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BFC21103 Hydraulics
Chapter 3. Specific Energy and Control Section
Tan Lai Wai, Wan Afnizan & Zarina Md [email protected]
Updated: September 2014
Learning Outcomes
At the end of this chapter, students should be able to:
i. Apply specific energy concept in determining critical flow conditions
ii. Analyse flow over broad‐crested weir
iii. Analyse flow through width constriction
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Specific energy (introduced by Bakhmeteff) is the energy of flow measured with respect to the channel bottom.
Bottom slope So
Datum
θ
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1.1 Concept of Specific Energy
gV
yE2
2
+=
Energy line slope Sf
1 2
Water surface or hydraulic grade line slope Sw
2z
2y
fh
gV2
22
gV2
21
1y
1z
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For constant Q, 2
2
2gAQ
yE +=
The concept of specific energy is useful in defining critical depth and in the analysis of flow problems.
Variation of E with y is represented by a cubic parabola,
E = y
45°E
y
subcritical, Fr < 1
supercritical, Fr > 1critical, Fr = 1
Emin E1= E2
y1
y2
gV2
21
gV2
22
ysuper
yc
ysub
y1y2
yc
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For a specific E (except Emin), there are two flow depths y1 and y2, i.e.
Subcritical y
Supercritical yAlternate depths
If there is energy loss, e.g. during hydraulic jump, y1 and y2 are known as conjugate (or sequent) depths
Critical flow occurs when specific energy is minimum, Emin with yc = critical depth
Note: Negative flow depth is not possible.
1.2 Alternate Depths and Critical Depth
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At minimum specific energy Emin, y = yc and A = Ac
Specific energy 2
2
2gAQ
yE +=
yA
gAQ
yE
dd
1dd
3
2
−=
cc
TgAQ
3
2
10 −=
yA
Tdd
=
12
2
=cc
c
AgATQ
dydA
12
=c
c
gDV
1=c
c
gDV
1Fr =
Differentiating
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Since
Specific Energy of Flow in Rectangular Section
qBQ = 2
2
2gyq
yE +=
Rearranging ( )yEgyq −= 22
Variation of q with y is represented by the following curve,
yc
ysub
y1
y2
yc
subcritical, Fr < 1
supercritical, Fr > 1
critical, Fr = 1
ysuper
q
y
qmaxq1= q2
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For a specific q (except qmax), there are two flow depths y1 and y2, i.e.
Subcritical y
Supercritical yConjugate depths
Critical flow occurs when discharge per unit width is maximum, i.e. qmax
Keeping E constant,
( )yEgAQ −= 2
( )( )yEggA
yEgyA
yQ
−−−=
22
dd
dd
12
2
=cc
c
AgATQ
1Fr =
QgA
AQ
T c
cc
2
0 −=
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State of flow can be established by comparing yo with yc.
Characteristics Flow condition
Fr = 1yo = yc
Critical flow
Fr < 1yo > yc
Subcritical flow
Fr > 1yo < yc
Supercritical flow
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Activity 3.1
The rate of flow in a 3‐m wide rectangular channel is 10 m3/s. Calculate the specific energy if the depth of flow is
(a) 3 m; and
(b) 1.2 m.
Given Q = 10 m3/s and B = 3 m.
When y = 3 m, m 063.33381.92
103
2 22
2
2
2
=×××
+=+=gAQ
yE
When y = 1.2 m, m 593.12.1381.92
102.1
2 22
2
2
2
=×××
+=+=gAQ
yE
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1.3 Calculation of Critical Depth
Critical depth can be determined by:
i. Trial and error; or
ii. Graphically
1.3.1 Critical Depth from Trial‐and‐Error
For all channel sections, during critical flow (Emin)
13
2
=c
c
gATQ
gQ
TA
c
c23
=Rewritten as a function of critical depth,
is usually provided
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For rectangular channel, T = B and A = By
becomes
gQ
TA
c
c23
=
gQ
ByB c
233
=
gBQ
yc 2
23 =
Since BQ
q = 3
2
gq
yc = (only applies to rectangular channel)
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Critical depth also occurs when q is maximum
( )yEgyq −= 22
( )yEgyq −= 22 2
Differentiating q with respect to y
( )cc yEgyyq
q 322dd
2 min −=
032 min =− cyE0dd
=yq
gives
cyE23
min = (only applies to rectangular channel)
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Critical slope Sc is used to categorize the type of channel slope
Condition of So Type of slopeSo = Sc Critical slope
So < Sc Mild slope
So > Sc Steep slope
Critical slope Sc can be calculated by equating Manning resistance flow equation to critical flow condition
21
323 1
cccc
c SRAnT
gAQ ==At critical slope, So = Sc
13
2
=c
c
gATQ
34
2
cc
cc
RT
gAnS =
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Activity 3.2
A 4.0 m wide rectangular channel conveys water to a reservoir. If the discharge in the channel Q = 25 m3/s and Manning coefficient n = 0.02, find
(a) Critical depth
(b) Critical velocity
(c) Critical slope
3
2
gq
yc =
Given Q = 25 m3/s, B = 4.0 m, n = 0.02
(a)
m 585.1481.9
253
2
2
=×
=cy
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1=c
c
gDV
(for rectangular section, T = B)
(b)
1=c
c
gyV
(for rectangular section, D = y)
m/s 943.3585.181.9 =×== cc gyV
(c)
007328.0
585.124585.14
585.181.902.0
34
2
=
⎟⎠⎞
⎜⎝⎛
×+×
××=cS
34
2
c
cc
R
gynS =
34
2
cc
cc
RT
gAnS =
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Activity 3.3
(a) An infinitely wide and straight river has a discharge of 5.0 m3/s/m.Calculate:(i) Critical depth(ii) Froude number of the flow when the flow depth is 6.0 m and
determine the type of flow(iii) Critical slope of the channel if Manning coefficient n = 0.0044.
