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HYDRAULICS ENGINEERING
UNIFORM FLOW IN OPEN CHANNELS
By
Erni Syuhada Bt Mazwil Ishan
HYDRAULICS ENGINEERING
• A scientific fluid flow particularly in water
thoroughly in pipe, open channel, orifice and
embankment, including the problem related
to energy and pressure.
• Related to water or fluid in dynamic condition.
CONTENT
 What is Open Channel
 Types of Open Channel
 Types of flowing water and control
 Solution of uniform flow in Open Channel
OPEN CHANNEL
An open channel :
a)The stream not completely enclosed by solid
boundaries
b)It has free surface subjected only to
atmospheric pressure.
c) Referred as free-surface flow or gravity flow
TYPES OF OPEN CHANNEL
Open Channel

Natural Channel
Irregular shape

Artificial Channel
Regular shape

i.e : river, hillsides
rivulets, tidal etuaries

i.e : drains, culverts,
sewer, tunnels
TYPES OF OPEN CHANNEL
TYPES OF FLOWING WATER AND ITS
CONTROL
Open
Channel
Steady Flow

Open Channel
Unsteady Flow
≠0

=0

Uniform Flow

Non-Uniform Flow

= 0

≠0

Gradually
Varied flow

Rapidly
Varied Flow

i.e : upstream
of obstruction

i.e : hydraulic
jump
TYPES OF FLOWING WATER AND ITS
CONTROL
Steady
• y (depth of water) and v (velocity) remain constant
with respect to time
Unsteady Flow
• y and v change with time
TYPES OF FLOWING WATER AND ITS
CONTROL

Uniform
• y (depth of water) and v (velocity) remain constant
along the channel. Figure 2.0

Figure 2.0

Non - uniform Flow
• y and v change along the length of the
channel
TYPES OF FLOWING WATER AND ITS
CONTROL
• Flow Classifications
1) Depending on the Reynolds number, Re
– Laminar Flow (if Re < 500): very slow and shallow
flowing water in very smooth open channels.
– Turbulent Flow (if Re > 1000): ordinary flow in
ordinary open channels.
– Transition Flow (if 500 < Re < 1000)

V = average channel velocity
L = length of channel
v = kinematic viscosity of fluid
TYPES OF FLOWING WATER AND ITS
CONTROL
2) Depending on Froude number, Fr
– Fr = 1 : Critical Flow
– Fr < 1 : Subcritical Flow – slow flowing water
– Fr > 1 : Supercritical Flow – fast flowing water
V = average channel velocity
g = gravity acceralation
D = hydraulics water depth
TURBULENT

LAMINAR
TYPES OF FLOWING WATER AND ITS
CONTROL
Critical Section (In uniform and non-uniform flow)
1) If So < Sc, y > yc : Subcritical flow
2) If So = Sc, y = yc : Critical flow
3) If So > Sc, y < yc : Supercritical flow

Figure 3.0
Bernoulli’s Equation
2

2

p1 V1
p2 V2
+
+ z1 =
+
+ z 2 + hL
γ 2g
γ
2g
GEOMETRIC PROPERTIES OF OPEN
CHANNELS
Open Channel
RECTANGULAR CHANNEL

TRAPEZOIDAL CHANNEL
GEOMETRIC PROPERTIES OF OPEN
CHANNELS
• The terminology of geometric elements
y : depth of flow
m : side slope

T : top width
So : channel bottom slope

b : bottom channel width
v : average flow density

Fr : Froude number
Q : flow rates , Q = AV
R: hydraulic radius at cross
section
ν : velocity
θ : flow temperature

Re : Reynold number
L : length of channel
A : area of the flow
P : wetted perimeter
D : hydraulics water depth V : volume
E : specific energy
∆z : weir height
q = discharge over width
(m)
GEOMETRIC PROPERTIES OF OPEN
CHANNELS
Type of
TOP WIDTH,
channel
T
RECTANGULAR
B

