EXPERIMENT NO 01 NAME OF THE EXPERIMENT: - Determination of performance characteristics of Pelton wheel APARATUS: - Pelton wheel turbine, spring balance, weight, manometer. FIGURE: FORMULA: 1. Discharge, Q = 1.84 Lh3/2 Where, L = Length of weir h = Head of the weir. 2. Shaft power developed (S.P.) P = (W-S) D/2 X 2πN = (W-S) πDN watts Where, (W S )DN kW 60 1000 W = Load applied on the brake drum (N) S = Spring balance reading (N) D = Mean diameter of the brake drum (m), and N = Speed in r. p. m. 3. Water power (W.P.) = Where, wQH kW 1000 W = Specific weight of water (= 9810 N/m3) Q = Discharge in m3 /s (as calculated at 1), and H = Head (of water) acting on Pelton wheel 4. Overall efficiency, o` = S .P. W .P. 1 THEORY: This is the only impulse type of hydrodynamic turbine now in common use.. It is well suited for operating under high heads. Figure shows the elements of a typical pelton wheel installation. The runner consists of a circular disc with a number of buckets evenly spaced round its periphery. The bucket has a shape of double hemispherical cup. Each bucket is divided into two symmetrical parts by a sharp edged ridge known as splitter. One or more nozzles are mounted so that each directs a jet along a tangent to the circle through the centers of buckets called pitch circle. The jet of water impinges on the splitter which divides the jet into two equal positions, each of which after flowing round the smooth inner surface of the bucket leaves it at its outer edge. The buckets are so shaped that angle at the outlet tip varies from 10º to 20 º so that the jet of water gets deflected through 160 º to 170 º. The advantages of having a double cup shaped bucket is that axial thrust neutralize each other, being equal and opposite and hence the bearing supports the wheel shaft are not subjected to any axial or end thrust. Further at the lower tip of the bucket, a notch is cut which prevents the jet striking the preceding the bucket being intercepted by the next bucket very soon, and it also avoids the deflection of water toward the centre of the wheel as the bucket firsts meets the jet. For low heads the buckets are made of cast iron, but for higher heads they are made of cast steel, bronze or stainless steel. In order to control the quantity of water striking the runner, the nozzle fitted or needle having a penstock, provided with a spear or needle having a streamlined head which is fixed to the end of a rod .The spear may be operated into either by a wheel in case of very small units or automatically by a governor in case of almost all the bigger units. When shaft of pelton wheel is horizontal then not more than two jets are used. But if the wheel is mounted on a vertical shaft then larger number of jet is possible. 2 PROCEDURE: i) Note down the internal diameter of initial pipe and throat ii) Keeps the gate opening at 20 % initially. iii) The setup is then started and the initial weight is kept zero kg. iv) The corresponding values of spring balance weight, speed in rpm, manometric head and present gauge reading were noted down. v) Increase the weight successively at 1, 2, 3 and 4 kgs and take the corresponding all the above mentioned reading vi) vii) viii) Stop the set up and keep opening at 40 %. Repeat step no. 3, 4, 5 Repeat the same procedure for gate opening at 50 % OBSERVATIONS: 1. Diameter of pipe = 2. Diameter of throat of venturimeter = 3. Perpendicular distance d = OBSERVATION TABLE Pressure gauge reading Speed(rpm) N Spring Manometer reading balance reading h1 h2 h3 FOR GATE OPENING 20% Break weight FOR GATE OPENING 30% FOR GATE OPENING 40% 3 Net eight= (W1W2) CALCULATION:Torqu Head Discharge e (H) (Q) (T) Input (KW) power Output Unit Efficien power speed cy(ή) (KW) (N) For 20%gate openings Unit discharge (Qu) Unit power (Pu) H (m) For 30%gate openings For 40% gate openings RESULT: - The working of pelton wheel turbine has been studied. The average efficiency of the turbine for different gate openings is found to be 1. For 20 % gate opening = 2. For 30 % gate opening = 3. For 40 % gate opening = 4 EXPERIMENT NO. 02 NAME OF THE EXPERIMENT: Determination of performance characteristics of Francis Turbine. APPARATUS: - Francis turbine set up, weights, manometer. FIGURE: THEORY: Francis turbine is mixed