(b) Based on the river characteristics given in (a), find the possible depth of flow y2 for the same specific energy and the corresponding Froude number.
Given q = 5.0 m3/s/m, y = 6.0 m, n = 0.0044, For infinitely wide channel R ≈ y
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(a) (i) m 366.181.95
3
2
3
2
===gq
yc
(a) (ii)
1086.0681.9
5Fr
33=
×===
gy
qgyV
For rectangular section, D = y
flow lsubcritica 11086.0Fr →<=
0001712.0366.1
81.90044.0
31
2
31
2
34
2
=×
===
cc
cc
y
gn
R
gynS
(a) (iii) For rectangular section, T = B
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(b) Specific energy at y1 = 6 m
m 035.6681.92
56
2 2
2
21
2
11 =××
+=+=gyq
yE
The alternate depth of y1 = 6 m with E2 = E1 = 6.035 m is
035.62 2
2
2
2 =+gyq
y
035.681.925
22
2
2 =××
+y
y
m 4789.02 =y
817.44789.081.9
5Fr
33=
×===
gy
qgyV
At y2 = 0.4789 m,
flow calsupercriti 1817.4Fr →>=
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Activity 3.4
For a trapezoidal channel with bottom width B = 6 m and side slope z = 2, find the critical flow depth if the discharge is 17 m3/s using trial‐and‐error method.
Given Q = 17 m3/s, B = 6 m, z = 2
z = 2y1
B = 6 m
Q = 17 m3/s
gQ
TA
c
c23
=
( )81.9
174626 232
=++
c
cc
yyy
( )365.7
233
32
=++
c
cc
yyy
m 8468.0=cyFrom trial‐and‐error,
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1.3.2 Graphical Method
Critical depth of flow yc can be solved by plotting y against ccc
c DATA
or 3
Activity 3.5
For a trapezoidal channel with bottom width B = 6 m and side slope z = 2, find the critical flow depth if the discharge is 17 m3/s graphically.
Given Q = 17 m3/s, B = 6 m, z = 2
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gQ
TA
c
c23
=
46.293
=c
c
TA
yc (m) Ac3/Tc
1 51.20
2 571.43
0.5 5.36
0.7 15.79
0.8 24.43
( )c
cc
c
c
yyy
TA
4626
323
++
=Also,
0
0.2
0.4
0.6
0.8
1
1.2
0 10 20 30 40 50 60c
c
TA3
yc (m)
29.46
0.84 m
m 84.0=cyFrom the graph,
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1.4 Control Sections
A control section is where for a given discharge Q, the flow depth yand velocity V are fixed.
The critical depth yc is also a control point since at this section Fr = 1, effective when subcritical flow changes to supercritical flow. When supercritical flow changes to subcritical flow, a hydraulic jumps usually bypass the critical depth as control point.
A control section 'controls' the upstream or downstream flow.
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Examples of control sections:
(a) Flow from a mild channel to steep channel
(b) A mild‐slope channel discharging into a pool
M2
S2yc
MildSteep
Drop
Pool
M2
yo
yo
yoyc
control control
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(c) Free overflow (sudden drop)
(d) Reservoir water flows on a steep slope
Horizontal bed
H2
yc
controlS2
yc
ReservoirSteep yo
control
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(e) Flow through sluice gate (f) Flow over spillway
M1
M3
ycMild
yo
control
M1
yc
control
control
Jump
Mild
yo
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(g) Flow over broad‐crested weir
(h) Flow through constricted channel width
ycH
Hump
control
yc
B
control
Plan view
Constriction
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1.5 Flow Over Broad‐Crested Weir
Flow in a prismatic open channel is uniform if there is no obstruction e.g. of a hydraulic structure.