AREA, A
By

WETTED
PERIMETER, P
B + 2y

TRAPEZOIDAL

By + my2

B+2y √ 1+m2

Where,

B+2my
UNIFORM FLOW IN OPEN CHANNEL
Uniform flow is an equilibrium condition that flow
tends to if the channel :
a)constant slope
b)constant cross section
c)constant roughness
d)depth, water area, velocity and discharge at every
section of channel are constant
e)channel bed, water surface and energy line are
parallel, So = Sw = S
f)y1 = y2 , V1 = V2
UNIFORM FLOW IN OPEN CHANNEL
• CHEZY FORMULA :
Where ; V = mean velocity (m/s)
C = Chezy’s factor of flow resistance (m1/2/s)
R = hydraulic radius
So = slope of energy line
Q = Discharge (m3/s)

• MANNING FORMULA :
Where ; V = mean velocity (m/s)
n = Manning’s coefficient of roughness (s/m1/3)
R = hydraulic radius
So = slope of energy line
Q = Discharge (m3/s)
UNIFORM FLOW IN OPEN CHANNEL
Typical values of Manning’s coefficient, n
Closed conduits flowing partly full
Corrugated metal storm drains
Concrete culvert
Unfinished concrete
Clay drain tile
Lined or built up channels
Unpainted steel
Planed wood
Unplaned wood
Trowel – finished concrete
Rough concrete
Glazed brick
Brick in cement mortar
Excavated channels
Clean earth (straight channel)
Earth with weeds (winding channel)
Natural streams
Clean and straight
Weedy reaches, deep pools

0.010
0.024
0.013
0.014
0.012
0.012
0.013
0.013
0.017
0.020
0.013
0.022
0.030
0.030
0.100
SOLUTION IN OPEN CHANNEL
• Conveyor Factor
From eq
We obtain ;
For Chezy

For Manning
SOLUTION IN OPEN CHANNEL
• Section Factor, Z
For Chezy ;
For Manning;
• Thus, normal depth, yo can be obtain by using
trial and error method
SOLUTION IN OPEN CHANNEL
• Example :
Given trapezoidal channel 10m wide with side
slope of 1:1.5. Bed slope is 0.0003. The
channel with concrete lining, n = 0.012.
Calculate the velocity, V and flow rate, Q
when the flow depth is 3.0m. If the flow rate
is 50m/s, determine the slope, So of channel.

