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Varshney, R.S., Gupta, S.C., Gupta, R.L., “Theory and Design of Irrigation Structure”. N.C. Jain, at Roorkee press, Roorkee, India, 1982. Garg, S.K., “Irrigation Engineering and Hydraulic Structures”, Khanna Publishers, Delhi, 1976. Abdulkadir, S. Z., Mero, S.K., Yaseen, D.S. “Design of Barrage on a Proposed River”, 4th Year Graduation Project, 2008.
Page 2
In addition to the weir proper, head works consist of the following components, Undersluices. Canal head regulator.
Divide wall or groyne. Fish ladder. Piers and abutments. Protection works. River training wall.
Page 3
These are gates controlled openings in the weir with crest at low level. They are located on the same side as off-take canal. If two canal take off on either side of the river, it would be necessary to provide undersluices on either side.
Page 4
Functions of undersluices
To preserve a clear and defined river channel approaching the canal regulator. To scour silt deposited in front of canal regulator and control silt entry in the canal. To facilitate working of weir crest shutters or gates. The flood can easily pass.
To lower the highest flood level.
Page 5
Discharge Capacity of undersluices is provided of the following:
i.Qu = 2 (Qmax.)offtake ii.Qu = 20% (Qmax.)flood
Page 6
A canal head regulator is to serve the following functions:
Regulate the supply of water in the canal. Control the entry of silt in the canal.
Page 7
The head regulator is normally aligned between 90° - 120° in respect to the axis of the weir. The regulation done by means of gates, steel gates of spans ranging between (8 m-12 m) are used and operated by electric winches. Height of gates = pond level - crest level To check flood water entering the canal a breast wall between pond level and high flood level (H.F.L). Unless H.F.L - pond level is nominal, breast wall is usually more economical than high gates.
Page 8
If silt excluder is provided, it is necessary to further raise the crest of head regulator by minimum of 0.75 m. To calculate the discharge, the drowned weir formula can be used: 2 𝑄 = 𝐶1 𝐿 2𝑔 𝐻 + 𝑎 3
2
3
− 𝑎
2
where: C1=0.577, C2=0.8
H=difference of u.s and d.s water levels. L=clear length of waterway. d=depth of d.s water level above the crest.
ha=head due to velocity of approach.
Page 9
3
+ 𝐶2 𝐿𝑑 2𝑔 𝐻 + 𝑎
In case of the waterway (L) worked out more than width of the canal, the crest level so adjusted as to keep (L) equal to the width of the canal. In exceptional cases waterway more than canal width may be provided with a flared wall in the d.s of the regulator to join the canal width. Note that, the most critical condition of uplift occurs when high flood level is passed down the weir and there is no flow in canal.
Page 10
It is a wall located between weir and undersluices extending a little u.s of canal regulator, and d.s up to end of loose protection of the undersluices. It is a concrete or masonry structure, with top width (t)=(l.5-3)m, and aligned at right angle to the weir axis.
Page 11
The functions of divide walls are
To separate the floor of scouring sluices which is at lower level than the weir proper. To isolated the pockets u.s of the canal head regulator to facilitate scouring operation. To prevent formations of cross currents to a void their damaging effects. Additional divide walls are sometimes provided for this purpose.
Page 12
The divide walls are costly structures.
These walls are likely to be subjected to maximum differential pressure when the full discharge of the river is passing through the weir, (there will be difference in water level on the two sides ). Also there may exit difference in silt pressure on the two side . The values of differential pressure are taken arbitrarily say 1.0 m for water heads and about 2.0 m for silt pressure (see Fig. (5)).
Page 13
Fish ladder or fish passes are generally provided to enable the fish to ascend the head waters of the river and thus reach their spawning grounds for propagation or to follow their migratory habits in search of food.
Page 14
The general requirements of a fish ladder are:
The slope of the fish ladder should not be steeper than 1:10 (i.e velocity not exceeding 2 m/s in any portion of the fish-way). The compartments of bays of the pass must be such dimensions that the fish do not risk collision with the sides and upper end of each bay when ascending.
Page 15
The general requirements of a fish ladder are (Continued)
Plenty of light should be admitted in the fish-way. The water supply should be ample at all times. The top and sides of a fish-way should be above ordinary high water level.(see fig.(6)).
Page 16
In barrages piers are provided at an interval of 10 to 20 m. The piers support bridge decking, and working platform for the operation of gates. Cutwaters are usually simple in shape and the side face of piers is often vertical. Tapering if done, does not exceed 1/50 to 1/40. Piers should be provided with separate foundation (see Fig. (5)).