If broad‐crested weir is installed, uniform flow changes to non‐uniform flow. Changes to the water surface profile is influenced by the weir height H and the flow condition before the weir (upstream flow), i.e. either supercritical or subcritical.
H
Weir
0 1 2 3
yo
yo = normal depth of flow
y1 = depth of flow just before weir
y2 = depth of flow on the weir
y3 = depth of flow just after weir
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Minimum Height of Weir Hmin
Height of weir H determines the depth of flow above the weir y2, i.e. whether y2 = yc or not.
Hmin = minimum height of weir which will start to produce critical flow depth above the weir (y2 starts to change to yc)
Generally, depth of flow above the weir y2 is
If H < Hmin → y2 ≠ yc
If H = Hmin → y2 = yc
If H > Hmin → y2 = yc
Therefore, y2 = yc and E2 = Emin if H ≥ Hmin
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Condition of upstream flow
yo
Case 1 Case 2 Case 3H y H y H y
Subcritical yo > yc
Supercritical yo < yc
H < Hminor
Emin + H < EoSubmerged
weir
y1 = y3 = yoy2 ≠ yc
E2 = Eo − H
H = Hminor
Emin + H = EoRarelyoccur
y1 = y3 = yoy2 = ycE2 = Emin
H > Hminor
Emin + H > EoControl weir
y1 ≠ y3 ≠ yoy1 = y1′y3 = y3′y2 = yc
E1,3 = Emin + HE2 = Emin
yo < y2 < yc
1 2 30H
y2
yo
yc
EoE2
yc < y2 < yo
1 2 30H
y2yo yc
EoE2
Eo
1 2 30
Hyo
y2=yc
E2 = Emin
1 2 30
H
yo y2=yc
E2 = Emin
Eo
1 2 30
Hyo
y2 = yc
E2 = Emin
Jump
Eo
y1′ > yc and y3′ < yo
yc y3
1 2 30
H
yo y2 = yc
E2 = Emin
Eo
y1′ > yo and y3′ < yc
yc y3
Backwater
y1
y1
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Steps in Analysing Flow Over Broad‐Crested Weir
1. Calculate yo and ycDetermine state of upstream flow yo, i.e. either subcritical or supercritical by comparing with yc.If yo > yc → subcritical upstreamIf yo < yc → supercritical upstream
2. Calculate HminBy comparing height of weir H with Hmin, the condition of flow over weir can be established, i.e.If H < Hmin → Case 1If H = Hmin → Case 2If H > Hmin → Case 3
3. Determine y1, y2 and y3.
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Case 1: H < Hmin
yo < y2 < yc
1 2 30H
y2
yo
yc
EoE2
Supercritical upstream yo < yc
E = y
E
y
Emin E2
y1,3 = yoy2yc
Eo
HHmin
yc < y2 < yo
1 2 30H
y2yo yc
EoE2
Subcritical upstream yo > yc
yc
E = y
E
y
Emin E2
y1 = y3 = yo
y2yc
EoH
Hmin
EGL
EGL
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For Case 1,
H < HminH < Eo − EminE1 = E3 = Eoy2 ≠ yc
StepsUseful equations
All sections Rectangular section
1. Calculate yo and yc
Manning: Manning:
2. Calculate Hmin
3. Determine y1, y2 & y3
y1 = y3 = yoE2 = Eo − H
21
o
32
S
QnAR =
gQ
TA
c
c23
= 3
2
gq
yc =
21
o
32
o
S
qnRy =
2
2
oo 2gAQ
yE += 2o
2
oo 2gyq
yE +=
cyE23
min =c
c gAQ
yE2
2
min +=
minomin EEH −=
222
2
2 2E
gAQ
y =+ 222
2
2 2E
gyq
y =+
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Case 2: H = Hmin
E = y
E
y
E2=Emin
y1,3 = yo
y2 = yc
Eo
H=Hmin
E = y
E
y
E2=Emin
y1 = y3 = yo
y2 = yc
Eo
H=Hmin
1 2 30
H
yo y2=yc
E2 = Emin
Eo
y2 = yc < yo
Subcritical upstream yo > yc
Eo
E2 = Emin
y2 = yc > yo
Supercritical upstream yo < yc
H
1 2 30
y2=yc
yo
EGL
EGL
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For Case 2,
H = HminHmin = Eo − EminE1 = E3 = EoE2 = Eminy2 = yc
StepsUseful equations
All sections Rectangular section
