(Part ii)- open channels
-
Upload
mohsin-siddique -
Category
Engineering
-
view
359 -
download
4
Transcript of (Part ii)- open channels
![Page 1: (Part ii)- open channels](https://reader034.fdocuments.us/reader034/viewer/2022042512/55a6c1231a28ab36688b4920/html5/thumbnails/1.jpg)
Open Channel Hydraulics
1
Hydraulics
Dr. Mohsin Siddique
Assistant Professor
![Page 2: (Part ii)- open channels](https://reader034.fdocuments.us/reader034/viewer/2022042512/55a6c1231a28ab36688b4920/html5/thumbnails/2.jpg)
Steady Flow in Open Channels
� Specific Energy and Critical Depth
� Surface Profiles and Backwater Curves in Channels of Uniform sections
� Hydraulics jump and its practical applications.
� Flow over Humps and through Constrictions
� Broad Crested Weirs and Venturi Flumes
2
![Page 3: (Part ii)- open channels](https://reader034.fdocuments.us/reader034/viewer/2022042512/55a6c1231a28ab36688b4920/html5/thumbnails/3.jpg)
Specific Energy and Critical Depth
Basic Definitions
� Head
� Energy per unit weight
� Energy Line
� Line joining the total head at different positions
� Hydraulics Grade Line
� Line joining the pressure head at different positions
3
![Page 4: (Part ii)- open channels](https://reader034.fdocuments.us/reader034/viewer/2022042512/55a6c1231a28ab36688b4920/html5/thumbnails/4.jpg)
Specific Energy and Critical Depth
Basic Definitions
� Open Channel Flow
1Z
g
V
2
2
1
Datum
So
1y
2Z
g
V
2
2
2
2y
HGL
EL
Water Level
lhg
VyZ
g
VyZ +++=++
22
2
222
2
111
4
![Page 5: (Part ii)- open channels](https://reader034.fdocuments.us/reader034/viewer/2022042512/55a6c1231a28ab36688b4920/html5/thumbnails/5.jpg)
� Slopes in Open Channel Flow
� So= Slope of Channel Bed = (Z1-Z2)/(Δx)= -ΔZ/Δx
� Sw= Slope of Water Surface= [(Z1+y1)-(Z2+y2)]/Δx
� S= Slope of Energy Line= [(Z1+y1+V12/2g)-(Z2+y2+V2
2/2g)]/Δx
= hl/ΔL
1Z
g
V
2
2
1
Datum
So
1y
2Z
g
V
2
2
2
2y
HGL
EL
Water
Level
Sw
S
∆L
∆x
Specific Energy and Critical Depth
Basic Definitions
5
![Page 6: (Part ii)- open channels](https://reader034.fdocuments.us/reader034/viewer/2022042512/55a6c1231a28ab36688b4920/html5/thumbnails/6.jpg)
Specific Energy and Critical Depth
Basic Definitions
� Slopes in Open Channel Flow
1Z
g
V
2
2
1
Datum
So
1y
2Z
g
V
2
2
2
2y
HGL
EL
Water
Level
Sw
S
∆L
∆xFor Uniform Flow
y1=y2 and V12/2g=V2
2/2gHence the line indicating the bed of the channel, water surface profile and energy line are parallel to each other.For θ being very small (say less than 5 degree) i.e ∆x=∆L
So=Sw=S6
![Page 7: (Part ii)- open channels](https://reader034.fdocuments.us/reader034/viewer/2022042512/55a6c1231a28ab36688b4920/html5/thumbnails/7.jpg)
Specific Energy and Critical Depth
Basic Definitions
� Froude’s Number (FN)
� It is the ratio of inertial forces to gravitational forces.
� For a rectangular channel it may be written as
� FN= 1 Critical Flow
> 1 Super-Critical Flow
< 1 Sub-Critical Flow
gy
VNF =
William Froude (1810-79)
Born in England and engaged
in shipbuilding. In his sixties
started the study of ship
resistance, building a boat
testing pool (approximately 75
m long) near his home. After his
death, this study was continued
by his son, Robert Edmund
Froude (1846-1924). For
similarity under conditions of
inertial and gravitational forces,
the non-dimensional number
used carries his name.