flow type of reaction turbine. It is named in ward radial flow type of reaction turbine in 1849. later on it was modified and the modern Francis is a mixed flow type, in which water enters the runner radically at its outer periphery and leaves axially at its centre. The water from the penstock enters a scroll casing which completely surround sterner. The purpose of the casing is to provide an even distribution of water around the circumference of the turbine runner, maintaining an approximately constant velocity for the water so distributed. From the scroll casing the water passes through a speed ring on stay ring. From the speed ring, the water passes through a series of guide vanes or wicket gate provided all around the periphery of the turbine runner. The function of guide vanes is to regulate the quantity of water supplied to the runner and to direct water on to the runner to an angle Appropriate to the design The main purpose of the components is to lead the water to the runner with minimum loss of energy. The runner of francis turbine Consists of series of curved vanes evenly arranged around the circumference in the annular transmitted to the generator through the shaft space between two plates. The torque produced by the runner is which is usually connected to the generator shaft by bolted flanged Connection. The water after passing through runner flows to the tail race through a draft tube PROCEDURE:i) Initially before starting the startup of Francis turbine priming process was completed. ii) Keep the gate opening initially at 50%. iii) Start the setup and keep the initial weight to zero. iv) Note down the corresponding values of spring balance weight, speed in rpm, manometer head and pressure gauge . v) Increase the weight successively as 1,2,3,4 and 5 kgs and take reading of corresponding values of all the above mentioned readings vi) Stop the setup and keep the gate openings at 60%. vii) Repeat the same procedure for 60% and 70% gate opening. 5 OBSERVATION TABLE: Sr.No PRESURE GAUGE(p) KG/CM2 VACCUM GAUGE SPEED (RPM) BREAK BALANCE SPRING BALANCE MANOMETER READING h1 h 2 h 50% GATE OPENING 60% GATE OPENING 70% GATE OPENING CALCULATION:H’(m) V’(M) T(M) Q(lpm) H(m) Input power Output power η% 50%GATE OPENING 60%GATE OPENING 70%GATE OPENING RESULT: The Working of Francis Turbine Has Been Studied. The average efficiency of the Turbine at different gate openings is found as follows: a. For 50%gate openings (η)= b. For 60% gate openings(η)= c. For 70%gate openings(η)= 6 NET WEIGHT EXPERIMENT NO :03 NAME OF THE EXPERIMENT: Determination of performance characteristics of Centrifugal Pump APPARATUS: Centrifugal Pump (Constant Speed), Scale, Stop Watch, etc. FIGURE: THEORY: The hydraulic machines, which convert the mechanical energy into hydraulic energy, are called pumps. The hydraulic energy is in the form of pressure energy. If the mechanical energy is converted into pressure energy by means of centrifugal force acting on the fluid, the hydraulic machine is called as centrifugal Pump. The centrifugal pump act as a reversed of an inward radial form reaction turbine. This means that the flow in the centrifugal pumps is in the radial outward direction. The centrifugal pump works on the principle of forced vortex flow which means that when a certain mass of liquid is rotated by an external tongue, the rise in pressure head of rotating liquid takes place. The rise of pressure head at any point of rotating liquid in proportional to square of tangential velocity of the liquid at that point. Main Parts of Centrifugal Pump. The following are the main parts of the centrifugal pum 1. Impeller : The rotating part of a centrifugal pump is called impeller. It consists of a series of backward curved vanes. The impeller is mounted on shaft which is connected to the shaft of an electric motor. 2. Casing: The casing of centrifugal pump is an air tight passage surrounding the impeller and is designed in such a way that the kinetic energy of the water discharged at the outlet of the impeller is converted into pressure energy before the water leaves the casing and enters the delivery pipe. The following 3 types of casings are a). Volute casing b). Voter casing c). Casing with guide blades. 