1. Calculate yo and yc
Manning: Manning:
2. Calculate Hmin
3. Determine y1, y2 & y3
y1 = y3 = yoy2 = yc
21
o
32
S
QnAR =
gQ
TA
c
c23
= 3
2
gq
yc =
21
o
32
o
S
qnRy =
2
2
oo 2gAQ
yE += 2o
2
oo 2gyq
yE +=
cyE23
min =c
c gAQ
yE2
2
min +=
minomin EEH −=
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E = y
E
y
E2=Emin
y2 = yc
E′1=E3Hmin
1 2 30
Hyo
E2 = Emin
JumpEo
y1′ > yc and y3′ < yo
yc y3
y1
y2 = yc < yoy′1 > yoy′3 < yc
Subcritical upstream yo > yc
y2 = yc > yoy′1 > yoy′3 > yc
Supercritical upstream yo < yc
EGL y1 = y1′ ≠ yo
y3 ≠ yo
E = y
E
y
E2=Emin
y1 = y1′ ≠ yo
y2 = yc
Eo
H>Hmin
1 2 30
H
yo y2 = yc
E2 = Emin
Eo
y1′ > yo and y3′ < yc
yc y3
Backwater
y1
EGL
y3 ≠ yo
Hmin
E′1,3
yo
yo
Eo
H>Hmin
y2 = yc
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For Case 3,
H > HminH > Eo − EminE′1 = E′3 ≠ Eoy2 = yc
StepsUseful equations
All sections Rectangular section
1. Calculate yo and yc
Manning: Manning:
2. Calculate Hmin
3. Determine y1, y2 & y3
y′1 ≠ y′3 ≠ yoE′1,3 = Emin + H
3
2
gq
yc =
21
o
32
o
S
qnRy =
2o
2
oo 2gyq
yE +=
cyE23
min =
minomin EEH −=
3,123,1
2
1,3 2E
AgQ
y ′=′
+′3,12
1,3
2
1,3 2E
ygq
y ′=′
+′
gQ
TA
c
c23
=
2
2
oo 2gAQ
yE +=
cc gA
QyE
2
2
min +=
21
o
32
S
QnAR =
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Activity 3.6
10 m3/s of flow is conveyed in a rectangular channel of 4 m width, n= 0.015 and So = 0.0075. If a weir with height 0.92 m is built in the channel, determine the depth of flow on the weir.
Given Q = 10 m3/s, B = 4 m, n = 0.015, So = 0.0075, and H = 0.92 m
B
y
Step 1. Determine yo and yc
21
o
32
o
S
qnRy =
21
32
o
oo
0075.0
015.0410
244
×⎟⎠⎞
⎜⎝⎛
=⎟⎟⎠
⎞⎜⎜⎝
⎛+ yy
y
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m 8605.081.9410
3
2
3
2
=⎟⎠⎞
⎜⎝⎛
==gq
yc
4330.024
4 32
o
oo =⎟⎟
⎠
⎞⎜⎜⎝
⎛+ yy
y
m 6804.0o =y
yo < yc → supercritical flow
m 369.16804.081.92
410
6804.02 2
2
2o
2
oo =××
⎟⎠⎞
⎜⎝⎛
+=+=gyq
yE
m 291.18605.023
23
min =×== cyE
Step 2. Calculate Hmin
m 078.0291.1369.1minomin =−=−= EEH
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Step 3. Determine y2
Since H = 0.92 m > Hmin = 0.078 m → Case 3 Hydraulic jump &y2 = yc = 0.8605 m
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Activity 3.7
A rectangular channel conveys flow at yo = 1.6 m and R = 0.77 on So = 1/3000 and Manning n = 0.01.
(a) What is the minimum height of weir to control the flow in the channel?
(b) Calculate depth of flow upstream, downstream and above the weir in (a).
(c) Calculate depth of flow upstream, downstream and above the weir if the height of weir is(i) 0.4 m, and(ii) 0.6 m.
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Given yo = 1.6 m, R = 0.77, So = 1/3000, n = 0.01
(a) Step 1. Determine yo and yc
m 8499.081.9454.2
3
2
3
2
===gq
yc
m 6.1o =y
yo > yc → subcritical flow
/s/mm 454.230001
77.06.101.011 32
1
32
21
o32
o =⎟⎠⎞
⎜⎝⎛×××== SRy
nq
m 720.16.181.92
454.26.1
2 2
2
2o
2
oo =××
+=+=gyq
yE
m 275.18499.023
23
min =×== cyE
Step 2. Calculate Hmin
m 445.0275.1720.1minomin =−=−= EEH
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(b)
In (a), H = Hmin → Case 2.
For Case 2, y1 = y3 = yo = 1.6 my2 = yc = 0.8499 m
(c) (i) If H = 0.4 m < Hmin = 0.445 m → Case 1
For Case 1, y1 = y3 = yo = 1.6 m
E2 = Eo − H = 1.72 − 0.4 = 1.32 m
Step 3. Determine y1, y2 & y3.