7
![Page 8: (Part ii)- open channels](https://reader034.fdocuments.us/reader034/viewer/2022042512/55a6c1231a28ab36688b4920/html5/thumbnails/8.jpg)
Specific Energy and Critical Depth
(Rectangular Channels)
� Specific Energy � Specific Energy at a section in an open channel is the energy
with reference to the bed of the channel.
� Mathematically;
Specific Energy = E = y+V2/2g
For a rectangular Channel
q = Discharge per unit width m3/s per m
B
( )Vy
B
VBy
B
AV
B
Qqwhere
yE
yE
yg
q
gV
====
+=
+=
2
2
2
2
2 y
8
Datum
![Page 9: (Part ii)- open channels](https://reader034.fdocuments.us/reader034/viewer/2022042512/55a6c1231a28ab36688b4920/html5/thumbnails/9.jpg)
Specific Energy and Critical Depth
� As it is clear from E~y diagramdrawn for constant discharge forany given value of E, there wouldbe two possible depths, say y1 andy2. These two depths are calledAlternate depths.
� However for point Ccorresponding to minimumspecific energy Emin, there wouldbe only one possible depth yc. Thedepth yc is know as critical depth.
� The critical depth may be definedas depth corresponding to minimumspecific energy discharge remainingConstant.
� E~y Diagram or E-Diagram
Static Head
Line
BQqwhereyEyg
q/2
2
2=+=
9
![Page 10: (Part ii)- open channels](https://reader034.fdocuments.us/reader034/viewer/2022042512/55a6c1231a28ab36688b4920/html5/thumbnails/10.jpg)
Specific Energy and Critical Depth
� For y>yc , V<Vc Deep Channel
� Sub-Critical Flow, Tranquil Flow, Slow Flow.
� For y<yc , V>Vc Shallow Channel
� Super-Critical Flow, Shooting Flow, Rapid Flow, Fast Flow.
10
![Page 11: (Part ii)- open channels](https://reader034.fdocuments.us/reader034/viewer/2022042512/55a6c1231a28ab36688b4920/html5/thumbnails/11.jpg)
Specific Energy and Critical Depth Relationship Between Critical Depth and Specific Energy
for rectangular channels
22
2cc y
g
V=
Substituting in eq. (1)
( )
( )( )
( )g
yVc
g
yVc
ccg
yV
c
g
q
c
cg
q
c
gy
q
dydE
gy
q
dydE
gy
q
gV
cc
cc
cc
y
y
yVqy
y
yyy
yyE
2
3
3
3/1
3/1
23
3
2
32
22
2
2
2
22
22
22
2
2
2
2
)2(
)(
01
1
)1(
=
=
==
=
==
=−=
−=
+=+=
Q
Q
)5(23
2min
cc
y
cc
yE
yEE c
=
+==
11
)4(1
)3(22
2
=
=
c
c
c
gy
V
y
gVc
Froude # =1 !!
![Page 12: (Part ii)- open channels](https://reader034.fdocuments.us/reader034/viewer/2022042512/55a6c1231a28ab36688b4920/html5/thumbnails/12.jpg)
Example
12
![Page 13: (Part ii)- open channels](https://reader034.fdocuments.us/reader034/viewer/2022042512/55a6c1231a28ab36688b4920/html5/thumbnails/13.jpg)
Problem
13
( ) 3/12
g
q
cy =
( ) 2/1
cc gyV =
2/13/2486.1oSAR
nQ =
![Page 14: (Part ii)- open channels](https://reader034.fdocuments.us/reader034/viewer/2022042512/55a6c1231a28ab36688b4920/html5/thumbnails/14.jpg)
Problem 11.38
� Water is released from a sluice gate in a rectangular channel 1.5m wide such that depth is 0.6 m and velocity is 4.5 m/s. Find
(a). Critical Depth for this specific energy
(b). Critical Depth for this rate of Discharge
(c). The type of flow and alternate depth by either direct solution or the discharge Curve.
