Fluid Flow or Discharge • When a fluid that fills a pipe flows through a pipe of cross-sectional area A with an average velocity v, the flow or discharge Q is determined by: Q Av Equation of Continuity • Suppose an • incompressible (constant density) fluid fills a pipe and flows through it. If the cross-sectional area of the pipe is A1 at one point and A2 at another point, the flow through A1 must equal the flow through A2. Q A1 v1 Q A2 v2 A1 v1 A 2 v 2 Equation of Continuity • The equation of continuity in the form A1 v1 A 2 v 2 applies only when the density of the fluid is constant. If the density of the fluid is not constant, the equation of continuity is D1 A1 v1 D2 A 2 v 2 • mass flow rate (units kg/s): m D A v t • volume flow rate (units m3/s): V A v t Equation of Continuity • The equation of continuity shows that where the • cross-sectional area is large, the fluid speed is slow and that where the cross-sectional area is small, the fluid speed is large. This explains why water shoots out of a hose faster when you place your thumb across the opening, reducing the cross-sectional area through which the water can come out. Viscosity and Viscous Flow • Viscosity h of a fluid is a measure of how difficult it is to cause the fluid to flow. • In an ideal fluid there is no viscosity to hinder the fluid layers as they slide past one another. • Within a pipe of uniform cross-sectional area, every layer of an ideal fluid moves with the same velocity, even the layer next to the wall. Viscosity and Viscous Flow • When viscosity is present, the fluid layers do not all have the same velocity. – The fluid closest to the wall does not move at all, while the fluid at the center of the pipe has the greatest velocity. – The fluid layer next to the wall surface does not move because it is held tightly by intermolecular forces. – The intermolecular forces are so strong that if a solid surface moves, the adjacent fluid layer moves along with it and remains at rest relative to the moving surface. Viscosity and Viscous Flow • This is why a layer of dust lies on the • surface of fan blades even at high speeds. The layer of air in contact with the fan blade has no velocity relative to the fan blade and does not blow off the dust. Force F needed to move a layer of viscous fluid with constant velocity: – – – – h = viscosity η A v F A = area d v = velocity d = distance from the immobile surface Viscosity and Viscous Flow • Viscosity of liquids and gases depend on temperature. – Usually, the viscosities of liquids decrease as the temperature increases. – The viscosities of gases increase as the temperature increases. • Viscous fluids have a high viscosity, such as tar and molasses. Forces Exerted By a Fluid • If a fluid were subjected to a tangential force F, the layers of the fluid would slide past one another without friction. • This means that a fluid can sustain only a perpendicular force, and conversely, can exert only a force perpendicular to the surface. •If a fluid were subjected to a tangential force F, the layers of the fluid would slide past one another without friction. •This means that a fluid can sustain only a perpendicular force, and conversely, can exert only a force perpendicular to the surface. Forces Exerted By a Fluid • Suppose that a nonelastic fluid is between 2 plates. If the velocity v of the upper plate is not too large, the fluid shears in the way indicated. The viscosity h is related to the force F required to produce the velocity v by: vA η F d Forces Exerted By a Fluid • A = area of either plate • d = distance between • • • plates units for h: N·s/m2 or kg/m·s or lb· s/ft2 1 poiseuille (Pl) = 1 N·s/m2 = 1 kg/m·s 1 poise (P) = 0.1 kg/m·s Poiseuille’s Law • The fluid flow through a cylindrical pipe of length l and cross-sectional radius r is given by: 4 π r (P1 P2 ) Q 8 η l • P1 - P2 is the pressure difference between the two ends of the pipe. Work Done by a Piston • Work done by a piston in forcing a volume V of fluid into a cylinder against an opposing pressure P is given by: W = P·V Bernoulli’s Principle • If a fluid is incompressible - a change in pressure does not cause a change in volume - the volume of fluid entering per second must equal the volume leaving per second. V1 V2 Volumetric flow rate: t t 1 = entering 2 = leaving Let v represent the speed with which a liquid moves in a cylindrical pipe, so that during the time t the liquid moves a distance equal to v·t (where v is velocity. Bernoulli’s Principle • The volume of liquid passing a cross-sectional area A is given by V Avt • Volumetric flow rate Q: V Q Av t • Because the liquid is incompressible, the • volumetric flow rate is the same entering and leaving the system. Volumetric flow rate (system): A v A v 1 1 2 2 Bernoulli’s Principle • 2 0 . 