222
2
2 2E
gyq
y =+
32.181.92
454.222
2
2 =×
+y
y
Since yo is subcritical, yo > y2 > yc, y2 = 1.032 m
Through trial‐and‐error, y2 = 1.032 m or y2 = 0.7085 m
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(c) (ii) If H = 0.6 m > Hmin = 0.445 m → Case 3: Backwater
For Case 3, y2 = yc = 0.8499 m
Through trial‐and‐error, y′1 = 1.778 m and y′3 = 0.4669 m
since y′1 > yo and y′3 < yc
3,121,3
2
1,3 2E
ygq
y ′=′
+′
m 875.16.0275.1min3,1 =+=+=′ HEE
875.181.92454.2
21,3
2
1,3 =′×
+′y
y
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1.6 Flow Through Constricted ChannelIf width of a prismatic channel is reduced/enlarged at a section, uniform flow changes to non‐uniform flow. Changes to the water surface profile is influenced by the width of constriction B2 and the flow condition before the constriction, i.e. either supercritical or subcritical.
B2q
B
1 2 30
q2
Plan view
2o
2o
2gyq
22
22
2gyq
q2q
1 2 30
EGL
y1 y3y2yo
q
y
qmaxqo
yoy2yc
q2
min32Eyc =
y
E
Side viewyoy2
qoq2
322
2
2 gBQ
yc =
Since B2 < Bo, q2 > qo
21
21
2
1
21
11 22 ygBQ
yg
VyE +=+=
22
22
2
2
22
22 22 ygBQ
yg
VyE +=+=
Bed elevations at 1 and 2 are the same, E1 = E2
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Maximum Width of Constriction Bmax
Width of constriction B2 determines the depth of flow at the constricted section y2, i.e. whether y2 = yc2 or not.
Bmax = maximum width of constriction which will start to produce critical flow depth at the constriction (y2 starts to change to yc2)
yco or yc1 = critical depth of flow along the unconstricted section
yc2 = critical depth of flow at the constricted section.
Generally, depth of flow at constriction y2 is
If B2 > Bmax → y2 ≠ yc2
If B2 = Bmax → y2 = yc2
If B2 < Bmax → y2 = y′c2> yc2Therefore, y2 = yc2 or y′c2 and E2 = Emin if B2 ≤ Bmax
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Condition of upstream flow
yo
Case 1 Case 2 Case 3B y B y B y
Subcritical yo > yco
Supercritical yo < yco
B2 > Bmaxor
Emin 2 < Eoor
q < qmax
y1 = y3 = yoy2 ≠ yc2E2 = Eo
B2 = Bmaxor
Emin 2 = Eoor
q = qmax
y1 = y3 = yoy2 = yc2
E2 = Emin 2 = Eo
B2 < Bmaxor
Emin 2 > Eoor
q > qmaxControl constriction
y1 ≠ y3 ≠ yoy1 = y1′y3 = y3′y2 = yc2
E1,3 = E'min 2 ≠ EoE2 = E'min 2
yo < y2 < yc2
1 2 30yo
EoE2 = Eo
yc2 < y2 < yo
1 2 30
yoEo
E2 = Eo
Eo
1 2 30yo
E2 = Emin 2 = Eo
1 2 30
yo
E2 = Emin 2 = Eo
Eo
ycoy2 yc2
yco y2 yc2
ycoy2=yc2
y2=yc2yco
1 2 30
yo
E2 = E′min 2
Eo
y1′ > yo and y3′ < yc2
yco y3
Backwater
y1y2=yc2
yo1 2 30
E2 = E′min 2
Jump
Eo
y1′ > yc2 and y3′ < yo
yco y3
y1y2=yc2
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Steps in Analysing Flow Through Constriction
1. Calculate yo and ycoDetermine state of upstream flow yo, i.e. either subcritical or supercritical by comparing with yco.If yo > yco → subcritical upstreamIf yo < yco → supercritical upstream
2. Calculate yc2, qmax and BmaxWhen width of a channel is being constricted, yc2 can be obtained since Emin = Eo. Once Bmax is calculated, the condition of flow through the constriction can be established, i.e.If B2 > Bmax → Case 1If B2 = Bmax → Case 2If B2 < Bmax → Case 3