� Solution
B=1.5 m
y=0.6 m
V= 4.5 m/sec
(a)
mEy
mg
VyEnergySpecific
c 088.13
2
632.12
2
==
=+=
sluice gate
14
Critical flow
![Page 15: (Part ii)- open channels](https://reader034.fdocuments.us/reader034/viewer/2022042512/55a6c1231a28ab36688b4920/html5/thumbnails/15.jpg)
Problem 11.38
(b)
(c)
CriticalSuperisFlowTherefore
ymg
qy
mpermvyq
mByVAVQ
c
−
>=
=
==
===
906.0
sec/7.2
sec/05.4
3/12
3
CriticalSuperisFlow
gy
VFN
−
>== 1855.1
2
2
2
2
3
)81.9(2
7.2632.1
2
sec/05.4
yy
gy
qyE
mByVAVQ
+=
+=
===
my
my
yy
46.1
6.0
037156.0632.1 23
=
=
=+−
15
![Page 16: (Part ii)- open channels](https://reader034.fdocuments.us/reader034/viewer/2022042512/55a6c1231a28ab36688b4920/html5/thumbnails/16.jpg)
Specific Energy and Critical Depth
(Non Rectangular Channels)
� Hydraulic Depth
� The hydraulic depth, yh for non rectangular channel is the depth of arectangular channel having flow area and base width the same as the flowarea and top width respectively as for non rectangular channel.
dy
T
A y
dy
T
A yh
16
![Page 17: (Part ii)- open channels](https://reader034.fdocuments.us/reader034/viewer/2022042512/55a6c1231a28ab36688b4920/html5/thumbnails/17.jpg)
Specific Energy and Critical DepthRelationship Between Critical Depth and Specific Energy
� Froude’s number may be numerically calculate as
3
2
2
22
gA
TQF
T
Ay
gA
QF
gy
VF
N
h
TA
h
N
N
=
==
=
ycyg
Q
T
A
Therefore
dy
dEflowCriticalfor
TgA
Q
dy
dE
TdydASince
=
=
=
−=
=
23
3
2
0
1
17
dy
dA
gA
Q
dy
dE
gA
QyEEq
3
2
2
2
1
2)1.(
−=
+=⇒
![Page 18: (Part ii)- open channels](https://reader034.fdocuments.us/reader034/viewer/2022042512/55a6c1231a28ab36688b4920/html5/thumbnails/18.jpg)
Problems11.45
� A Trapezoidal canal with side slopes 1:2 has a bottom width of 3m and carries a flow of 20 m3/s.
a). Find the Critical Depth and Critical velocity.
b). If the canal is lined with Brick (n=0.015), find the critical slope for the same rate of discharge.
� Solution
B=3m
T
A= (B+xy)y
P= B+2y(1+x2)1/2
T= B+2xy
1
x
Q=20 m3/s
x= 2
18
![Page 19: (Part ii)- open channels](https://reader034.fdocuments.us/reader034/viewer/2022042512/55a6c1231a28ab36688b4920/html5/thumbnails/19.jpg)
Problem 11.45
�Q2/g = A3/T
� (b)
Q2/g y A T A3/T
40.775 1 5 7 17.85
2 14 11 249.45
1.2 6.48 7.8 34.88
1.25 6.883 8.004 40.74
1.2512 6.885 8.0048 40.77
224433.0
2/1
2/3
=
=
cS
SP
A
n
AQ
19
![Page 20: (Part ii)- open channels](https://reader034.fdocuments.us/reader034/viewer/2022042512/55a6c1231a28ab36688b4920/html5/thumbnails/20.jpg)
Problem
� The 50o triangular channel in Fig. E10.6 has a flow rate Q 16 m3/s. Compute (a) yc, (b) Vc, and (c) Sc if n 0.018.