3. Suction Pipe with a foot valve and strainer: A pipe whose one end is connected to the inlet of the pump and other end dips into water in a sump is known as suction pump. A foot valve which is non-return valve or one way type of valve is fitted at the lower end of suction pipe. The foot valve is open only in the upward direction. A strainer is also fitted at the lower end of the suction pipe. 7 4. Delivery Pipe : A pipe whose one end is connected to the outlet of the pump and other end delivers the water at required height is known as delivery pipe Head and efficiencies of Centrifugal Pump 1. Suction Head: It is the vertical height of the center line of a centrifugal pump above the water. This is called the suction head, denoted by “hs 2. Delivery Head : The vertical distance between the center line of the pump and water surface in the tank to which water is delivered is known a delivery head denoted by hd. 3. Static Head : The sum of suction head and delivery heads is known as static head. This is represented by Hs and given by Hs = hx + hd 4. Manometer Head : The manometric head is defined as the head against which a centrifugal pump has to work and is denoted by “Hm”. Efficiencies of Centrifugal Pump In case of centrifugal pump, the power is transmitted from the shaft of the electric motor to the shaft of the pump and then the water. The following are the efficiencies of centrifugal pump A. Manometer Efficiency ( Man) : The ratio of the manometric head to the head imparted by impeller to the water in m as manometric efficiency. Man 9 Hm vw H 2 B. Mechanical Efficiency ( m) : The power of the shaft of the centrifugal pump is more than the power available to the impeller of the pump. The ratio of power at the centrifugal pump is known as mechanical efficiency m = Power at the impeller. C. Overall Efficiency( 0) : It is defined as the ratio of power output of the pumnp to the power input to the pump. The power output of the pump Weight of water lifted x Hm 1000 0 = S.P. WHm [ ] 1000 0 = S.P 0 = mano x m x v 8 PROCEDUR: 1. Open the suction valve in the inlet pipe 2. Prime the pump by pouring water into collecting tank and suction pipe till it get full 3. Close the outlet valve of the delivery pipe 4. Open the delivery valve fully for maximum discharge 5. Note the pressure guage reading on the delivery side and record 6. Record the time in seconds for 10 revolutions of the energy meter 7. Note the vaccum guage reading on the suction side and not 8. Measure the internal dimensions of the collecting tank OBSERVATION: Pressure gauge readings Sr.No Discharge Pd (m3/s) (kg Pd Hd (m) /cm2) (kg Hd (m) /cm2) Wattmeter Manometric readings Head Hm X (watts) (m) Output Input Pi P0 (H.P.) (H.P.) 0 CALCULATION: Perform the Following Calculation for each opening of the delivery Valve 1. Vd = 2. Hd = Q ( / 4)d s 2 ; Vs = Q ( / 4)d s 2 P Pd ; Hs = s w w 3. Hm Form eqn. (1) 4. P0 = wQHm H .P 75 5. Pi = P0 100 Pi RESULT: The efficiency of the centrifugal pump is found to be ------------. 9 EXPERIMENT NO 04 NAME OF THE EXPERIMENT: Determination of performance characteristics reciprocating pump . APPARATUS: Reciprocating pump setup, collecting tank, suction gauge, delivery gauge, stopwatch. FIGURE: THEORY : The theoretical discharge can be calculated by formula: Qth Where, ALN 60 Qth = Theoretical discharge A = area of cylinder L=length of piston rod N=speed of motor Percentage of slip can be calculated as % slip = ( Oth - Qact )/ Qth %η = Input X100 Output PROCEDURE:i) Open fully the gate valve in the delivery pipe ii) Keep the field resistance of the rheostats in the minimum resist position (i.e. for minimum speed) start the motor. iii) Adjust core shaft by varying the field rheostat. iv) Adjust the gate valve to get the required head. v) Note the following a) Pressure and vacuum gauge reading b) Voltmeter and ammeter reading c) Height of pressure gauge (m) above vacuum gauge vi) Take some more sets of reading by varying the head 10 OBSERVATIONS: Dia Of Cylinder = length of piston rod= speed of motor =N= area of collecting tank= OBSERVATION TABLE:SR.NO t Qa Qth Cd T OBSERVATION TABLE HS Hd Po ηo %Slip Pi CALCULATIONS:volume 1. Qa= Time 2. Qth ALN Qth - Qact = % slip = 60 Qth RESULT: The following results are obtained a. coefficient of discharge = b. overall efficiency of pump = c. percentage slip = 11 EXPERIMENT NO.05 NAME OF THE EXPERIMENT: Study of flow around immersed bodies by Hele Shaw Apparatus APPARATUS: 1. Hele-Shaw apparatus 2. The object around which the flow pattern is to be determined. 