanced methods such as trial load analysis and finite
element methods.
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a. Thin Cylinder (Ring) Theory
The weight of concrete and water in the dam is carried directly to the
foundation
The horizontal water load is carried entirely by arch action
In thin cylinder theory, the stresses in the arch are assumed to be
nearly the same as in a thin cylinder of equal outside radius
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Contd
If R i h b i i i h
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If R is the abutment reaction its component in the upstream
direction which resist the pressure force P is equal to
The hydrostatic pressure acting in the radial) direction
Total hydrostatic force = hydrostatic pressure x projected area
Summing forces parallel to the stream axis
2sinθ R
hP wγ =
2sin2 θ γ ew
r hP ×=
ew
ew
hr R
hr R
γ
θ γ θ
=
= 2/sin22/sin2
Contd
If th thi k (t) f th h i i ll d ith it b
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If the thickness (t) of the arch ring is small compared with re it may be
assumed that uniform compressive stress is developed in the arch
ring
The transverse unit stress
For a given stress, thickness t
Note: the hydrostatic pressure γ w h may be increased by earth quake and
other pressure forces where applicable:
t
hr
t
Rew
γ σ ==
1*
all
ewhr t σ
γ =
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• This equation indicates that the thickness t of the arch ring increases
linearly with depth below the water surface and for a given pressure
the required thickness is proportional to its radius.
• Thickness relation in terms of intrados, ri and mean radius rc , can be
derived as follows
since r e = r c + 0.5t and r e = r i + t
OR
all
ewhr t
σ
γ =
h
hr t
wall
cw
γ σ
γ
5.0−=
h
hr t
wall
iw
γ σ
γ
−=
Contd
B C l A l
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• Best Central Angle
The concrete volume of any given arch is proportional to the
product of the arch thickness and the length of the centerline arc
The volume of unit height of arch
2
2
2/sin2
)1*(
==
===
θ θ θ
σ
γ θ
Bk kr V
kr hr
t
r t V w
Differentiating V with respect to θ and setting to zero, θ = 133.5o
which is the most economical angle for arch with minimum volume
For = 133.50 ,r = 0.544B
Contd
b Thi k C li d (Ri ) Th
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b. Thick Cylinder (Ring) Theory
Improvement in thin cylinder theory was made by the considering
the arch as thick cylinder .
)( 222
22
2
m MN
r r
r
r r r P
ie
ie
ew
−
×+
=σ
The compressive horizontal ring stress, σ, for radius r is given by
Contd
Stress is maximum at the downstream face
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Stress is maximum at the downstream face ,
Thickness assumed uniform at any elevation h,
With
ie r r t −=
hP wγ =
( )
+
=ie
ew
r r t
hr r 2
max
2σ for ir r =
Contd
E l
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• Example:
# Given a canyon with the following dimensions, compute and draw the
layout of arch dams of constant radius and constant angle profiles.
Data - Maximum height = 100m
-Top width of the valley = 500m-Bottom width of valley =200m
-Allowable stress in concrete, MPaall 5=σ
Contd
S l ti U i hi li d h d
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• Solution-Using thin cylinder method
1. Constant radius
Let the central angle be 150o
Assume top width , 1.5m or assume 0
hhhr
t
m B
r
all
ew
e
508.05000
82.25881.9
82.25875sin2
500
2sin2
=×
==
===
σ
γ
θ
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Depth
(m)
Valley
width(m) t=0.508h ri = re - t B/2re
0 500 0 258.82 0.965910 470 5.08 253.74 0.9080
20 440 10.16 248.66 0.8500
30 410 15.24 243.58 0.7921
40 380 20.32 238.5 0.7341
50 350 25.4 233.42 0.6761
60 320 30.48 228.34 0.6182
70 290 35.56 223.26 0.5602
80 260 40.64 218.18 0.5023
90 230 45.72 213.1 0.4443100 200 50.8 208.02 0.3864
( )er B 2
sin2 −
=θ
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Contd
2 C t t A l
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2. Constant Angle
The best central angle 05.133=θ
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