� Answer: (a). 2.37m, (b). 3.41m, (c ) 0.00542
2020
![Page 21: (Part ii)- open channels](https://reader034.fdocuments.us/reader034/viewer/2022042512/55a6c1231a28ab36688b4920/html5/thumbnails/21.jpg)
Surface Profiles and
Backwater Curves in Channels of
Uniform sections
21
![Page 22: (Part ii)- open channels](https://reader034.fdocuments.us/reader034/viewer/2022042512/55a6c1231a28ab36688b4920/html5/thumbnails/22.jpg)
Steady Flow in Open Channels
� Specific Energy and Critical Depth
� Surface Profiles and Backwater Curves in Channels of Uniform Sections
� Hydraulics jump and its practical applications.
� Flow over Humps and through Constrictions
� Broad Crested Weirs and Venturi Flumes
22
![Page 23: (Part ii)- open channels](https://reader034.fdocuments.us/reader034/viewer/2022042512/55a6c1231a28ab36688b4920/html5/thumbnails/23.jpg)
Types of Bed Slopes
� Mild Slope (M)yo > yc
So < Sc
� Critical Slope (C)yo = yc
So = Sc
� Steep Slope (S)yo < yc
So > Sc
So1<Sc
So2>Sc
yo1
yo2
yc
Break
23
yo= normal depth of flowyc= critical depthSo= channel bed slopeSc=critical channel bed slope
![Page 24: (Part ii)- open channels](https://reader034.fdocuments.us/reader034/viewer/2022042512/55a6c1231a28ab36688b4920/html5/thumbnails/24.jpg)
Occurrence of Critical Depth
� Change in Bed Slope
� Sub-critical to Super-Critical
� Control Section
� Super-Critical to Sub-Critical
� Hydraulics Jump
Control Section
So1<Sc
So2>Sc
yo1
yo2
yc
Break where
Slope changes
Dropdown Curve
So1>Sc
So2<Sc
yo1
yo2
yc
Hydraulic Jump
24
![Page 25: (Part ii)- open channels](https://reader034.fdocuments.us/reader034/viewer/2022042512/55a6c1231a28ab36688b4920/html5/thumbnails/25.jpg)
Occurrence of Critical Depth
� Change in Bed Slope
� Free outfall
� Mild Slope
� Free Outfall
� Steep Slope
yb~ 0.72 yc
So<Sc
yo yc
3~10 ycBrink
yc
So>Sc
25
![Page 26: (Part ii)- open channels](https://reader034.fdocuments.us/reader034/viewer/2022042512/55a6c1231a28ab36688b4920/html5/thumbnails/26.jpg)
Non Uniform Flow or Varied Flow.
� For uniform flow through openchannel, dy/dl is equal to zero.However for non-uniform flow thegravity force and frictionalresistance are not in balance. Thusdy/dl is not equal to zero whichresults in non-uniform flow.
� There are two types of nonuniform flows.
� In one the changing conditionextends over a long distance andthis is called gradually varied flow.
� In the other the change may occurover very abruptly and the transitionis thus confined to a short distance.This may be designated as a localnon-uniform flow phenomenon orrapidly varied flow.
So1<Sc
So2>Sc
yo1
yo2
yc
Break
26
![Page 27: (Part ii)- open channels](https://reader034.fdocuments.us/reader034/viewer/2022042512/55a6c1231a28ab36688b4920/html5/thumbnails/27.jpg)
Energy Equation for Gradually Varied Flow.
1Z
g
V
2
2
1
Datum
So
1y
2Z
g
V
2
2
2
2y
HGL
EL
Water Level
lhg
VyZ
g
VyZ +++=++
22
2
222
2
111
Theoretical EL
Sw
hL
∆X
∆ L
S
27Remember: Both sections are subject to atmospheric pressure
![Page 28: (Part ii)- open channels](https://reader034.fdocuments.us/reader034/viewer/2022042512/55a6c1231a28ab36688b4920/html5/thumbnails/28.jpg)
Energy Equation for Gradually Varied Flow.