3. Dye, tracing paper and water supply. The Hele-shaw apparatus consists of two closely spaced parallel, transparent flat plates. The narrow gap is of the order of 1.5 mm. They are connected to small transparent reservoirs at two opposite ends one being the unlit reservoir and the other out reservoir. At the other two sides the gap is sealed at the edges by means of clamps to prevent outflow. The level of liquid in both the inlet and outlet reservoirs is maintained as steady during the experiment. An arrangement for injection of dye is provided at various equally spaced points on the inlet side. The object around which the flow pattern is to be determined is placed centrally in the gap between the plates. When the dye is injected in the flow between the plants, the dye filaments form streamlines depicting the flow pattern around the object. FIGURE: THEORY: In order to understand flow of complex nature it is often necessary to have a mental picture of the qualitative pattern of the flow this can be obtained by means of flow visualization techniques. One such technique, developed by Hele shaw, stimulates the streamline patterns of two dimensional flow based on the principle of viscous flow between parallel plates. It is well known that any acting forces. The apparatus developed by Hele Shaw takes advantage of this fact to trace streamlines in two dimensional flows. 12 PROCEDURE: 1. Insert the object between the plates centrally. 2. Put water in the inlet reservoir and let it flow through the gap between the parallel plates unlit the inlet and outlet reservoirs attain steady levels. 3. Introduce dye into the flow and wait until a well defined pattern of streamlines is observed 4. Fix a tracing paper over the glass plate, between the inlet and outlet reservoir and trace the pattern of the streamlines and the geometry of the given object. RESULT The flow around immersed bodies by Hele Shaw Apparatus is studied PRECAUTIONS 1. Ensure that the levels of the liquid in the inlet and outlet reservoirs remain steady while plotting the flow of pattern. 2. Keep the rate of flow between the plates very low 13 EXPERIMENT NO :06 NAME OF THE EXPERIMENT: Determine of the Darcy-Weisbach Friction Factor for a given pipe. APPARATUS: U – tube manometer connected across a pipe line, Stop Watch, Collecting tank . FIGURE: FORMULA: Head loss due to friction in pipe 4flv 2 Flv 2 OR hf 2gd 2gd Where, F = friction factor = (4f) l = length of pipe V = Velocity of flow through pipe. d = Diameter of pipe. g = Acceleration due to gravity. f = Coefficient. of friction THEORY: The experimental set up consists of a large number of pipes of different diameters. The pipes have tapping at certain distance so that a U – Tube manometer is connected in between them. The flow of water through a pipeline is regulated by operating a control valve which is provided in main supply line, for measuring the head loss. The length of the pipe is considered as a distance between the two pressure tapping, to which a U – Tube mercury manometer is fitted. Actual discharge through pipeline is calculated by collecting the water in collecting tank and by noting the time for collection. Velocity of flow = V Q ( A / t) = a a Where, A = Area of tank. H = Depth of water collected in tank. t = Time required to collect the water up to a height “H” in the tank. a = Area of pipe. Q = Discharge through pipe. Now applying Bernoulli’s equation between two pressures tapping, we have. 14 PA P h p .g Z B ( Z hm ) m m w w w PROCEDURE : 1. Note down the diameter of pipe (d). 2. Note the density of manometric liquid (m) and that of fluid (water) flowing through a pipe i.e. (m). 3. Connect the U – tube manometer to the pipe in between two pressure tapings. 4. Start the flow and adjust the control valve in pipe line for required discharge. 5. Measure the pressure difference at two points A & B of a pipe by means of a U – tube manometer. 6. By collecting the water in collecting tank for a particular period of time. 7. Determine the velocity of flow (V) and frictional head loss (hf) by using appropriate equations. 