Chap1 open channel flow

25
HYDRAULICS UNIFORM FLOW IN OPEN CHANNELS By Erni Syuhada Bt Mazwil Ishan

description

Uniform Flow in Open Channel

Transcript of Chap1 open channel flow

Page 1: Chap1 open channel flow

HYDRAULICS

UNIFORM FLOW IN OPEN CHANNELS

ByErni Syuhada Bt Mazwil Ishan

Page 2: Chap1 open channel flow

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.

Page 3: Chap1 open channel flow

CONTENT

What is Open Channel Types of Open ChannelTypes of flowing water and controlSolution of uniform flow in Open Channel

Page 4: Chap1 open channel flow

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

Page 5: Chap1 open channel flow

Open Channel

TYPES OF OPEN CHANNEL

Natural ChannelIrregular shape

i.e : river, hillsides rivulets, tidal etuaries

Artificial ChannelRegular shape

i.e : drains, culverts, sewer, tunnels

Page 6: Chap1 open channel flow

TYPES OF OPEN CHANNEL

Page 7: Chap1 open channel flow

TYPES OF FLOWING WATER AND ITS CONTROL

Rapidly Varied Flow

i.e : hydraulic jump

Non-Uniform Flow

≠ 0

Uniform Flow

= 0

Gradually Varied flow

i.e : upstream of obstruction

Open Channel

Steady Flow

= 0

Open ChannelUnsteady Flow

≠ 0

Page 8: Chap1 open channel flow

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

Page 9: Chap1 open channel flow

TYPES OF FLOWING WATER AND ITS CONTROL

Uniform• y (depth of water) and v (velocity) remain constant

along the channel. Figure 2.0

Non - uniform Flow• y and v change along the length of the

channel

Figure 2.0

Page 10: Chap1 open channel flow

• Flow Classifications1) 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)

TYPES OF FLOWING WATER AND ITS CONTROL

V = average channel velocityL = length of channelv = kinematic viscosity of fluid

Page 11: Chap1 open channel flow

2) Depending on Froude number, Fr

– Fr = 1 : Critical Flow

– Fr < 1 : Subcritical Flow – slow flowing water

– Fr > 1 : Supercritical Flow – fast flowing water

TYPES OF FLOWING WATER AND ITS CONTROL

V = average channel velocityg = gravity acceralationD = hydraulics water depth

Page 12: Chap1 open channel flow

TURBULENT

LAMINAR

Page 13: Chap1 open channel flow
Page 14: Chap1 open channel flow
Page 15: Chap1 open channel flow

TYPES OF FLOWING WATER AND ITS CONTROL

Critical Section (In uniform and non-uniform flow)1) If So < Sc, y > yc : Subcritical flow2) If So = Sc, y = yc : Critical flow3) If So > Sc, y < yc : Supercritical flow

Figure 3.0

Page 16: Chap1 open channel flow

Bernoulli’s Equation

Lhzg

Vpz

g

Vp 2

222

1

211

22

Page 17: Chap1 open channel flow

Open Channel

GEOMETRIC PROPERTIES OF OPEN CHANNELS

RECTANGULAR CHANNEL TRAPEZOIDAL CHANNEL

Page 18: Chap1 open channel flow

• The terminology of geometric elementsy : depth of flow T : top width b : bottom channel widthm : side slope So : channel bottom slope v : average flow density

Fr : Froude number Re : Reynold number L : length of channelQ : flow rates , Q = AV A : area of the flow P : wetted perimeterR: hydraulic radius at cross section

D : hydraulics water depth V : volume

ν : velocity E : specific energy ∆z : weir height : flow temperature q = discharge over width

(m)

GEOMETRIC PROPERTIES OF OPEN CHANNELS

Page 19: Chap1 open channel flow

Type of channel

TOP WIDTH, T

AREA, A WETTED PERIMETER, P

RECTANGULAR B By B + 2yTRAPEZOIDAL B+2my By + my2 B+2y √ 1+m2

GEOMETRIC PROPERTIES OF OPEN CHANNELS

Where,

Page 20: Chap1 open channel flow

UNIFORM FLOW IN OPEN CHANNEL

Uniform flow is an equilibrium condition that flow tends to if the channel :

a)constant slopeb)constant cross sectionc)constant roughnessd)depth, water area, velocity and discharge at every section of channel are constante)channel bed, water surface and energy line are parallel, So = Sw = Sf)y1 = y2 , V1 = V2

Page 21: Chap1 open channel flow

• CHEZY FORMULA :

UNIFORM FLOW IN OPEN CHANNEL

Where ; V = mean velocity (m/s)C = Chezy’s factor of flow resistance (m1/2/s)R = hydraulic radiusSo = slope of energy lineQ = Discharge (m3/s)

• MANNING FORMULA :Where ; V = mean velocity (m/s)

n = Manning’s coefficient of roughness (s/m1/3) R = hydraulic radiusSo = slope of energy lineQ = Discharge (m3/s)

Page 22: Chap1 open channel flow

UNIFORM FLOW IN OPEN CHANNEL

Closed conduits flowing partly fullCorrugated metal storm drains 0.010Concrete culvert 0.024Unfinished concrete 0.013Clay drain tile 0.014Lined or built up channelsUnpainted steel 0.012Planed wood 0.012Unplaned wood 0.013Trowel – finished concrete 0.013Rough concrete 0.017Glazed brick 0.020Brick in cement mortar 0.013Excavated channelsClean earth (straight channel) 0.022Earth with weeds (winding channel) 0.030Natural streamsClean and straight 0.030Weedy reaches, deep pools 0.100

Typical values of Manning’s coefficient, n

Page 23: Chap1 open channel flow

SOLUTION IN OPEN CHANNEL

• Conveyor FactorFrom eq

We obtain ; For Chezy

For Manning

Page 24: Chap1 open channel flow

• Section Factor, Z For Chezy ;

For Manning;

SOLUTION IN OPEN CHANNEL

• Thus, normal depth, yo can be obtain by using trial and error method

Page 25: Chap1 open channel flow

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.