3. Determine y1, y2 and y3.
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Case 1: B2 > Bmax
yo < y2 < yc2
Supercritical upstream yo < yco
yc2 < y2 < yo
Subcritical upstream yo > yco
E = y
E
y
EminoEmin 2
y1 = y3 = yoy2
yco
Eo=E1=E2=E31 2 30
y2yo
yc2
EoE2
yco
EGL
yc2B2 or q2B or qo
E = y
E
y
Emino Emin 2
y1 = y3 = yo
y2yco
Eo=E1=E2=E3
yc2B2 or q2B or qo
1 2 30yo
EoE2
EGL
ycoyc2
y2
Bmax or qmax
Bmax or qmax
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For Case 1,
B2 > BmaxEmin 2 < EoE2 = Eoy2 ≠ yc2
Steps Useful equations
1. Calculate yo and yco
Manning: or
2. Calculate yc2, qmax and Bmax
3. Determine y1, y2 & y3
y1 = y3 = yoE2 = Eo
21
o
32
S
QnAR =
3
2
o gq
yc =
21
o
32
o
S
qnRy =
;2 2
o
2
oo gyq
yE += 2min 23
cyE =
222
2
2 2E
gyq
y =+
;3
2max
2 gq
yc =max
max BQ
q =
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Case 2: B2 = Bmax
y2 = yc2 > yo
Supercritical upstream yo < yco
y2 = yc2 < yo
Subcritical upstream yo > yco
E = y
E
y
Emino
y1 = y3 = yo
yco
Emin 2 = Eo1 2 30
yoy2=yc2
Eo
yco
EGL
y2 = yc2
B or qo
E = y
E
y
Emino
y1 = y3 = yo
yco
Emin 2 = Eo
y2 = yc2
B or qo1 2 30
yo
EoE2
EGL
yco y2 =yc2
Bmax or qmax
Bmax or qmax
E2
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For Case 2,
B2 = BmaxEmin 2 = EoE2 = Emin 2 = Eoy2 = yc2
Steps Useful equations
1. Calculate yo and yco
Manning: or
2. Calculate yc2, qmax and Bmax
3. Determine y1, y2 & y3
y1 = y3 = yoy2 = yc2
21
o
32
S
QnAR =
3
2
o gq
yc =
21
o
32
o
S
qnRy =
;2 2
o
2
oo gyq
yE += 2min 23
cyE =
;3
2max
2 gq
yc =max
max BQ
q =
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Case 3: B2 < Bmax
y2 = yc2 > yo
Supercritical upstream yo < yco
y2 = yc2 < yo
Subcritical upstream yo > yco
E = y
E
y
Emino
yo
yco
Emin 21 2 30
yoEo
yco
EGL
y2 = y′c2
B or qo
E = y
E
y
Emino
y′3
yco
Emin 2
y2 = y′c2
B or qo1 2 30
yo
Eo
E2=E′min
EGL
ycoy′c2
Bmax
Bmax or qmax
E2=E′min
B2<Bmax
y′3y′c2 y′3
E′min 2
y′1
yc2y′1
yoy′3
y′1
Jump
Backwater
y′1
B2<Bmax
E′min 2
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For Case 3,
B2 < BmaxE′min 2 ≠ EoE2 = E′min 2y2 = y′c2
Steps Useful equations
1. Calculate yo and yco
Manning: or
2. Calculate yc2, qmax and Bmax
3. Determine y1, y2 & y3
y1 = y3 ≠ yo ; y2 = y′c2
21
o
32
S
QnAR =
3
2
o gq
yc =
21
o
32
o
S
qnRy =
;2 2
o
2
oo gyq
yE += 2min 23
cyE =
;3
2max
2 gq
yc =max
max BQ
q =
;2
max BQ
q =′
21,3
2max
1,31,3 2 ygq
yE′
′+′=′
3
2max
2 gq
yc′
=′
;23
2min cyE ′=′
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Activity 3.8
A bridge is to be built across a 50‐m wide rectangular channel carrying flow of 200 m3/s at depth 4.0 m. For reducing the span of the bridge, what is the minimum width of channel such that the upstream water level will not be influenced by the constriction?
Given Q = 200 m3/s, yo = 4 m, B = 50 m
Step 1. Determine yo and yco
m 177.181.94
3
2
3
2
o ===gq
yc
m 0.4o =y
yo > yco → subcritical flow
/s/mm 0.450200 3
o ===BQ
q
yc is influenced by q. When q changes, yc varies as well. Therefore, at constriction where q ≠ qo, yc2 exists (calculated in Step 2).
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Step 2. Calculate yc2 and Bmax
m 051.4481.92
44
2 2
2
2o
2o
2
oo =××
+=+=ygB
QyE
m 701.2051.432
32
min2 =×== Eyc
3
2max
2 gq
yc =
m 39.149.13
200
maxmax
maxmax ===→=
BBQ
q
With no energly loss, Emin = Eo, therefore
At width Bmax, E2 = Emin and q2 = qmax
Also,
/sm 90.13701.281.9 2332max =×== cgyq
rearranging gives
Since
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Activity 3.9
A bridge is to be built across a 50‐m wide rectangular channel carrying flow of 200 m3/s at depth 4.0 m. The construction has caused the width of the channel to be reduced to 30‐m. Determine the depth of flow upstream, downstream and under the bridge.
