lOMoARcPSD|23181365 MAAE 2300 - Flow Through a Sluice Gate and Hydraulic Jump Report Fluid Mechanics I (Carleton University) Studocu is not sponsored or endorsed by any college or university Downloaded by mehmet basari (mortalcombact69@gmail.com) lOMoARcPSD|23181365 - CARLETON UNIVERSITY - Experiment 3: Flow Through a Sluice Gate and Hydraulic Jump Summary: Downloaded by mehmet basari (mortalcombact69@gmail.com) lOMoARcPSD|23181365 This laboratory report analyzes Experiment 3: Flow Through a Sluice Gate and Hydraulic Jump, during which a hydraulic jump was created by the flow of water passing from a sluice gate, through a channel, and contacting an end barrier. The experiment was performed by measuring the water flow heights at three different points along the channel, that is, before, at, and after the jump. Before the jump, the flow of the water was classified as supercritical and after the jump, it was classified as subcritical. This ultimately demonstrated that the flow type conversion was induced by the jump. The purpose of this laboratory is to verify the course techniques of flow prediction as discussed throughout MAAE 2300. Nomenclature: V1 = Upstream velocity, inside tank (m/s) VT2 = Theoretical downstream velocity, preceding jump (m/s) VA2 = Experimental downstream velocity, preceding jump (m/s) V3 = Velocity after jump (m/s) P1 = Upstream flow pressure, inside tank (Pa) P2 = Downstream flow pressure, preceding jump (Pa) Patm = Atmospheric pressure (101 325 Pa) ρ = water Density of water (1 000 kg/m3) A1 = Area of upstream cross section, inside tank (m2) A2 = Area of downstream cross section, preceding jump (m2) Q = Flow rate (m3/s) H1 = Upstream head, inside tank (m) H2 = Downstream head, preceding jump (m) H3 = Downstream head, following jump (m) h1 = Upstream flow height, inside tank (m) h2 = Downstream flow height, before jump (m) h3 = Downstream flow height, following jump (m) w = Channel width (6.25 in) Flow Analysis: Downloaded by mehmet basari (mortalcombact69@gmail.com) lOMoARcPSD|23181365 Bernoulli’s Equation relates the stagnation, static, and statics pressures of two given points along a stream line of flow: 1 1 P1+ ρV 21 + ρg z 1=P2 + ρV 22 T + ρg z 2 2 2 (Eq. 1) Conservation of momentum demonstrates that the mass flow rate of water at any given point throughout the system is equivalent. This implies that, since the density is constant throughout the system, the velocity of flow and area through which flow passes are inversely proportional: ḿ1=ḿ2 (Eq. 2) The following equation is used to calculate the total head, or total mechanical energy, at any given point throughout the system: (Eq. 3) Volumetric Flow Equation: Q= A 2 V 2 (Eq. 4) Experimental Setup: [3] [1] [2] Experimental Procedure: Executed procedure was consistent with instructed procedure from MAAE 2300 Fluid Mechanics I Laboratory Exercises manual. No changes were made. Results and Discussion: Downloaded by mehmet basari (mortalcombact69@gmail.com) lOMoARcPSD|23181365 Flow 1 Flow 2 Position Flow Flow Head Flow Flow Head Height (m) (m) Height (m) (m) V-Notch 0.140335 N/A 0.140462 N/A [1] 0.4810125 0.4810125 0.180975 0.1825625 [2] 0.0277368 0.4191 0.048768 0.1524 [3] 0.173736 0.1778 0.1164336 0.13335 Refer to MAAE 2300 Fluid Mechanics I Laboratory Exercises, Analysis and Discussion section. 