8. Determine the friction factor (f) in pipe by using Darcy – Weisbach formula. 9. Change the flow rate by adjusting the control valve & repeat the process for at least five times. 10. Find out the mean friction factor (f) mean of the pipe. 11. Plot a graph of velocity of flow (V) on y – axis verses frictional head loss (hf) on x – axis which shows a straight line. OBSERVATION: 1) l = Length of Pipe = cm 2) d = Dia of Pipe = cm 3) Size of collecting tank = _______ x _______ cm2 4) m = Density of mercury = 13600 kg / m3 5) w = Density of water = 1000 kg / m3 15 OBSERVATION TABLE : Manometic Reading Left Right Sr.No Lim Lim Diff. b b (hBhA) HA HB Frictional Hedad Actual Tank Reading Loss Discharge p 1 hf hm m Diff. Time AH pm Initial Final H – Set Qac 2 t Height Height PA PB 3 H 1 M /Sec Meter hf Qw .g 1 2 3 4 5 Calculation: (d ) 2 1. a = c/s area of pipe = 2. A = Area of tank =-------------- 4 = 2 = _____ M2 4 For Reading No. 1 Frictional head loss = hf = hm Actual Discharge Qac = ----- M³ / sec Velocity of flow, V = Qac / a = ------ m / Sec F F 2hf .g .d lV 2 2hf .g.d hf .gh 4l.V 2 2lv 2 Result: The friction factor “ F ” for the pipe is found to be ________. 16 Velocity of flow Qac a M/Sec V Frict on factor F EXPERIMENT NO 7 NAME OF THE EXPERIMENT: Determine of Manning’s& chezy’s constant for an open channel.. APPARATUS: Standard tilting hydraulic flume. FIGURE THEORY: In 1989, Robert manning’s presented a formula according to which the mean velocity of uniform flow in a channel is expressed in terms of a coefficient of roughness ‘n’ called manning’s “n” hydraulic radius and channel bottom slope so .the manning’s formula expressed is in m TYPE OF CHANNEL BOUNDARY SURFACE Very smooth concrete and planed timber Smooth concrete Glazed brickwork Good wood Vitrified clay Brick surface lined with cement mortar Cement concrete finish VALUE OF ‘n’ 0.01 0.011 0.012 0.013 0.013 0.014 0.014 0.015 0.015 Unified cement surface 0.017 Earth channel in best condition Neatly excavated rock 0.017 0.02 Straight unlined earth canals in good condition Rubble masonary Corrugated metal surface 0.02 0.02 0.02 Rivers and earth canals in fair condition Earth channel with gravel bottom Earth channel eith dense weed Mountain stream with rock beds and rivers with variable section and some vegetation 17 0.025 0.025 0.035 0.045 FORMULA :Discharge Q = A Discharge Q= AX V Q A C R SO V C R SO PROCEDURE: 1) Set the flume at the suitable bed slope(so) 2) Measure width B of the flume. 3) Take manometer readings for the measurement of discharge. 4) Open the inlet valve of the flume and allow water to flow through --------5) Take the manometric readings 6) Measure depth of flow at three different locations (y1,y2,y3) 7) Repeat the steps from 4 to 6 for different discharges. OBSERVATIONS TABLE: Manometer reading LHS RHS x H=12.6x Q= K√H Y1 Y2 Y3 Yavg Observations table: A = Bx y P=B+2y R = A/P C n RESULT: for the flow range of ______m3/sec to ________m3/sec through a open channel with width B= and bed slope SO______, the Chezy’s constant “c “and Manning’s constant “‘n’ are as follows: ‘c’=______ ‘n’=_______ 18 EXPERIMENT NO 08 NAME OF THE EXPERIMENT: Developing specific energy diagram for rectangular channel APPARATUS: Venturiflume FIGURE THEORY: A channel may be defined as a passage through which water flows under atmospheric pressure as such in channels the flow of water take place with a free surface which is subjected to atmospheric pressure. The channels without any cover at the top are known as open channels In case of long channels often it becomes necessary to provide transitions. A transition is the portion of a channel with varying cross sections, which connects one uniform channel to other which may or may not have the same cross section form. The variation of channels section may be caused either by reducing or increasing width Or by raising or lowering bottom of channel The critical depth of flow may be obtained at certain section in an open channel where the channel bottom is raised by the construction of low hump or the channel is constructed by reading its width. Since at critical state of flow, the relationship Between depth of flow and discharge is definite and is independent of channel