Given Q = 200 m3/s, yo = 4 m, B = 50 m
Step 1. Determine yo and yco (similar to the solution in Activity 3.8)
m 177.181.94
3
2
3
2
o ===gq
yc
m 0.4o =y
yo > yco → subcritical flow
/s/mm 0.450200 3
o ===BQ
q
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Step 2. Calculate yc2 and Bmax (similar to solution in Activity 3.8)
m 051.4481.92
44
2 2
2
2o
2o
2
oo =××
+=+=ygB
QyE
m 701.2051.432
32
min2 =×== Eyc
3
2max
2 gq
yc =
m 39.149.13
200
maxmax
maxmax ===→=
BBQ
q
With no energly loss, Emin = Eo, therefore
At width Bmax, E2 = Emin and q2 = qmax
Also,
/sm 90.13701.281.9 2332max =×== cgyq
rearranging gives
Since
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Step 3. Determine y1, y2 and y3
m 051.4o2 == EE
Since B2 = 30 m > Bmax = 14.39 m → Case 1
At B2 = 30 m,
222
22
2
2 2E
ygBQ
y =+
051.43081.92
20022
2
2
2 =×××
+y
y
From trial‐and‐error, y2 = 0.8399 m or y2 = 3.902 m
Since yo > yco, thus yc2 < y2 < yo. Therefore, y2 = 3.902 m
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Activity 3.10
A rectangular channel of 2.0 m width is required to convey 3 m3/s of flow. The normal depth is 0.8 m. At downstream of the channel, the width of the channel is to be reduced.
(a) Determine the width of the maximum constriction for critical depth to occur.
(b) Calculate the depth of flow upstream, downstream and at the constriction if the constricted width is 1.2 m.
Given Q = 3 m3/s, B = 2.0 m, yo = 0.8 m
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(a) Step 1. Determine yo and yco
m 6121.081.95.1
3
2
3
2
o ===gq
yc
m 8.0o =y
Since yo > yco → subcritical flow
/s/mm 5.123 3
o ===BQ
q
Step 2. Calculate yc2 and Bmax
m 9792.08.081.92
5.18.0
2 2
2
2o
2o
oo =××
+=+=gyq
yE
m 6528.09792.032
32
min2 =×== Eyc
m 816.1652.13
maxmax ===
B
/sm 652.16528.081.9 2332max =×== cgyq
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(b) If B2 = 1.2 m,
m 816.1max2 =<BB → Case 3, where new qmax, i.e. q′max is required
Step 3. Calculate y1, y2 and y3
/sm 5.22.13 2
2max ===′
BQ
q
m 8605.081.95.2
3
2
3
2max
22 ==′
=′=g
qyy c
m 291.18605.023
23
2min =×=′=′ cyE
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1,321,3
2max
1,3 2E
ygq
y ′=′
′+′
min31 EEE ′=′=′
291.181.925.2
21,3
2
1,3 =′××
+′y
y
From trial‐and‐error, y′1 = 0.8735 m or y′3 = 0.8476 m
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Activity 3.11
Flow inside a rectangular channel of 3.0 m width has a velocity of 3.0 m/s at 3.0 m depth. The channel is experiencing a step of 0.61 m high at the channel bottom. What is the constriction to be made to the channel width in order to ensure the depth of flow upstream does not change.
Given V = 3 m/s, B = 3 m, yo = 3 m, and H = 0.61 mThus, q = yoV = 3 × 3 = 9 m2/s
Step 1. Determine yo and yco
m 021.281.99
3
2
3
2
o ===gq
yc
m 0.3o =y
Since yo > yco → subcritical flow
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m 459.3381.92
93
2 2
2
2o
2
oo =××
+=+=gyq
yE
m 032.3021.223
23
min =×== cyE
Step 2. Calculate Hmin
m 427.0032.3459.3minomin =−=−= EEH
Step 3. Determine y1, y2 and y3
Since H = 0.61 m > Hmin = 0.427 m
→ Case 3: Backwater upstream of weir
m 642.361.0032.3min3,1 =+=+=′ HEE
In order to maintain the same specific energy and reduce y′1 to yo, q has to be increased, i.e. via width constriction.