5 D v h D g P has the same The quantity value at every point in an incompressible fluid moving in streamline (non-turbulent) flow. • Bernoulli’s equation: 0.5 D v12 h1 D g P1 0.5 D v 22 h2 D g P2 Bernoulli’s Principle • If the fluid is not moving, then both speeds are zero. The fluid is static. If the height at the top of the column is h1 is defined as zero, and h2 is the depth, then Bernoulli’s equation reduces to the equation for pressure as a function of depth: P1 P2 D g h2 • If the fluid is flowing through a horizontal pipe with a constriction, as shown in the figure on the next slide, there is no change in height and the gravitational potential energy does not change. Bernoulli’s equation reduces to: P1 2 0.5 D v1 P2 0.5 D v 2 2 1 1 2 2 P1 h1 D g D v1 P2 h 2 D g D v 2 2 2 Work per unit volume done by the fluid Potential energy per unit volume Kinetic energy per unit volume Points 1 and 2 must be on the same streamline Bernoulli’s Principle • The flow rate Q in the tube has to be constant, therefore, the fluid has to move faster through the constriction to maintain the constant flow rate Q. • The velocity at point a is greater than at either the meter entrance or the meter exit. • The pressure in a fluid is related to the speed of flow, therefore the pressure in the fluid is less at point a and greater at the meter entrance, as illustrated by the liquid levels in the U-tube manometer. • The pressure difference is equal to: P hDg Bernoulli’s Principle • Bernoulli's principle describes the relationship between pressure and velocity in a fluid and describes the conservation of energy as it applies to fluids. • Bernoulli’s principle also explains why a roof blows off of a house in violent winds. – Wind creates a low pressure region above the peak of the roof, creating a pressure difference inside and outside the house which results in the loss of the roof. Bernoulli's Equation and Lift • The shape of a wing forces • • air to travel faster over the curved upper surface than it does over the flatter lower surface. According to Bernoulli’s equation, the pressure above the wing is lower (faster moving air), while the pressure below the wing is higher (slower moving air). The wing is lifted upward due to the higher pressure on the bottom of the wing. Bernoulli's Equation and Lift • Air flows over the top of an airplane wing of area A • with speed vt, and past the underside of the wing (also of area A) with speed vu. the magnitude FL of the upward lift force on the wing will be: 2 FL 0.5 D A v t v u • Ski jumpers use this same principle to help 2 themselves stay in the air longer during jumps. • A boomerang with a curved surface will turn in the direction of the curved face due to pressure differences created by the different air velocities over the two surfaces. Control surfaces on a plane • By extending the slats, the wing area A can be increased to generate more lift at low speeds for take off and landing. Curveball Pitch Torricelli’s Theorem • If an opening exists in a tank containing a liquid at a distance h below the top of the liquid, then the velocity v of outflow from the opening is: v 2 g h provided the liquid obeys Bernoulli’s equation and the top of the liquid may be regarded as motionless (v = 0 m/s). Tidal Waves • Tidal waves are the dissipation of energy in a viscous fluid over an inclined plane; tidal waves have nothing to do with tides. • The energy source is usually an under-sea earthquake (it could also be an under-sea explosion or a meteor strike); the viscous fluid is the ocean; the inclined plane is the ocean floor sloping upward toward land. • Earthquake: – When the Earth moves up and down it also moves the ocean water up and down. This generates a huge wave traveling outward in a series of concentric rings. – In deep water, most of the tidal wave (tsunami) remains hidden beneath the surface. But as the tidal wave moves toward more shallow water, its enormous energy is forced to the surface. – In the open ocean, tidal waves are hundreds of miles wide and travel at jetliner speeds. Near land they slow down to freeway speeds. – What makes a tidal wave so destructive is the speed and tremendous volume of water delivered onto a coastal or island environment as the tidal wave is forced by the inclining ocean floor onto the land. Bernoulli’s Principle and Syringes • The force applied to the plunger is equal to the • • • pressure times the area of the plunger. Viscous flow will occur within the barrel of the syringe and only a little pressure difference is needed to move the fluid through the barrel to point 2, where the fluid will enter the narrow needle. The pressure applied to the plunger is nearly equal to the pressure P2 at point 2. The pressure at point 1, P1, is also known as the gauge pressure. Bernoulli’s Principle and Syringes • Apply Bernoulli’s principle, 0.5 D v12 h1 D g P1 0.5 D v 22 h2 D g P2 and if the needle is held horizontally, P1 2 0.5 D v1 P2 0.5 D v 2 2 • Poiseuille’s Law may also be needed to solve this type of problem. P1 P2 8 η l Q πr 4 Bernoulli’s Principle and Siphons • A siphon is an inverted U-shaped pipe or tube that can transfer water from a higher container to a lower container by lifting the water upward from the higher container and then lowering it into the lower container. The water is simply seeking its level, just as it would if you connected the two containers with a pipe at their bottoms. In that case, the water in the higher container would flow out of it and into the lower container, propelled by the higher water pressure at the bottom of the higher container. In the case of a siphon, it's still the higher water pressure in the higher container that causes the water to flow toward the lower container, but in the siphon the water must temporarily flow