Page 17
In case, however, when raft is provided the piers may be constructed monolith with floor. Abutments are usually gravity section and founded on well packed closely in either direction. Perhaps in case of higher abutments a better alternative is to provide a counter fort type structure on open foundation.
Page 18
The sediment transporting capacity of water depends mainly on the discharge, slope and grade of material. As a result of putting obstruction across the river in form of weir, the river regime will be affected in the following sequence:
Page 19
A weir will pond up water leading to the flattening of water surface slope for some distance on the up-stream side. River would drop a part of its sediment load resulting in the formation of shoals in the pond. Clear water passes over the weir; this water scours the bed river to make up deficiency in its silt load and causes a progressive lowering or retrogression of downstream level.
Page 20
The progressive silting a formation of shoals in the u.s increases the resistance to flow of water to recover this resistance increase head is required. The overall effect of a weir is to take away the excess energy due to steep gradient by localizing it and ultimately dissipating it.
Page 21
The causes of failures may classify into:
Failure due to seepage or subsurface flow. Failure due to surface flow.
Page 22
Subsurface flow endangers the stability of a weir in the following two ways: Piping or floatation. Uplift pressure.
The surface flow endangers the weir in the following two ways: Unbalanced head due to standing wave (i.e. due to formation of the jump very high unbalanced pressures are developed in the trough). Scour in the upstream and downstream.(this occurs in the bed of alluvial rivers at flood).
Page 23
The design of weir and barrage like any hydraulic structure, consist of many phases. The two main phases are The hydraulic design (evaluation hydraulic forces acting on the structure). The structural design (dimensioning of the various part of the structure to enable it to resist safely all the forces acting on it).
Page 24
The problem involved in the hydraulic design of weir and barrage on permeable foundation may be treated under the following: Sub soil flow, and Surface flow.
Page 25
Page 26
a) Crest level of a barrage is fixed on the consolidation of existing river bed level, at the proposed site. b) The undersluices crest is usually kept as near the bed level in the deepest channel as is practically possible. The barrage bay crest is kept slightly higher and at about the general bed level in the remaining portion of the river. The undersluice crest is kept lower to attract a deep current in front of the regulators, so that the dry weather current may remain near the regulator.
Page 27
Note that afflux and discharge per meter are related to crest levels. So lower crest levels, result in lesser afflux, but higher discharge per meter. Low set barrage with increase depth of water over crest may result in an increased height of gates, thickness of floor, and cost of superstructure above floor level.
Page 28
It's necessary to check that the maximum. Flood discharge passes down the works without exceeding the afflux. The following discharge formulas may be used for this purpose: a) For broad crested weir:
𝑄 = 1.705 𝐿 − 0.1 𝑛𝐻 𝐻3
2
b) For sharp crested weir:
𝑄 = 1.84 𝐿 − 0.1 𝑛𝐻 𝐻3 where: L= total clear waterway (m)
n= number of end contractions H= the head over crest in (m) Page 29
2
Afflux actually denotes loss of head and its magnitude is represented by the difference in total energy level on upstream and the downstream of the works. Afflux is generally limited to 1 meter, but may be kept higher if permissible. To adopt for waterway is given by the following formula representing Lacey's wetted perimeter, 𝑃 = 4.83 𝑄 where: P= Lacey's wetted perimeter, and Q= Maximum flood discharge.
Page 30
In boulder reaches of the river it would be economical to reduce the waterway to about (0.6 - 0.8) time Lacey's waterway. In plains where the silt factor is in the neighborhood of unity it is generally economical to keep the waterway (1.0 - 1.2) times the Lacey's waterway. Generally the shorter waterway is preferable.
Page 31
1. Maximum flood discharge "Q“ 2. Stage discharge curve of the river at barrage. 3. Minimum water level.
Page 32
4. Cross section of the river at barrage site the following have to be decided: Lacey's silt factor (f) this is determined from the equation: 𝐹 = 1.76 𝑀𝑟
Length of waterway, discharge per meter and afflux. Safe exit gradient. Depth of sheet piles: • Scour depth. • Exit gradient.
Page 33
5. Level and length of horizontal part of d.s. impervious floor in coordination with hydraulic jump. 6. Thickness of d.s. impervious floor. •
with reference to uplift pressure.
•
with reference to hydraulic jump or standing wave.
7. Length and thickness of protection works beyond pucca floor u.s. and d.s.
Page 34
Page 35
Determine head loss (HL) for different flow condition. HL = afflux (if there is no retrogression)* If allowance for retrogression is taken in d.s bed level then, HL = afflux + retrogression, usually, 0.5 m retrogression will be sufficient in most cases.