roughness And other uncontrollable factors, it provides a theoretical basis for the measurement of Discharge in open channel device which is commonly used for measurement of flow in open channels is known as venturiflime Venturiflume as shown in figure is a structure in a channel which has a contracted section called throat downstream of which follow a flared transition section. Designed to restore the stream to its original width. At the throat section there will be a drop in the water surface and this drop may be related to discharge the velocity of flow at the throat is always less than the critical velocity and hence the discharge passing through it will be a function of the difference between the depth of flow upstream of the entrance section and at the throat. Since the velocity of flow at the throat is less than critical velocity hydraulic jump will not be formed. Where, Q KAa 2 g ( H h) A2 a 2 Where, A and a are areas & H and h are depth of flow section at entrance and throat of flume. K=discharge coefficient of flume. 19 For rectangular channels the above eqn becomes Qk BH 2 g h h ( BH ) 2 (bh) 2 In which B and b are bottom width at entrance and throat respectively Tilting flume can also be used to determine chezy’s constant and manning’s constant With the help of flume velocity can be determined by knowing discharge and area Where area is a function of B and y, R can also be determined as R=A/P and bed slope can also be easily determined. Hence by performing various trials by varying discharge The value of c can be determined. Similarly manning’s constant can also be determined by V 1R 2 / 3 S 1 / 2 here too the value of V,R,S can be known and hence by experiments the value of n can be determine Development of specific energy curve can also be done by using this experiment. Since the free surface in case of channel flow represents the hydraulic gradient. Bernoulli’s equation can be applied between the section 1 and 2 which are L distance apart V 12 Y1 Z1 V 2 2 Y 2Z 2 ht 2g 2g hf = energy loss between two sections specific energy is the sum of the depth of flow at any section and velocity head Y V 2 Q2 E 2g 2GA2 Since V= Q/A E =function of depth Thus for given channel section and discharge eqn May be represented graphically In which specific energy is plotted along x axis and depth of flow on y axis the curve so obtained is called specific energy curve RESULT: The working of tilting flume is studied 20 EXPERIMENT NO. 09 NAME OF THE EXPERIMENT: Study of Gradually varied flow profiles APPARATUS: Venturiflume FIGURE THEORY: Open channel flow is characterized by existence of a free surface is atmospheric and is constant throughout the flow takes place due to gravity. Channel flow gradually varied flow:- (non uniform flow) Gravity force produces flow with continuously increasing velocity. The frictional resistance increases with velocity whereas gravity force is constant when there two exactly balance each other uniform flow occurs. CLASSIFICATION OF SURFACE PROFILES:The various water surface profiles occurring in the channel are designated with reference to the bottom slopes of the channel viz. M curve, S curve etc. They are further classified depending upon the relative position of actual depth (y) and the critical depth (yc) a shown below. For mild slope channel:Zone (i) dy/dx = +ve Where, y = yn, dy/dx= 0 When y = ∞, dy/dx = So Zone (ii) dy/dx = -ve (Yn >y > Yc) When, y = Yc dy/dx = ∞, When, y = Yn , dy/dx = 0 Zone (iii) dy/dx = +ve When y=Yc, dy/dx = ∞, Y= 0, dy/dx = 0 For steep slope channel (Yn<Yc) Zone (i) dy/dx = +ve When, y=Yc, dy/dx = ∞, Y= ∞,, dy/dx = So 21 Zone (ii) dy/dx = -ve When, y= Yn, dy/dx = 0 Y=Yc, dy/dx = ∞, Zone (iii) dy/dx = +ve When, y = Yn, dy/dx =∞, Y =0 dy/dx = 0 Similarly for Critical slope(Yn=Yc) Zone (i) y > Yn, dy/dx = +ve When, y = Yc, dy/dx = So = Sc Y = ∞, dy/dx= So =Sc Zone (ii) y < Yc = Yn, dy/dx = =ve As y= Yc dy/dx = So= Sc Y = ∞, dy/dx= So =Sc (iii) Horizantal slope channel (iv) Adverse slope profile can also be obtained in similar manner. DYNAMIC EQUATION FOR GVF Assumptions:Flow is steady ( Q is constant) Pressure distribution is hydrostatic. Loss of head due to friction is as per uniform condition i.e. Mannings and Chezy’s equation can be used to calculate the slope energy line in GVF as well Bed slope is small Channel is prismatic Velocity distribution does not changes (α = 1) Roughness coefficient n is constant and it does not depend on the flow depth. Total head H= z+y+v2/2g Differentiating with respect to x dH/dx =dz/dx +dy/dx +d (v2/2g)/dx -Sf = -So +dy/dx +d/dx(v2/2g) multiply the velocity term by dy / dy 22 dy/dx+ d/dx(v2/2g)dy/dy = So – Sf dy / dx = (So – Sf) ÷ (1+ d/dy[v2/2g])……………….