above the water level in the higher container on its way to the lower container. Bernoulli’s Principle and Siphons • Two means of initiating the liquid flow (assume the liquid is water): – You can make a siphon using a rubber hose and gravity is the key to getting it to work. A siphon needs to have the "dry" end of the hose lower than the end that is stuck in the water (the "wet" end). You can get the siphon started by first filling the hose with water. Once the hose is full, use your thumb to plug the end of the hose that will be removed from the water. Place the “dry” end into the second container and then remove your thumb. Gravity does all the work from there... How does it work? Think of the water in terms of distinct “packets". Since the dry end of the hose is lower than the wet end, there are more water "packets" towards the dry end. As such, the column of water being pulled downward by gravity is heavier than the column of water at the wet end of the tube. Gravity pulls on one “packet" of water on the dry end of the tube causing it to move down the tube. As it moves, it creates a small vacuum behind itself. This vacuum pulls the next “packet” forward (downward) as well. This suction is strong enough to pull other “packets” up the tube (against gravity) at the wet end. Once a given “packet” passes the highest point in the tube, gravity pulls it downward and the process continues. The siphon will work as long as the vertical (up and down) column of water outside the container is larger than the vertical column inside the container. If the two ends of the hose are exactly the same height (the columns are equal), the pull of gravity will be the same on each side and the flow of water will stop. If you then lower the free end, the flow of water will begin once again. Bernoulli’s Principle and Siphons – Sucking on the lower end of the tube causes a partial vacuum (a region of space with a pressure that's less than atmospheric pressure) at the top of the siphon. The partial vacuum results in a difference in pressure between the bottom of the tube and the top of the tube. With greater fluid pressure at the top than the bottom, the water is pushed up into the tube and over to the lower container. The same kind of partial vacuum exists in a drinking straw when you suck on it and is what allows atmospheric pressure to push the beverage up toward your mouth. Bernoulli’s Principle and Siphons Bernoulli’s Principle and Siphons • To get water up to the top of the tube, need to reduce pressure in the tube so that the atmospheric pressure will do the work to push the fluid up to the top of the tube where gravity will do the work to pull the fluid out the end of the hose. • Apply Bernoulli’s equation between points A and B to determine the maximum height h1 to which water can be lifted above the water surface. 1 1 2 2 Patm h D g D vt PB h1 D g D vB 2 2 h 0 set top surface of water as 0 ; vt 0 PB 0 (want this to be as small as possible) vB vC 2 g (d h 2 ) to be explained soon Patm Patm Patm 1 h1 D g D 2 g (d h 2 ) 2 1 h1 D g D 2 g (d h 2 ) 2 h1 D g D g (d h 2 ) 2 Bernoulli’s Principle and Siphons • To determine the speed of the liquid flow at the bottom of the siphon, start with Bernoulli’s equation: 0.5 D v t 2 ht D g Pt 0.5 D v b 2 hb D g Pb • Atmospheric pressure is found at the top of the liquid and at the bottom of the siphon, therefore, Pt and Pb are equal and cancel out. • Consider the velocity vt at the top of the liquid to be 0 m/s. Bernoulli’s Principle and Siphons • Consider the lower end of the siphon to be the point at which the height is 0 m. From the figure, the distance from the bottom of the to the siphon to the upper level of the liquid is d + h2. (d h2 ) D g 0.5 D v b 2 • The density cancels out: (d h2 ) g 0.5 v b • Solve for vb: 2 v b 2 d h2 g Equation of Continuity Example • What is the flow rate of water in a pipe whose diameter is 10 cm when the water is moving with a velocity of 0.322 m/s? d 10 cm 0.1 m; r 0.05 m A π r 2 π 0.05 m2 0.007854 m2 m Q A v 0.007854 m 0.322 s 2 m3 Q 0.002529 s Equation of Continuity Example • If the diameter of Qleft Qright ; A L v L A R v R 2 2 the pipe to the π rL v L π rR v R right is reduced 2 2 to 4 cm, what is rL v L rR v R m 2 the velocity of 0.05 m 0.322 2 rL v L s the fluid in the vR 2 r R right-hand side of 0.02 m2 the pipe? m v R 2.0125 s Bernoulli’s Example • The pressure P1= 53913.24 N/m2, whereas the velocity of the water v1 = 0.322 m/s. The diameter of the pipe at location 1 is 10 cm and it is at ground level. If the diameter of the pipe at location 2 is 4 cm, and the pipe is 5 m above the ground, find the pressure P2 of the water at position 2. – From the previous example, we know that the velocity of the water at location 2 is 2.015 m/s. Bernoulli’s Example P1 h1 D g 0.5 D v12 P2 h 2 D g 0.5 D v 2 2 h1 0 m (ground level);D 1000 kg m3 P1 0.5 D v12 P2 h 2 D g 0.5 D v 2 2 P2 P1 0.5 D v12 h 2 D g 0.5 D v 22 2 kg m kg m P2 2940 2 0.5 1000 3 0.322 5 m 1000 3 9.8 2 s m m m s N 2 kg m 0.5 1000 3 2.015 s m N N N N P2 53913 .24 2 51 .842 2 49000 2 2030 .1125 2 m m m m N P2 2934 .97 2 m Helpful Online Links • Hyperphysics Fluids • Work-Energy Applet (to determine the power needed in the pump for the waterjet to pass over the wall) • Gallery of Fluid Mechanics