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Chap1 open channel flow

  • 1. HYDRAULICS ENGINEERING UNIFORM FLOW IN OPEN CHANNELS By Erni Syuhada Bt Mazwil Ishan
  • 2. HYDRAULICS ENGINEERING • A scientific fluid flow particularly in water thoroughly in pipe, open channel, orifice and embankment, including the problem related to energy and pressure. • Related to water or fluid in dynamic condition.
  • 3. CONTENT  What is Open Channel  Types of Open Channel  Types of flowing water and control  Solution of uniform flow in Open Channel
  • 4. OPEN CHANNEL An open channel : a)The stream not completely enclosed by solid boundaries b)It has free surface subjected only to atmospheric pressure. c) Referred as free-surface flow or gravity flow
  • 5. TYPES OF OPEN CHANNEL Open Channel Natural Channel Irregular shape Artificial Channel Regular shape i.e : river, hillsides rivulets, tidal etuaries i.e : drains, culverts, sewer, tunnels
  • 6. TYPES OF OPEN CHANNEL
  • 7. TYPES OF FLOWING WATER AND ITS CONTROL Open Channel Steady Flow Open Channel Unsteady Flow ≠0 =0 Uniform Flow Non-Uniform Flow = 0 ≠0 Gradually Varied flow Rapidly Varied Flow i.e : upstream of obstruction i.e : hydraulic jump
  • 8. TYPES OF FLOWING WATER AND ITS CONTROL Steady • y (depth of water) and v (velocity) remain constant with respect to time Unsteady Flow • y and v change with time
  • 9. TYPES OF FLOWING WATER AND ITS CONTROL Uniform • y (depth of water) and v (velocity) remain constant along the channel. Figure 2.0 Figure 2.0 Non - uniform Flow • y and v change along the length of the channel
  • 10. TYPES OF FLOWING WATER AND ITS CONTROL • Flow Classifications 1) Depending on the Reynolds number, Re – Laminar Flow (if Re < 500): very slow and shallow flowing water in very smooth open channels. – Turbulent Flow (if Re > 1000): ordinary flow in ordinary open channels. – Transition Flow (if 500 < Re < 1000) V = average channel velocity L = length of channel v = kinematic viscosity of fluid
  • 11. TYPES OF FLOWING WATER AND ITS CONTROL 2) Depending on Froude number, Fr – Fr = 1 : Critical Flow – Fr < 1 : Subcritical Flow – slow flowing water – Fr > 1 : Supercritical Flow – fast flowing water V = average channel velocity g = gravity acceralation D = hydraulics water depth
  • 13.
  • 14.
  • 15. TYPES OF FLOWING WATER AND ITS CONTROL Critical Section (In uniform and non-uniform flow) 1) If So < Sc, y > yc : Subcritical flow 2) If So = Sc, y = yc : Critical flow 3) If So > Sc, y < yc : Supercritical flow Figure 3.0
  • 16. Bernoulli’s Equation 2 2 p1 V1 p2 V2 + + z1 = + + z 2 + hL γ 2g γ 2g
  • 17. GEOMETRIC PROPERTIES OF OPEN CHANNELS Open Channel RECTANGULAR CHANNEL TRAPEZOIDAL CHANNEL
  • 18. GEOMETRIC PROPERTIES OF OPEN CHANNELS • The terminology of geometric elements y : depth of flow m : side slope T : top width So : channel bottom slope b : bottom channel width v : average flow density Fr : Froude number Q : flow rates , Q = AV R: hydraulic radius at cross section ν : velocity θ : flow temperature Re : Reynold number L : length of channel A : area of the flow P : wetted perimeter D : hydraulics water depth V : volume E : specific energy ∆z : weir height q = discharge over width (m)
  • 19. GEOMETRIC PROPERTIES OF OPEN CHANNELS Type of TOP WIDTH, channel T RECTANGULAR B AREA, A By WETTED PERIMETER, P B + 2y TRAPEZOIDAL By + my2 B+2y √ 1+m2 Where, B+2my
  • 20. UNIFORM FLOW IN OPEN CHANNEL Uniform flow is an equilibrium condition that flow tends to if the channel : a)constant slope b)constant cross section c)constant roughness d)depth, water area, velocity and discharge at every section of channel are constant e)channel bed, water surface and energy line are parallel, So = Sw = S f)y1 = y2 , V1 = V2
  • 21. UNIFORM FLOW IN OPEN CHANNEL • CHEZY FORMULA : Where ; V = mean velocity (m/s) C = Chezy’s factor of flow resistance (m1/2/s) R = hydraulic radius So = slope of energy line Q = Discharge (m3/s) • MANNING FORMULA : Where ; V = mean velocity (m/s) n = Manning’s coefficient of roughness (s/m1/3) R = hydraulic radius So = slope of energy line Q = Discharge (m3/s)
  • 22. UNIFORM FLOW IN OPEN CHANNEL Typical values of Manning’s coefficient, n Closed conduits flowing partly full Corrugated metal storm drains Concrete culvert Unfinished concrete Clay drain tile Lined or built up channels Unpainted steel Planed wood Unplaned wood Trowel – finished concrete Rough concrete Glazed brick Brick in cement mortar Excavated channels Clean earth (straight channel) Earth with weeds (winding channel) Natural streams Clean and straight Weedy reaches, deep pools 0.010 0.024 0.013 0.014 0.012 0.012 0.013 0.013 0.017 0.020 0.013 0.022 0.030 0.030 0.100
  • 23. SOLUTION IN OPEN CHANNEL • Conveyor Factor From eq We obtain ; For Chezy For Manning
  • 24. SOLUTION IN OPEN CHANNEL • Section Factor, Z For Chezy ; For Manning; • Thus, normal depth, yo can be obtain by using trial and error method
  • 25. SOLUTION IN OPEN CHANNEL • Example : Given trapezoidal channel 10m wide with side slope of 1:1.5. Bed slope is 0.0003. The channel with concrete lining, n = 0.012. Calculate the velocity, V and flow rate, Q when the flow depth is 3.0m. If the flow rate is 50m/s, determine the slope, So of channel.