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E = y
E (m)
y (m)
E2=Emin
y1 = y1′ ≠ yo
yc =2.021
Eo
H=0.61 m
1 2 30
0.61 m
3 myc=2.021 m
Emin=3.032 m
Eo=3.459 m
y1′ > yo and y3′ < yc
yc=2.021 m y3
Backwater
y1
EGL
y3 ≠ yo
Hmin=0.427 m
E′1,3
yo =3.459
E = y
E (m)
y (m)
E2=Emin
y1 = y1′ ≠ yo
yc =2.021
Eo
H=0.61 m
1 2 30
0.61 m
3 myc=2.021 m
Emin=3.032 m
Eo=3.459 m
y1′ > yo and y3′ < yc
yc=2.021 m y3
Backwater
y1
EGL
y3 ≠ yo
Hmin=0.427 m
E′1,3
yo =3.459
E′′1,3
yc2
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m 642.33,1min =′=′ EE
m 428.2642.332
32
min2 =×=′= Eyc
m 7595.085.119
maxmax ===
B
/sm 85.11428.281.9 2332max =×== cgyq
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E = y
E (m)
y (m)
yc2 =2.021
Eo
H=0.61 m
1 2 30
0.61 m
3 m
Emin=3.642 m
Eo=3.459 m
yc=2.021 m y3
y1=3 m
EGL
y′3
Hmin=0.427 m
E′min
y′1 = yo =3.459
E′′1,3
B2=0.7595 mqoB=3 m
1 2 30
q2
Plan view
yc2=2.428 m
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Activity 3.12
A rectangular channel of 2.6 m width with Manning n = 0.015, and longitudinal slope of 0.0008 is conveying flow at 9.8 m3/s. If a constriction is made by reducing channel width to 2.4 m, calculate depth of flow upstream and downstream of the constriction. Sketch the flow surface profile.
Given Q = 9.8 m3/s, B = 2.6 m, B2 = 2.4 m, n = 0.015, So = 0.0008
Step 1. Determine yo and yco
21
o
32
S
QnAR =
21
32
o
oo
0008.0
015.08.9262
6.26.2
×=⎟⎟
⎠
⎞⎜⎜⎝
⎛+ y.y
y
BFC21103 Hydraulics Tan et al. ([email protected])
m 131.181.96.28.9
3
2
3
2
o =⎟⎠⎞
⎜⎝⎛
==gq
yc Since yo > yco → subcritical flow
197.5262
6.26.2
32
o
oo =⎟⎟
⎠
⎞⎜⎜⎝
⎛+ y.y
y
m 270.2o =yThrough trial‐and‐error,
Step 2. Calculate yc2 and Bmax
m 411.227.281.92
6.28.9
27.22 2
2
2o
2o
oo =××
⎟⎠⎞
⎜⎝⎛
+=+=gyq
yE
m 607.1411.232
32
min2 =×== Eyc
Bmax is when q = qmax, where Emin = Eo
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m 536.1381.68.9
maxmax ===
B
/sm 381.6607.181.9 2332max =×== cgyq
When B2 = 2.4 m, m 536.1max2 =>BB
Step 3. Calculate y1, y2 and y3
→ Case 1, where Emin2 < EoE2 = Eo
y1 = y3 = yo = 2.270 m
/sm 083.44.28.9 2
22 ===
BQ
q
m 193.181.9083.4
3
2
3
2
o ===gq
yc
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22
22
22 2gyq
yE +=
411.281.92083.4
22
2
2 =××
+y
y
411.28497.0
22
2 =+y
y
Through trial‐and‐error,
m 7059.0 orm 242.2 22 == yy
Since it is subcritical upstream, m 242.22 =y
1 2 30
y2=2.242myo=2.270m
yc2=1.607m
Eo = 2.411 m
E2
yco=1.193m
EGL
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1.7 ChokingChoking of flow occurs when
of a broad‐crested weir in an open channelminHH >
max2 BB < at the constricted width in an open channel
Choked conditions are undesirable in the design of culverts and other surface drainage features involving channel transitions.
i.e. when the specific energy or depth of flow immediately upstream of the weir or constriction increases or is being controlled.
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Assignment #3
Q1. (a) Critical depth occurs in an open channel when the specific energy is minimum. Sketch the corresponding flow depth versus specific energy graph. From this concept, derive the general equation used to determine critical flow depth in an open channel.
(b) A rectangular channel 3.05 m wide carries 3.4 m3/s uniform flow at a depth of 0.6 m. A 0.2 m‐high weir is placed across the channel.(i) Does the weir cause hydraulic jump upstream of the weir?
Provide reason why.
(ii) Calculate the flow depth above the weir, and just upstream of the weir. Classify the surface profile of flowupstream of the weir. Sketch the resulting flow‐surface profile and energy line, showing the critical depth yc and normal depth yo.
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Q2. (a) An engineer is to analyze flow in an open channel in which the channel is designed to be constricted by placing bridge embankment at both sides of the channel. Explain the consequences due to the constriction.
(b) An 8‐m wide rectangular channel is conveying flow uniformly at a rate of 18.6 m3/s and depth of 1.2 m. A temporary short span bridge is to be built across the channel in which bridge embankment is needed at both sides of the channel causing the channel to be constricted under the proposed bridge.(i) Calculate the maximum channel width under the proposed bridge
which will not cause backwater upstream.
(ii) If the channel width under the proposed bridge is 4 m due to theunavoidable condition, calculate the expected flow depth under the bridge, at just upstream and just downstream of the bridge.
(iii) If the flow depth just upstream of the proposed bridge is to be limited to 0.2 m higher than the normal depth, calculate the channel width under the bridge.
‐ End of Question ‐