FLUID MECHANICS EC 311 DEFINITION • Fluid mechanics is the study of all aspects of the behaviour of fluids, either at rest (fluid statics) or in motion (fluid dynamics). • Fluid mechanics is involved in nearly all areas of civil engineering either directly or indirectly. AREAS OF APPLICATIONS OF FLUID MECHANICS Aerospace engineering applications include the design of aircraft, aerospace vehicles, rockets, missiles, and propulsion systems. Biomedical applications include the study of blood flow and breathing. Mechanical engineering applications include the design of plumbing systems, heating ventilation and air conditioning systems, lubrication systems, process-control systems, pumps, fans, turbines, and engines. AREAS OF APPLICATIONS OF FLUID MECHANICS Naval architecture applications include the design of ships and submarines. Aside from engineering applications of fluid mechanics, the earth sciences of hydrology, meteorology, and oceanography are based largely on the principles of fluid mechanics. AREAS OF APPLICATIONS OF FLUID MECHANICS • Fluid mechanics is also involved in nearly all areas of civil engineering either directly or indirectly. AREAS OF APPLICATIONS OF FLUID MECHANICS Direct application o o o o o o o o o Sea and river (flood) defences Water distribution/sewerage (sanitation) networks Hydraulic design of water/sewage treatment works Oil and gas pipelines Canals Dams Irrigation Pumps and turbines Water retaining structures APPLICATIONS OF FLUID MECHANICS Indirect application o Flow of air in or around buildings Determination of wind loads on buildings o Bridge piers in rivers o Groundwater flow CHARACTERISTICS OF FLUIDS • Three states of matter are recognized: i. Solid ii. Liquid Fluids iii. Gas • These differ in the spacing and latitude of motion of their molecules, these variables being large in a gas, smaller in a liquid, and extremely small in a solid. • Liquids and gases have a common characteristic in which they differ from solids: they are fluids, lacking the ability of solids to offer a permanent resistance to a deforming force. CHARACTERISTICS OF FLUIDS DEFINITION OF A FLUID • A fluid is a substance that deforms continuously when subjected to a shear stress, no matter how small that shear stress maybe. B B’ C φ F A D C’ F DIFFERENCES BETWEEN LIQUIDS AND GASES LIQUIDS GASES 1 Molecular movement is Molecular movement is restricated by cohesive forces unrestricated by cohesive forces 2 Has a fixed volume Incompressible Has free surface 3 4 Has no shape or volume Compressible Has no free surface THE CONTINUUM • Continuous distribution of matter with no empty space. • When the behaviour of a small element or particle of fluid is studied, it will be assumed that it contains so many molecules that it can be treated as part of this continuum. • Quantities such as velocity and pressure can be considered to be constant at any point, and changes due to molecular motion may be ignored. • Variations in such quantities can also be assumed to take place smoothly, from point to point. PROPERTIES OF FLUIDS • Density, ρ ‒ defined as mass per unit volume δm ρ = δlim V →ε δV ‒ In gases density is highly variable and it is nearly constant in liquids ‒ In gases density increases proportionally to the pressure level whereas in liquids it is considered independent to the pressure level ‒ Typical values at atmospheric pressure: water, 1000 kg/m3; air, 1.23 kg/m3. PROPERTIES OF FLUIDS Variation of densities of pure water with temperatures between 0oC and 100oC Density vs Temperature 1005 1000 995 990 Density (kg/m3) • 985 980 975 970 965 960 955 0 20 40 60 Temperature 80 (oC) 100 120 PROPERTIES OF FLUIDS Variation of densities of pure water with temperatures between 0oC and 10oC Density vs Temperature (0 - 10oC) 1000.0 1000.0 999.9 Density (kg/m3) • 999.9 999.8 999.8 999.7 999.7 999.6 0 2 4 6 Temperature (oC) 8 10 12 PROPERTIES OF FLUIDS • Specific weight, w or γ ‒ defined as weight per unit volume w = ρg ‒ Units: newtons per cubic metre (N/m3) ‒ Typical values: water, 9.81 x 103 N/m3 (9.81 kN/m3); air, 12.07 N/m3 PROPERTIES OF FLUIDS • Specific gravity, s.g ‒ defined as the ratio of density of a fluid to the density of a standard reference fluid, usually water at 4oC for liquids, and air for gases. ‒ For liquids ρ subs tan ce density of substance = s.g = o density of water at 4 C ρ water at 4o C PROPERTIES OF FLUIDS • Specific gravity, s.g Substance* Specific Gravity (SG) Substance* Specific Gravity (SG) Gold 19.3 Seawater 1.025 Uranium 18.7 Water 0.998 Mercury 13.6 SAE 10-W motor oil 0.92 Lead 11.4 Dense oak wood 0.93 Copper 8.91 Ice (0oC) 0.916 Steel 7.83 Benzene 0.879 Cast iron 7.08 Crude oil 0.87 Aluminium 2.64 Ethyl alcohol 0.790 Concrete (cured) 2.4 Gasoline 0.72 Blood (at 37oC) 1.06 Balsa wood 0.17 Example • Mercury has a density of 13600 kg/m3. What are its specific weight and specific gravity? PROPERTIES OF FLUIDS • Specific volume, v ‒ defined as the volume occupied by a unit mass of fluid. ‒ it is simply a reciprocal