( )
( ) ( )
profilesurfacewateroflengthLWhere
SS
EEL
LSLSEE
Now
forL
ZZ
X
ZZS
L
hS
hZZg
Vy
g
Vy
o
o
o
oL
L
=∆
−
−=∆
∆+∆−=
<∆
−≈
∆
−=
∆=
+−−+=+
)1(
6,
22
21
21
2121
21
2
22
2
11
θ
An approximate analysis of gradually varied, non uniform flow can be achieved by considering a length of stream consisting of a number of successive reaches, in each of which uniform occurs. Greater accuracy results from smaller depth variation in each reach.
28
![Page 29: (Part ii)- open channels](https://reader034.fdocuments.us/reader034/viewer/2022042512/55a6c1231a28ab36688b4920/html5/thumbnails/29.jpg)
Energy Equation for Gradually Varied Flow.
3/4
22
2/13/21
m
m
mm
R
nVS
SRn
V
=
=
The Manning's formula (or Chezy’s formula) is applied to average conditions in each reach to provide an estimate of the value of S for that reach as follows;
2
2
21
21
RRR
VVV
m
m
+=
+=
In practical, depth range of the interest is divided into small increments, usually equal, which define the reaches whose lengths can be found by equation (1)
29
![Page 30: (Part ii)- open channels](https://reader034.fdocuments.us/reader034/viewer/2022042512/55a6c1231a28ab36688b4920/html5/thumbnails/30.jpg)
Problem 11.59� A rectangular flume of planer
timber (n=0.012) is 1.5 m wideand carries 1.7m3/s of water. Thebed slope is 0.0006, and at acertain section the depth is 0.9m.Find the distance (in one reach) tothe section where depth is 0.75m.Is the distance upstream ordownstream ?
3
1
2
Rectangular Channel
0.012
1.5
1.7 / sec
0.0006
0.9
0.75
o
n
B m
Q m
S
y m
y
=
=
=
=
=
=
B
y
30
![Page 31: (Part ii)- open channels](https://reader034.fdocuments.us/reader034/viewer/2022042512/55a6c1231a28ab36688b4920/html5/thumbnails/31.jpg)
Problem 11.59
Solution
1 2
2 2
4 / 3
2
1
2
2
1
2
1 1 1
2 2 2
1 1
2 2
&
1.5 0.9 1.35
1.5 0.75 1.125
1.5 2 0.9 3.3
1.5 2 0.75 3
/ 0.41
/ 0.375
/ 1.26 / sec
/ 1.51 / sec
o
m
m
Since
E EL
S S
V nS
R
A x m
A x m
P x m
P x m
R A P
R A P
V Q A m
V Q A m
−∆ =
−
=
= =
= =
= + =
= + =
= =
= =
= =
= =
2 2
4 /3
1 2
2 2
1 21 2
0.3925
1.385
& 0.000961
2 2
317.73
m
m
m
m
o
o
R m
V m
V nS
R
E ENow L
S S
V Vy y
g gL
S S
m Downstream
=
=
= =
−∆ =
−
+ − +
∆ =
−
=
31
upstream
![Page 32: (Part ii)- open channels](https://reader034.fdocuments.us/reader034/viewer/2022042512/55a6c1231a28ab36688b4920/html5/thumbnails/32.jpg)
Problem
32
5ft
yo
1ft
L
![Page 33: (Part ii)- open channels](https://reader034.fdocuments.us/reader034/viewer/2022042512/55a6c1231a28ab36688b4920/html5/thumbnails/33.jpg)
Problem
33
![Page 34: (Part ii)- open channels](https://reader034.fdocuments.us/reader034/viewer/2022042512/55a6c1231a28ab36688b4920/html5/thumbnails/34.jpg)
Problem
34
![Page 35: (Part ii)- open channels](https://reader034.fdocuments.us/reader034/viewer/2022042512/55a6c1231a28ab36688b4920/html5/thumbnails/35.jpg)
Problem 11.66
� The slope of a stream of a rectangularcross section is So=0.0002, the widthis 50m, and the value of Chezy C is43.2 m1/2/sec. Find the depth foruniform flow of 8.25 m3/sec/m of thestream. If a dam raises the water levelso that at a certain distance upstreamthe increase is 1.5m, how far from thislatter section will the increase be only30cm? Use reaches with 30cm depth.