* Retrogression is lowering d.s bed caused by water scour
Page 36
For known values of q and HL find Ef2 from blench curve (from Blench curves (Next slide)). With known values of Ef2 read corresponding values of D2. Cistern Level = D.S.T.E.L – Ef2
Ef2 = down stream specific energy. D2 = post jump corresponding to Ef2 Ef1 = Upstream specific energy. D1 = per jump depth corresponding to Ef1
Page 37
Page 38
Ef1 = Ef2 + HL Knowing Ef1 , Ef2 & q read values of D1 and D2 from Fig. 10 (next slide), energy of flow curves. Provide minimum cistern length = 5(D2–D1). = 6(D2–D1).
Page 39
Page 40
Determine scour depth from the formula
𝑅 = 1.35
1 3 2 𝑞
𝑓
Depth of u.s. sheet pile =(1–1.25)R Depth of d.s. sheet pile =(1.25–1.5)R
Page 41
Work out the value 1 𝜋 𝜆
GE =h/d.
1 𝜋 𝜆
=
from equation:
𝑑 G.E.
1 𝜋 𝜆
∝ =[(2𝛌–1)²–1]½ b=∝ 𝑑
Page 42
(for given GE.)
Provide total length of floor = ∝ 𝑑
Disposition of total floor length may be as follows 1. Cistern length = 5(D2–D1) to 6(D2–D1) 2. Glacis length = 3 to 5 times (crest level – cistern level) For 3:1 to 5:1 slope of glacis 3. Upstream floor = the balance.
Page 43
Find u.s pile and d.s pile % pressure; the pressure distribution assumed to be linear; used Khosla’s method; correct due to floor thickness, interference of sheet pile and slope.
Page 44
Page 45
Plotting water profile before and after the jump formation (Fr=
𝑞 𝑞𝐷1³
)
The intercept between the profile of hydraulic jump and the gradient gives the unbalance dynamic head. The floor thickness is, however, designed for ⅔ the max. unbalance head in jump through.
Floor thickness = H/(G–1) where: H = max static head or ⅔ max. unbalance head. (use the greater head of the two)
Page 46
The protection works are now designed in respect to the scour depth.
Page 47
Page 48
A barrage is to be constructed on Tigris River having high flood discharge 8500 cumecs. The relevant data are as follows: Average bed level of river
100 m
High flood level
105.75 m
Normal pond level
103.5 m
Permissible afflux
1m
Lacey silt factor
1m
Safe exit gradient for bed material
1/6
Concentration
20٪
Bed retrogression
0.5
Pier contraction coefficient
0.1 m
Page 49
Design a suitable regulator with reference of the barrage with the following data: 1. Full supply discharge of off-take canal
=220 cumecs
2. full supply level of canal
=102 m
3. water depth in canal
=3.5m
4. bed level of canal
=98.5 m
5. angel of off take canal
=115˚
6. safe exit gradient
=1/6
7. side slopes
=2H:1V
Page 50
-Crest of under sluice is to be provided at bed level of the river = 100 m
-Crest level of other barrage is to be (1.25)m higher than under sluice crest = 100+1.25=101.25 m -Minimum water way = 4.83 𝑄. from Lacey new edition using factor (4.75) instead of (4.83)‚ but the factor (4.83) is used for more safe. = 4.83 𝑄 = 4.83 8500 = 445.3 𝑚
Page 51
-Assume water way is as follows:
Under sluice water way: -
5 bays (13 m) each
=65m
-
4 piers(2.5m) each
=10m
Total under sluice
=75m
Other barrage water way -
30 bays (10m) each
=300m
-
29 piers(2m) each
=58m
-
Total other barrage
=358m
-
Divide wall thickness
=3m
Total water way Page 52
= 75+358+3=436m
Page 53
D.S.H.F.L =105.75 m
U.S.H.F.L =D.S.H.F.L + Afflux =105.75+1=106.75 m q =Q/B =8500/436=19.5 cumec /m 1 3
𝑅 = 1.35
𝑞2 𝑓
𝑞 V= 𝑅
1.99 m/sec
19.5 = = 9.78
= 1.35
9/52 1
1 3
= 9.78 𝑚