1.0 Determining the theoretical downstream velocity, preceding jump, VT2: 1.1.1 Conservation of Momentum Equation (Eq. 2) is expanded to find upstream velocity, inside tank (V1): ḿ1=ḿ2 ρw A 1 V 1 =ρw A 2 V 2 A2V 2 V 1= A1 whV 2 V 1= wh1 h2 V 2 V 1= h1 1.1.2 Downstream velocity, following jump, V2, is unknown. This is found using Bernoulli’s Equation (Eq. 1): 1 1 2 2 P1+ ρV 1 + ρg z 1=P2 + ρV 2 + ρg z 2 2 2 1 1 Patm + ρ V 21 +ρg z 1=Patm + ρ V 2T 2 + ρg z 2 2 2 1 2 1 V 1+ g z 1= V 2T 2 +g z 2 2 2 1.1.3 Variable substitutions are made; h1 and h2 for z1 and z2 respectively as well as V1 for the above expression: Downloaded by mehmet basari (mortalcombact69@gmail.com) lOMoARcPSD|23181365 2 1 h2 V 2 1 ( ) + g h1 = V 2T 2 +g h2 2 h1 2 2 h V 2 −( 2 2 ) −2 g h1+2 g h2=−V 2 h1 ( ) h2 V T 2 2 2 g h 2−2 g h1 = −V 2T 2 h1 ( ) h2 2 2 g ( h2−h1 ) =V ( −1) h1 2 T2 V T 2= √( ) 2 g ( h2−h1 ) h2 2 −1 h1 The known variables are substituted into the above equation to determine VT2 (refer to Appendix B): Flow 1: VT2 = 2.99 m/s Flow 2: VT2 = 1.67 m/s 1.2 Determining the experimental downstream velocity, preceding jump, VA2: 1.2.1 Volumetric Flow Rate Equation (Eq. 4) is used to determine VA2: Q= A 2 V A 2 1.2.2 MAAE 2300 Fluid Mechanics I Laboratory Exercises provides that Q=1.38 H 2.5 : A 2 V A 2=1.38 H 2.5 V A 2= 1.38 H 2.5 A2 V A 2= 1.38 H wh2 2.5 The known variables are substituted into the above equation to determine VA2 (refer to Appendix B): Downloaded by mehmet basari (mortalcombact69@gmail.com) lOMoARcPSD|23181365 Flow 1: VA2 = 1.71 m/s Flow 2: VA2 = 0.054 m/s Both Flow 1 and Flow 2 trials demonstrate the experimental downstream velocities, preceding the jump, are lower than their theoretical values. This trend is to be expected due to the unideal conditions in which this experiment was performed. Friction from the water’s contact with the channel walls and floor would be the main factor here, as well as turbulent flow throughout the system. 2. Determining and comparing the total heads measured inside tank and in supercritical flow, H1 and H2: 2.1 Determining total head of supercritical flow, H1: 2 P VT1 +h1 H 1= + ρg 2 g Flow 1: H 1=1.22 m Flow 2: H 1=0.97 m 2.2 Determining total head of subcritical flow, H2: 2 P V H 2= + T 2 +h2 ρg 2 g Flow 1: H 2=1.23 m Flow 2: H 2=0.99 m The theoretical head totals are higher than the experimental head totals, however the trend remains the same; there is only a slight increase of head totals before and after the sluice gate. 4. Calculating the total head change across the hydraulic jump for between each flow before jump and the flow after the jump: 4.1 Total head of flow inside tank, H1: Downloaded by mehmet basari (mortalcombact69@gmail.com) lOMoARcPSD|23181365 2 P V H 1= + T 1 +h1 ρg 2 g Flow 1: H 1=1.23 m Flow 2: H 1=0.97 m 4.2 Total head of supercritical flow, H2: H 2= P V 2T 2 + +h2 ρg 2 g Flow 1: H 2=1.22 m Flow 2: H 2=0.99 m 4.2 Total head of subcritical flow, H1: H 3= √ H2 h 2Q22 + 3+ 2 4 g w2 h2 Flow 1: H 2=0.91 m Flow 2: H 2=0.64 m 4.4 The average total head change across the hydraulic jump: Flow 1: dH =0.315 m Flow 2: dH =0.34 m Conclusions: This laboratory experiment has demonstrated a directly proportional relationship between head totals at any given point in a flow. However, assumptions made in order to use the simplified equations developed in the MAAE 2300 course, such as frictionless surfaces and laminar flow, result in inaccuracies between experimental and theoretical flow data. Appendix A: Downloaded by mehmet basari (mortalcombact69@gmail.com) lOMoARcPSD|23181365 Appendix B: Downloaded by mehmet basari (mortalcombact69@gmail.com) lOMoARcPSD|23181365 Downloaded by mehmet basari (mortalcombact69@gmail.com)