� Given That
1.5m
yo
0.3m
1/ 2
3
0.0002
50
43.2 / sec
8.25 / sec/
508.25 43.2 0.0002
50 2
6.1
o
oo o
o
oo
o
o
S
B m
C m
q m m
Aq y C S
P
yy
y
y m
=
=
=
=
=
=+
=
L
35
![Page 36: (Part ii)- open channels](https://reader034.fdocuments.us/reader034/viewer/2022042512/55a6c1231a28ab36688b4920/html5/thumbnails/36.jpg)
Problem 11.66
y A P R V E E1-E2 Vm Rm S S-So ∆L Σ∆L
By B+2y A/P q/y y+v2/g (v1+v2)/2 Vm2/(RmC2)
(E1-E2) /(S-So)
m m2 m m m/s m m m/s m m/m m/m m m
7.6 380 65.2 5.82 1.09 7.66
0.295 1.11 5.74 0.000115 -0.000085 -3454.33 -3454.33
7.3 365 64.6 5.65 1.13 7.365
7.0
6.7
6.4
V=C(RS)1/2
36
![Page 37: (Part ii)- open channels](https://reader034.fdocuments.us/reader034/viewer/2022042512/55a6c1231a28ab36688b4920/html5/thumbnails/37.jpg)
Water Surface Profiles in Gradually Varied
Flow.
1Z
g
V
2
2
1
Datum
So
1y
2Z
g
V
2
2
2
2y
HGL
EL
Water Level
g
VyZHeadTotal
2
2
++=
Theoretical EL
Sw
hL
∆X
∆L
37
![Page 38: (Part ii)- open channels](https://reader034.fdocuments.us/reader034/viewer/2022042512/55a6c1231a28ab36688b4920/html5/thumbnails/38.jpg)
Water Surface Profiles in Gradually Varied
Flow.
( )
01
0
)2(1
.
1
1
2
.tan..
22
2
2
3
22
3
2
2
2
2
22
1
=−
−∴
=
−
−=
−
=−+−=−
−+=
−
++=
++=++=
N
o
N
NNo
F
SS
dx
dyflowuniformFor
F
SSo
dx
dyor
gsindecreaisflow
ofdirectionalongheadtotalthatshowssignve
gy
qFF
dx
dySS
gy
q
dx
dy
dx
dZ
dx
dH
gulartanrecastionseccrossgConsiderin
gy
q
dx
d
dx
dy
dx
dZ
dx
dH
xdirectionhorizontalincedistrwHheadtotaltheatingDifferenti
gy
qyZ
g
vyZH
Q
Equation (2) is dynamic Equation for
gradually varied flow for constant value
of q and n
If dy/dx is +ve the depth of flowincreases in the direction of flow andvice versa
38
Important assumption !!
![Page 39: (Part ii)- open channels](https://reader034.fdocuments.us/reader034/viewer/2022042512/55a6c1231a28ab36688b4920/html5/thumbnails/39.jpg)
Water Surface Profiles in Gradually Varied
Flow.
3/10
3/10
22
3/10
22
2/13/5
2/13/2
1
1
=∴
=
=
=
=
≈
y
y
S
S
y
qnS
channel
gulartanrecinflowuniformFor
y
qnS
orSyn
q
orSyn
V
yR
channelgulartanrecwideaFor
o
o
o
o
21 F
SS
dx
dy o
−
−=
� Consequently, for constant q and n,when y>yo, S<So, and the numeratoris +ve.