Velocity head =V²/2g =1.99²/2(9.81) =0.2 m U.S.T.E.L =106.75+0.2 = 106.95 m
Page 54
Head over under sluice crest =106.95-100 = 6.95 m
Head over other barrage crest =106.95-101.25=5.7 m Qunder sluice = 1.705(L-0.1nH) H3/2 =1.705(65-0.1×8×6.95)(6.95)3/2 =1856.87 m³/sec Qother barrage =1.84(L-0.1 nH) H3/2 =1.84(300-0.1×58×5.7) ×5.73/2 =6684.1 m³/sec Qtotal 1856.87 + 6684.1 = 8540.98 m³/sec >8500 m³/sec
OK Page 55
2.2.1 High flood condition
I. For high flood without concentration and retrogression q =C H3/2 =1.705(6.95)3/2=31.24 cumec/m D.S.H.F.L= 105.75 m U.S.H.F.L= 106.75 m U.S.T.E.L= 106.95 m D.S.T.E.L=105.95 m HL = U.S.T.E.L-D.S.T.E.L =106.95- 105.95 = 1 m
Page 56
II. For high flood with 20% concentration and 0.5 m bed retrogression q =1.2×31.24 = 37.488 cumec/m q =C H3/2 𝑞 𝐶
H=( )2/3 =(
37.488 2/3 ) 1.705
=7.848 m
U.S.T.E.L= 100+7.848 = 107 .848 m
D.S.H.F.L with 0.5 retrogression = 105.25 m D.S.T.E.L=105.25+0.2 = 105.45 m HL= 107.848- 105.45 = 2.398 m
Page 57
2.2.1.2 Flow at pond level
Ι. without concentration and retrogression Head over under sluice crest = 103.5-100 =3.5 m Head over other barrage crest = 103.5-101.25 =2.25 m Q =1.705(65-0.1×8×3.5×3.53/2 +1.84(300-0.1×58×2.25) ×2.253/2 = 694.41 + 1781.959 = 2476.369 m³/sec 𝑄 𝐵
q= =
Page 58
2476.369 436
=5.68 m³/sec/m
Page 59
𝑞² 1/3 R=1.35( ) 𝑓
= 4.297 m
𝑞 𝑅
V= =1.32 m/sec 𝑉² hv = 2𝑔
=0.089 m
U.S.T.E.L =103.5+ 0.089 = 103.59 m D.S water level when flood discharge of 2476.369 m³/sec is passing = 102.7 m
Page 60
From stage discharge curve Fig .8
D.S.T.E.L =102.7 + 0.089 = 102.789 m q between piers = C H3/2
= 1.705(3.5) 3/2= 11.164 m³/sec/m HL = 103.59- 102.789 = 0.801 m Page 61
II. with 20% concentration and 0.5 m retrogression
q = 1.2×11.164 = 13.3968 cumec/m head for this intensity =(
13.3968 2/3 ) 1.705
=3.9523 m
U.S.T.E.L =100+3.9523 = 103.9523 m D.S.W.L with 0.5 m retrogression = 102.7-0.5 =102.289 m
D.S.T.E.L = 102.2 + 0.089 =102.289 m HL = 103.9523-102.289 = 1.663 m
Page 62
2.2.2 Hydraulic jump calculations High Flood No.
1 2 3 4 5 6 7 8 9 10 11 12
Item
Discharge q D.S.W.L U.S.W.L D.S.T.E.L U.S.T.E.L HL Ef2 Ef1=Ef2+HL Level at which jump occurs D1 D2 Length of floor 5(D2-D1) 𝐪 √𝐠𝐃𝟏³
13 63 Page F=
Pond Flow
31.24 105.75 106.75 105.95 106.95 1 8 9
With retrogression and concentration 37.488 105.25 106.75 105.45 107.85 2.40 9.75 12.15
Without retrogression and concentration 11.16 102.7 103.5 102.79 103.59 0.80 4.20 5.00
With retrogression and concentration 13.39 102.2 103.5 102.29 103.95 1.663 5.07 6.733
97.95
95.70
98.59
97.22
2.81 6.85
2.70 8.63
1.25 3.71
1.25 4.51
20.2
29.68
12.3
16.3
2.117
2.70
2.55
3.06
Without retrogression and concentration
2.2.2 Hydraulic jump calculations
Provide the D.S floor at elevation 95.65 m with horizontal length of 32 m
Page 64
Table (2):the water surface profile u.s of the jump
Distance from u.s end of crest
U.S.T.E.L = 107.848 m q= 37.488 cumec/m R .L of glacis
High flood
Ef1=U.S.T.E.LR.L of glacis 3.00 4.23 6.00 6.15 8.34 9.00 12.00 12.90 Page 65
99.00 98.59 98.00 97.95 97.22 97.00 96.00 95.70
8.848 9.259 9.848 9.898 10.629 10.848 11.848 12.148
U.S.T.E.L=103.952 m q=13.396 cumec/m Pond flow
D1
3.76 3.50 3.31 3.25 3.10 3.00 2.76 2.60
Ef1=U.S.T.E.LR.L of glacis 4.952 5.363 5.952 6.002 6.733 6.952 7.952 8.252
D1
1.75 1.70 1.45 1.40 1.35 1.30 1.15 1.10
Page 66
Table (3): the water surface profile d.s the jump SL No .