(1) equation 1 is dynamic equation of GVF which gives variation of depth y w.r.t.distance along the bottom of the channel x. If dy/dx = 0 (uniform Slope) If dy/dx = +ve (y increases with x , back water curve) If dy/dx = -ve (y decreases with x, drawdown curve) Alternative form of equation (i) V = Q/A d/dy (v2/2g) = d/dy (q2 / {A2 x 2g) dy / dx = (So – Sf) ÷ (1- Q2T/gA3)………………………(ii) Fr2 = Q2 T /gA3 Dy / dx = (So – Sf ) ÷ (1- Fr2 ) Sf / So = (Ko / K)2 Q=√(S) Dy/dx = So (1- (Kn/K) 2 )÷ ( 1- (Zc/Z) 2 ) The final genral form of GVF equation is as follows:Dy / dx = So (1- (Yn/Y)n ÷ (1 – (Yc / Y )) CLASSIFICATION OF CHANNEL SLOPES:i) Mild slope Yn > Yc ii) Step slope--- Yn < Yc iii) Critical Slope -- Yn = Yc iv) Horizontal slope -- So = 0 v) Adverse Slope --- So = -ve Some of the possible water surface profiles are shown in the sketch i) Mild slope followed by a steep slope ii) Steep slope followed by a mild slope iii) Horizontal slope channel followed by steep slope iv) Steep followed by horizontal ending in free fall RESULT:-Gradually varied flow (GVF) profiles have been studied. 23 EXPERIMENT NO.10 NAME OF THE EXPERIMENT: Study of Hydraulic jump in a rectangular channel APPARATUS: 1. A glass Walled rectangular channel of sufficient length equipped with head and tail gates. 2. A pointer gauge which can be moved along the length of the channel on top rails provided on the side walls. 3. A regulated water supply with a discharge measurement unit in the supply line. FIGURE THEORY In an open channel when rapidly flowing stream abruptly changes to slowly flowing stream, a distinct rise or jump in the elevation of liquid surface takes place, this phenomenon is know as distinct rise or jump in the elevation of liquid surface takes place this phenomenon is know as hydraulic jump. The hydraulic jump converts kinetic energy of stream rapidly flowing into potential energy. Due to this there is a loss of kinetic energy. At the place where hydraulic jump occurs rollers of turbulent water form, which cause dissipation of energy. A hydraulic jump occurs in practice at the toe of spillways or below a sluice gate where the velocity is very high. y1 1 1 8( Fr1 ) 2 1 y2 2 Where, Fr1 = V1 gy1 Froude’s number corresponding to the pre-jump depth. The other elements of the jump Height of jump, H j = y2 – y1 Length of jump, L j 5Hj Loss of energy head occurring in the jump, EL= ( y 2 y1 ) 3 4 y1 y 2 PROCEDURE : 1. Take point gauge reading corresponding to the bed level of the channel (y0). 2. Open the supply valves fully and allow the water to flow in the channel. Allow the flow to stabize, and measure the discharge Q actual with the help of orifice meter. 3. Adjust the depth of flow with the help of head gate such that it is less than the critical depth i.e. Fr1>1 24 4. Adjust the height of tailgate to set up a hydraulic jump approximately midway along the channel. 5. Let the jump stabilize and take the pointer readings corresponding to the water surface just upstream (y1’) and downstream (y2)of the jump 6. Measure the length of the jump Lj 7. Repeat steps 3 to6 for different values of Fr1 always keeping it greater than one adjusting the opening of the head gate. OBSERVATIONS Pointer gauge readings Discharge S.No ( / S ) y1 3 Q (cm) y2 Initial Sequent Height of Length depth depth jump of jump y1(cm) y2(cm) Hj =( y1- y2) Lj (cm) (y2/y1) (y2/y1) act th. (cm) CALCULATION: 1. Initial depth , y1 = y1 ‘-y0 ,and Final Depth y2 ‘-y0 y 2. 2 y Using y1 and y2 calculated aborut. actual 3. Fr1 Q B gy 3 4. Hj = y1- y2 5. E L ( y1 - y 2 ) 3 4y1 y 2 6. Plot the following curves y2/y1 vs Fr1 L/y2 vs Fr1 EL vs Fr1 RESULT:PRECAUTIONS:1. Pointer gauge readings must be taken only after the jump stabilizes. 2. Pointer gauge readings upstream and downstream of the jump should be taken at the section where the water surface is tranquil. 25