� Conversely, when y<yo, S>So, andthe numerator is –ve.
� To investigate the denominator weobserve that,
� if F=1, dy/dx=infinity;
� if F>1, the denominator is -ve; and
� if F<1, the denominator is +ve.
39
![Page 40: (Part ii)- open channels](https://reader034.fdocuments.us/reader034/viewer/2022042512/55a6c1231a28ab36688b4920/html5/thumbnails/40.jpg)
Classification of Surface Profiles
� Mild Slope (M)
yo > yc
So < Sc
� Critical Slope (C)
yo = yc
So = Sc
� Steep Slope (S)
yo < yc
So > Sc
� Horizontal (H)
So = 0
� Adverse (A)
So = -ve
� Type 1: If the streamsurface lies above both thenormal and critical depth offlow (M1, S1)
� Type 2: If the streamsurface lies between normaland critical depth of flow(M2, S2)
� Type 3: If the streamsurface lies below both thenormal and critical depth offlow. (M3, S3)
40
![Page 41: (Part ii)- open channels](https://reader034.fdocuments.us/reader034/viewer/2022042512/55a6c1231a28ab36688b4920/html5/thumbnails/41.jpg)
Water Surface ProfilesMild Slope (M)
1
2
3
1:1
2 :1
3:1
oo c
N
oo c
N
o
o c
N
S Sdy Vey y y Ve M
dx F Ve
S Sdy Vey y y Ve M
dx F Ve
S Sdy Vey y y Ve M
dx F Ve
− +> > = = = + ⇒
− +
− −> > = = = − ⇒
− +
− −> > = = = + ⇒
− −
yc
Note:
For Sign of Numerator compare
yo & y
For sign of denominator compare
yc & y
If y>yo then S<So and Vice Versa
41
![Page 42: (Part ii)- open channels](https://reader034.fdocuments.us/reader034/viewer/2022042512/55a6c1231a28ab36688b4920/html5/thumbnails/42.jpg)
Water Surface ProfilesSteep Slope (S)
1
2
3
1:1
2 :1
3:1
oc o
N
oc o
N
oc o
N
S Sdy Vey y y Ve S
dx F Ve
S Sdy Vey y y Ve S
dx F Ve
S Sdy Vey y y Ve S
dx F Ve
− +> > = = = + ⇒
− +
− +> > = = = − ⇒
− −
− −> > = = = + ⇒
− −
Note:
For Sign of Numerator compare
yo & y
For sign of denominator compare
yc & y
If y>yo then S<So and Vice Versa
yc
42
![Page 43: (Part ii)- open channels](https://reader034.fdocuments.us/reader034/viewer/2022042512/55a6c1231a28ab36688b4920/html5/thumbnails/43.jpg)
Water Surface ProfilesCritical (C)
1
3
1:1
2 :1
oo c
N
oo c
N
S Sdy Vey y y Ve C
dx F Ve
S Sdy Vey y y Ve C
dx F Ve
− +> = = = = + ⇒
− +
− −= > = = = + ⇒
− −
Note:
For Sign of Numerator compare
yo & y
For sign of denominator compare
yc & y
If y>yo then S<So and Vice Versa
yo=yc
C2 is not possible
43
![Page 44: (Part ii)- open channels](https://reader034.fdocuments.us/reader034/viewer/2022042512/55a6c1231a28ab36688b4920/html5/thumbnails/44.jpg)
Water Surface ProfilesHorizontal (H)
( ) 2
( ) 3
1:1
2 :1
oo c
N
oo c
N
S Sdy Vey y y Ve H
dx F Ve
S Sdy Vey y y Ve H
dx F Ve
∞
∞
− −> > = = = − ⇒
− +
− −> > = = = + ⇒
− −
Note:
For Sign of Numerator compare
yo & y
For sign of denominator compare
yc & y
If y>yo then S<So and Vice Versa
yc
H1 is not possible bcz water has to lower down
44
![Page 45: (Part ii)- open channels](https://reader034.fdocuments.us/reader034/viewer/2022042512/55a6c1231a28ab36688b4920/html5/thumbnails/45.jpg)