1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 Page 67 16
𝑋 𝐷1 1 2 4 6 8 10 11.88 12 14 16 18 20 22 24 25.6 26.4
High Flood Condition Fr=2.698, Fr²=7.279, D1=2.7 m 𝒀 𝑫𝟏 1.3 1.70 2.40 2.7 2.9 3.09 3.21
X
Y
2.7 5.4 10.8 16.2 21.6 27 32
3.51 4.6 6.48 7.28 7.83 8.34 8.66
Pond Flow Condition Fr=3.061, Fr²=9.37, D1=1.25 m 𝒀 𝑫𝟏 1.3 1.70 2.40 2.75 3.10 3.40 3.6 3.65 3.85 3.90 3.95 4.00 4.00 4.00 4.00 4.00
X 1.25 2.5 5.0 7.5 10.0 12.5 14.8 15.0 17.5 20.0 22.5 25 27.5 30 32 33
Y 1.625 2.125 3.00 3.44 3.875 4.25 4.50 4.56 4.81 4.88 4.94 5.00 5.00 5.00 5.00 5.00
Page 68
2.2.3 Depth of sheet pile lines from scour condition
Ι. Depth of scour Total discharge passing through under sluice =1856.87 cumec Under sluice over all water way = 75 m q =average discharge =
1856.87 75
=24.758 m²/sec
1/3 = 11.468 m R (depth of scour) = 1.35(𝑞² ) 𝑓
Page 69
II. U.S sheet pile
On the U.S side allow
1.1R = 1.1 ×11.468 = 12.615 m
R.L of bottom of scour hole =106.75-12.615 = 94.135 m Provide sheet pile line at elevation 94 m Depth of U.S sheet pile = 100-94 = 6 m
Page 70
III. D.S sheet pile
On D.S sheet pile allow 1.25 R = 1.25×11.468 = 14.34 m R.L of bottom of scour hole =105.25-14.34 =90.91 m Provide D.S sheet pile line at elevation 90 m D.S sheet pile depth = 95.65 - 90 = 5.65 m
Page 71
2.2.4. Total floor length and exit gradient:
Safe exit gradient =
1 6
Maximum static head =103.5 – 95.65 =7.85 m Depth of D.S sheet pile = 95.65 – 90.0 = 5.65 m 𝐻 1 1 7.85 1 𝐺𝐸 = , = 𝑑𝜋 𝜆
6
5.65 𝜋 𝜆
λ=7.704, 𝛼 = [ 2𝜆 − 1
Page 72
2
− 1]½=13.0437
b = 𝛼𝑑
b = 13.0437 ×5.65 = 73.697 m provide D.S sheet pile = 6 m λ = 6.243, 𝛼 = 11.44 𝑚 b = 6.243 × 11.44 = 68.64 m provide total floor length = 69 m provide D.S sheet pile line at elevation 89.65 m
Page 73
Floor length should be distributed as following:
D.S horizontal floor =32 m D.S glacis length =3(100- 95.65) =13.05 m The balance should be provided as U.S floor = 23.95 m Total length = 69 m
Page 74
Assume U.S floor thickness 1.0 m and D.S floor thickness 1.5 m
I. Upstream pile line: d =100 – 94 = 6 m 1 𝛼
=
𝑑 𝑏
=
6 69
=0.084
∅𝐷1 = 100% − ∅% , ∅𝐷 = 18% ∅𝐷1 = 82% ∅𝐶1 = 100% − ∅𝐸% , ∅𝐸 = 27% ∅𝐶1 = 73%
Page 75
Correction of Thickness: 𝑡 𝑑
Ct = (∅𝐷1 − ∅𝐶1 ) 1 6
= (82%-73%) = 1.5%
Page 76
Correction of Interference of Piles:
D =(100 – 1) – 89.65 = 9.35 m d =(100 - 1) - 94 =5 m b'=69 – 0.5 – 0.5 =68 m 𝐷 𝐷:𝑑 ) 𝑏′ 𝑏
cp =19√ (
9.35 9.35:5 =19√ ( ) 68 69
= 1.465٪
Corrected ∅𝐶1 =73% +1.5% +1.465% =75.965% Page 77
II. D.S pile line
Depth of d.s sheet pile = 6 m 1 ∝
𝑑 𝑏
= =
6 69
=0.08695~ 0.087
∅𝐸 = 27٪ , ∅𝐷 = 18٪ Correction of thickness: 𝑡 𝑑
ct = - (∅𝐸 − ∅𝐷) =-
Page 78
1.5 ( 6
27 – 18 ) = - 2.25٪
Correction of interference:
d =(95.65 – 1.5 ) – 89.65 =4.5 m D =(95.65 – 1.5 ) – 94 =0.15 m 0.15 0.15:4.5 ( )= 68 69
Cp = - 19 √
- 0.06 ٪
Correction of ∅𝐸 = 27 − 2.25 – 0.06 =24.69٪
Page 79
condition D.S water level datum (m) 1 No flow maximu m static head High Flood
Flow at pond level
Page 80
U.S water level datum (m)
H
2
3
4
95.65
103.5
7.85
105.25
106.75
102.289 103.5
𝑒𝑖𝑔𝑡 Of sub Soil H. 𝑒𝑙𝑒𝑣𝑎𝑡𝑖𝑜𝑛 U.S Pile line
G line
above
datum
D.S Pile line
∅𝐸 100٪ 5 7.85
∅𝐷1 82٪ 6 6.437
∅𝐶1 ∅𝐸 75.965٪ 24.69٪ 7 8 5.963 1.938
∅𝐷 18٪ 9 1.413
∅𝐶 0 10 0
103.5 1.5
102.087 1.23
101.613 97.582 1.14 0.3704
97.063 0.27
95.65 0
106.75 1.211
106.48 0.9930
106.39 0.9199
105.52 0.2180
105.25 0
103.5
103.282
103.210 102.588
1.5 105.620 0.2990
1.211 102.507 102.289
1. down stream floor thickness : Distance from D.S end
Page 81
Static head (m)
3
2.0860
6 9 12 15 18 21 24 27 30 32
2.2636 2.4411 2.6187 2.7963 2.9738 3.1514 3.3290 3.5066 3.6841 3.8025
Dynamic head (m)
Minimum thickness from calculation 2 1.68 1.6* =1.067 3 1.33 1.83 1.467 1.97 1.87 2.11 2 2.26 2.267 2.40 2.67 2.54 3.267 2.68 4.0 3.22 4.867 3.92 5.13 4.13
Provided thickness
1.70 1.90 2.00 2.2 2.40 2.5 2.70 2.80 3.3 4.0 4.2
Provide 4.0 m of floor thickness extend by 3 m inside beyond the toe of glacis. 2.U.S floor thickness: The floor thickness is required however minimum thickness of shall be provided.
Page 82
1m
Ι. Upstream protection
a) Block protection R = 11.467 m Provide 1.5 R = 1.5×11.467 =17.20 m R.L of bottom of scour hole =106.75 – 17.2 =89.55 m Scour depth below U.S floor = 100 – 89.55 = 10.45 m say 11 m Volume of block = D m³/m = 11m³/m Provide 1.6m × 1.6m ×1.0m c/c block over 0.4 m thick graded filter.
Length Page 83
11 = 1:0.4
= 7.857 m
Provide 5 row of c/c block in a length of 8 m
Ι. Upstream protection (continued)
b) Launching apron provide 2.25 D m³/m = 2.25 * 11 =24.75 m³/m Length =
24.75 1.4
= 17.67857 m
Provide launching apron of a length of 18 m and 1.4 m thickness.
Page 84
II. Down stream protection
Anticipated scour depth = 2 R = 2 ×11.467 = 22.934 m R.L of bottom scour hole = 105.25 – 22.934 = 82.316 m Depth of scour hole below D.S floor = 95.65 – 82.316 = 13.334 m Say 13.4 m
Page 85
II. Down stream protection (continued)
a) Block protection Length = 1.0 D = 1.0 × 13.4 = 13.4 m Provide 1.6 × 1.6 × 1.0 c/c block with 10 cm gaps filled with bajri over 1.0 m thick graded filter . No. of rows required =13.4/(1+1) = 6.7 m Provide 7 rows of blocks in a length of 11.9 m
Page 86
II. Down stream protection (continued)
b) Launching apron Thickness of launching apron = 2.0 m Length of launching apron =
2.25×13.4 2
=15.0075 m
Provide 20 m length of launching apron in the downstream.
Page 87
Page 88
Page 89
I) High flood level
i) Without concentration and retrogression U.S.W.L = 105.75 + 1 = 106.75 m U.S.T.E.L = 106.75 + 0.2 = 106.95 m Head over other barrage crest = 106.95 – 101.25 = 5.7 m q =C.H3/2 = 1.84 (5.7)3/2 =25.04 m D.S.W.L = 105.75 m D.S.T.E.L =105.75 + 0.2 = 105.95 m HL = 106.95 – 105.95 = 1 m
Page 90
I) High flood level
ii) with 20٪ concentration and 0.5 m retrogression q =1.2 × 25.04 = 𝑞 𝑐
H =( )2/3 =(
30.048 2/3 ) = 1.84
30.048 cumecs/m 6.43673 m
U.S.T.E.L
101.25 + 6.437 =107.687 m
D.S.W.L
105.75 – 0.5 = 105.25 m
D.S.T.E.L
105.25 +0.2 = 105.45 m
HL = 107.687 – 105.45 =2.237 m
Page 91
II. Pond flow condition
i)With out concentration and retrogression: head over under sluice crest = 103.5 – 100 = 3.5 m head over other barrage crest = 103.5 – 101.25 = 2.25 m Q =1.705 (65 – 0.1 × 8 × 3.5 ) × 3.5 + 1.84 (300 – 0.1 × 58 × 2.25) × 2.253/2 = 694.41 + 1781.9595 =2476.369 cumecs q
Page 92
2476.369 = 436
= 5.679 m²/sec ~ 5.68
i)With out concentration and retrogression (continued):
R= 1.35 V
𝑞 = 𝑅
hv
Page 93
5.68² 1/3 ( ) 1
5.68 = 4.297
𝑉² = 2𝑔
= 4.297
=1.32 m/sec
=0.089 m
i)With out concentration and retrogression (continued):
U.S.T.E.L =103.5 +0.089 = 103.589 m D.S water level when flood discharge of 2476.369 cumecs is passing =102.7 m ,for stage discharge curve
D.S.T.E.L = 102.7 + 0.089 =102.789 m HL =103.589 – 102.789 = 0.80 m q =1.84 (2.25)^1.5 = 6.21 cumecs/m
Page 94
ii) with 20٪ concentration and 0.5 retrogression
q = 1.2 * 6.21 = 7.452 cumecs/sec H=(
7.452 2 )^ 1.84 3
=2.54 m
U. S.T.E.L =101.25 + 2.54 = 103.79 m D.S.W.L = 102.7 – 0.5 = 102.2 m
D.S.T.E.L =102.2 +0.089 = 102.289 m HL = 103.79 – 102.289 = 1.501 m
Page 95
High No.
1 2 3 4 5 6 7 8 9
Discharge q D.S.W.L U.S.W.L D.S.T.E.L U.S.T.E.L HL Ef2 Ef1 =Ef2+HL
10 11 12
D1 D2 Length of floor 5(D2 - D1) 𝑞 F=
13
Page 96
Item
Level at which jump occurs
√𝑔𝐷1³
Flood
Pond
Flow
Without concentration and retrogression
With concentration and retrogression
Without concentration and retrogression
With concentration and retrogression
25.04 105.75 106.75 105.95 106.95 1 7.0 8.0 98.95
30.048 105.25 106.75 105.45 107.687 2.237 8.43 10.667 97.02
6.21 102.7 103.5 102.789 103.589 0.80 3.0 3.8 99.778
7.54 102.2 103.5 102.289 103.79 1.501 3.506 5.007 98.78
2.25 6.06 19.05
2.28 7.45 25.85
0.81 2.66 9.237
0.81 3.18 11.85
2.369
2.786
2.72
3.302
Provide the downstream floor at elevation 96.8 m with horizontal length of 27 m .
Distance from R.L of U.S end glacis of crest
0.75 3 3.75 6.0 6.75 9 9.75 12 12.69
Page 97
100.25 100 99.25 99 98.25 98 97.25 97.02
U.S.T.E.L=107.687 q =30.048 U.S.T.E.L= 103.79 cumecs/m q =7.54 cumecs / m High flood Pond flow Ef1 =U.S.T.E.L – Ef1=U.S.T.E.L R.L of glacis – R.L of glacis D1 D1 7.437 7.687 8.437 8.687 9.437 9.687 10.437 10.667
3.4375 3.218 2.844 2.75 2.560 2.50 2.344 2.281
2.79 3.54 3.79 4.54 4.79 5.54
1.5625 1.125 1.06 0.906 0.84375 0.78125
Page 98
Sl No.