Water Surface ProfilesAdverse (A)
( ) 2
( ) 3
1:1
2 :1
oo c
N
oo c
N
S Sdy Vey y y Ve A
dx F Ve
S Sdy Vey y y Ve A
dx F Ve
∞
∞
− −> > = = = − ⇒
− +
− −> > = = = + ⇒
− −
Note:
For Sign of Numerator compare
yo & y
For sign of denominator compare
yc & y
If y>yo then S<So and Vice Versa
yc
A1 is not possible bcz water has to lower down
45
![Page 46: (Part ii)- open channels](https://reader034.fdocuments.us/reader034/viewer/2022042512/55a6c1231a28ab36688b4920/html5/thumbnails/46.jpg)
Problem 1
46
� Classify the water surface profile for given data,
� Channel type: rectangular
� n=0.013
� B=1.6
� So=0.0005, Q=1.7m
� y= varies from 0.85-1.0m
� Solution:
� Calculate normal depth of flow yo using Manning’s equation
21 F
SS
dx
dy o
−
−=
( ) 2/1
0
3/2
2/1
0
3/2
2
11S
yB
ByBy
nSAR
nQ
o
oo
+==
y< yo
![Page 47: (Part ii)- open channels](https://reader034.fdocuments.us/reader034/viewer/2022042512/55a6c1231a28ab36688b4920/html5/thumbnails/47.jpg)
Problem 1
47
� Determine Critical depth
� Thus yo > yc � slope is Mild and profile type will be one of M type
� Since y lies between both yo and yc i.e. yo >y> yc, the profile type is M2
( )m
g
qyc 486.0
81.9
6.1/7.13/1
23/12
=
=
=
![Page 48: (Part ii)- open channels](https://reader034.fdocuments.us/reader034/viewer/2022042512/55a6c1231a28ab36688b4920/html5/thumbnails/48.jpg)
Problem 2
48
� Classify the water surface profile for given data,
� Channel type: rectangular
� n=0.013
� B=1.6
� So=-0.0004 < 0 adverse slope
� Q=1.7m
� y= varies from 0.85-1.0m
� Solution:
� Calculate normal depth of flow yo:
21 F
SS
dx
dy o
−
−=
yyo >∞=
![Page 49: (Part ii)- open channels](https://reader034.fdocuments.us/reader034/viewer/2022042512/55a6c1231a28ab36688b4920/html5/thumbnails/49.jpg)
Problem 2
49
� Determine Critical depth
� Thus yo > yc � Since slope is Adverse and profile type will be one of A type
� Since y lies between both yo and yc i.e. yo >y> yc, the profile type is A2
( )m
g
qyc 486.0
81.9
6.1/7.13/1
23/12
=
=
=
![Page 50: (Part ii)- open channels](https://reader034.fdocuments.us/reader034/viewer/2022042512/55a6c1231a28ab36688b4920/html5/thumbnails/50.jpg)
Problem 3
50
� B=15m, rectangular channel, Q=1400cfs, yo=6ft. � y=2.8m� Determine y to yo depth increase of decrease towards
downstream. � Solution: Determine yc
� yo< yc mean So>Sc, Steep slope (S)
� Now comparing all depths
� yc > yo >y
Hence the slope type is S3
+=+
+=
−
−=
21 F
SS
dx
dy o
Water depth will increase
![Page 51: (Part ii)- open channels](https://reader034.fdocuments.us/reader034/viewer/2022042512/55a6c1231a28ab36688b4920/html5/thumbnails/51.jpg)
Practice problems
51
![Page 52: (Part ii)- open channels](https://reader034.fdocuments.us/reader034/viewer/2022042512/55a6c1231a28ab36688b4920/html5/thumbnails/52.jpg)
Thank you
� Questions….
� Feel free to contact:
52