𝑋 𝐷1
High Fr=2.78 𝑦 𝐷1 1 1 1.3 2 2 1.67 3 4 2.286 4 6 2.71 5 8 3.0 6 10 3.19 7 12 3.286 8 12.28 3.3 9 14 10 16 11 18 12 20
Page 99
flood Condition Pond Fr²=7.76 D1=2.28m Fr=3.302 𝑌 X Y 𝐷1 2.28 2.964 1.3 4.56 3.8070 2.714 9.12 5.212 2.38 13.68 6.179 2.86 18.24 6.84 3.143 22.8 7.27 3.524 27.36 7.49 3.62 28 7.524 3.64 3.86 4.0 4.095 4.19
Flow Condition Fr²=10.9 D1=0.81m X Y 0.81 1.62 3.24 4.86 6.48 8.1 9.72 9.947 11.34 12.96 14.58 16.2
1.053 1.39 1.93 2.316 2.546 2.85 2.93 2.95 3.126 3.24 3.317 3.4
Page 100
Ι. Depth of scour
Total discharge passing through other barrage =6684.1 cumecs Other barrage over all water way =358 m q=
6684.1 358
= 18.6706 cumecs/m
𝑞² 𝑓
R =1.35( )1/3 = 9.5 m
Page 101
II. U.S sheet pile
Allow 1.1 R = 1.1 × 9.5 = 10.45 m R.L of the bottom of scour hole = 106.75 – 10.45 = 96.3 m Provide sheet pile lines at elevation 96 m Depth of U.S sheet pile = 100 – 96 = 4 m
Page 102
III. D.S sheet pile :
Allow 1.25 R = 1.25 × 9.5 = 11.675 m R.L of bottom of scour = 105.25 – 11.875 = 93.375 m Provide sheet pile lines at elevation 92 m
Page 103
1 6
Safe exit gradient = max. static head = 103.5 – 96.8 = 6.8 m Depth of D.S cut off = 96.8 – 92 = 4.8 m GE = 1 6
=
𝐻 1 𝑑 𝜋 𝜆
6.8 1 4.8 𝜋 𝜆
𝛼 =
, λ = 7.32
2𝜆 − 1
2
− 1 ½ = 13.6
b = 𝛼𝑑 = 13.6 × 4.8 =65.28 m say 66 m provide floor length = 66 m
Page 104
The floor length is distributed as follows:
down stream horizontal floor =27 m down stream glacis length = 3(101.25 – 96.8) = 13.35 m width of crest = 2 m Upstream glacis length = 22.4 m Total floor length = 66 m
Page 105
Assume up stream floor thickness 1.0 m and down stream floor thickness 1.5 m Ι. Upstream pile line d = 100 – 96 = 4 m 1 ∝
𝑑 𝑏
= =
4 66
= 0.0606
∅𝐷1 = 100 − ∅𝐷 ,
∅𝐷 = 15٪
= 100 – 15 = 85٪ ∅𝐶1 = 100 − ∅𝐸 , ∅𝐸 = 22 ٪ = 100 – 22 = 78 ٪
Page 106
Correction of thickness : 𝑡 𝑑
Ct = (∅𝐷1 − ∅𝐶1) 1 4
= (85 – 78 ) = 1.75 ٪
Correction of interference : Cp =
𝐷 𝑑:𝐷 19√ ( ) 𝑏` 𝑏
= 19√
7 3:7 ( ) 65 66
= 0.945 ٪
Corrected ∅𝐶 = 78 + 1.75 + 0.945 = 80.695 ٪
Page 107
II. Down stream sheet pile lines 1 ∝
𝑑 𝑏
= =
4.8 66
= 0.0727
∅𝐷 = 16٪
,
∅𝐸 = 24 ٪
Correction of thickness : 𝑡 𝑑
Ct = - (∅𝐸 − ∅𝐷) =-
1.5 4.8
(24 – 16) = - 2.5 ٪
Corrected ∅𝐸 = 24 − 2.5 = 21.5٪ Correction of interference: There is no correction of pile interference . Page 108
Condition
1 No flow max. static head High Flood Flow at pond level
Page 109
Height/Elevation of sub soil H.G. line above datum
D.S water level datum (m)
U.S water level datum (m)
H
2
3
4
96.8
103.5
6.7
U.S Pile Line
D.S Pile Line
∅𝑬𝟏 100
∅𝑫𝟏 85
∅𝑪𝟏 80.695
∅𝑬 21.5
∅𝑫 16
∅𝑪 0
5
6
7
8
9
10
5.695
5.4065
1.4405
1.072
0
102.495
102.2065
98.2405
97.872
96.8
1.275
1.21
0.3225
0.24
0
106.525 1.105
106.46 1.049
105.5725 0.2795
105.49 0.208
105.25 0
103.305
103.249
102.4795
102.408
102.2
6.7
105.25
106.75
1.5
1.5
102.2
103.5
1.3
1.3