of density V 1 = ν = m ρ PROPERTIES OF FLUIDS • Temperature ‒ Temperature T is related to the internal energy level of a fluid. Engineers often use Celsius or Fahrenheit scales for convenience ‒ Many applications require absolute (Kelvin or Rankine) temperature scales. K = oC + 273.15 ‒ Where K and oC are temperatures in Kelvin and degree Celsius. PROPERTIES OF FLUIDS • Vapour pressure ‒ Defined as the partial pressure exerted by the vapour molecules on the liquid surface ‒ The vapour pressure of a given fluid depends on the temperature, and increases with increasing temperature ‒ Boiling of liquids occurs when pressure above the liquid equals the vapour pressure of the liquid ‒ In flowing liquids boiling would occur if the pressure of the liquid is reduced to below the vapour pressure PROPERTIES OF FLUIDS • Vapour pressure Vapour Pressure vs Temperature Vapour Pressure (kN/m2) 100 10 1 0 0.1 10 20 30 40 50 Temperature (oC) 60 70 80 90 100 PROPERTIES OF FLUIDS • Compressibility ‒ all matter is to some extent compressible ‒ compressibility of a perfect gas is described by the perfect gas law ‒ compressibility of liquids is described by the bulk modulus of elasticity, K ‒ In liquids, compressibility is only possible in situations involving either sudden or great changes in pressure PROPERTIES OF FLUIDS • Compressibility ‒ For liquids, bulk modulus of elasticity is given by ‒ δP K =− δV or K = V dP dρ ρ ‒ where δp = increase in pressure δV = decrease in volume ‒ Compressibility is the reciprocal of bulk modulus of elasticity PROPERTIES OF FLUIDS • Surface tension, σ ‒ Caused by the force of cohesion at the free surface ‒ At the free surface a thin layer of molecules is formed ‒ It is because of this film that a small needle can float on the free surface. ‒ Surface tension is usually expressed in N/m. ‒ Formation of bubbles, droplets and free jets are due to the surface tension of the liquid. PROPERTIES OF FLUIDS • Surface tension, σ PROPERTIES OF FLUIDS • Pressure inside a water droplet ‒ Liquids have a tendency of minimizing their surface area ‒ As such drops of liquid tend to take a spherical shape in order to minimize surface area PROPERTIES OF FLUIDS • Pressure inside a water droplet ‒ From free body diagram, we have π 2 i. Pressure force, F = P × d 4 ii. Surface tension force acting around the circumference = σ × πd ‒ Under equilibrium conditions these two forces will be equal and opposite i.e. P× π 4 d = σ × πd 2 4σ ⇒P= d Example • In order to form a stream of bubbles, air is introduced through a nozzle into a tank of water at 20oC. If the process requires 3.0 mm diameter bubbles to be formed, by how much the air pressure at the nozzle must exceed that of the surrounding water? Take surface tension of water at 20oC = 0.0735 N/m. PROPERTIES OF FLUIDS • Capillarity ‒ Rise or fall of a liquid in a capillary tube Causes of rise and fall cohesion ‒ when cohesion is greater than adhesion liquid level in a tube will fall adhesion ‒ when adhesion is greater than cohesion liquid level in a tube will rise PROPERTIES OF FLUIDS • Capillarity • Liquids rise in tubes they wet and fall in tubes they do not wet . PROPERTIES OF FLUIDS • Capillarity - wetting and contact angle This represents the case of a liquid which wets a solid surface well. The angle θ shown is the contact angle between the edge of the liquid surface and the solid surface. It measures the quality of wetting. For perfect wetting, in which the liquid spreads as a thin film over the surface of the solid, θ is zero. PROPERTIES OF FLUIDS • Capillarity - wetting and contact angle This represents the case of no wetting. If there was exactly zero wetting, θ would be 180o. PROPERTIES OF FLUIDS • Capillarity - height of capillary rise h= 4σ cos θ ρgd • Example Water has a surface tension of 0.4 N/m. In a 3 mm diameter vertical tube a liquid rises 6 mm above the liquid outside the tube, calculate the contact angle. PROPERTIES OF FLUIDS • Viscosity, μ ‒ property of a fluid which offers resistance to shear deformation ‒ resistance to shear deformation is achieved by cohesion and interaction between molecules ‒ the resisting forces are referred to as shear forces and these forces induce shear stresses in the fluid as a result of particle movement PROPERTIES OF FLUIDS • Viscosity, μ For a pipe in which water is flowing i. At the pipe wall the velocity of fluid particles is zero ii. At the centre of the pipe the velocity is maximum ‒ This way adjacent fluid particles will have different velocities • particles closer to the pipe boundary will move slower than the particles closer to the centre PROPERTIES OF FLUIDS • Viscosity, μ Velocity profile PROPERTIES OF FLUIDS • Viscosity, μ - Newton's law of viscosity PROPERTIES OF FLUIDS • Viscosity, μ - Newton's law of viscosity • F = shear force F F =τ • shear sress = = A δz × δx • Shear stress is measured by the deformation angle Φ, the shear strain x shear strain, φ = y PROPERTIES OF FLUIDS • Viscosity, μ - Newton's law of viscosity • Experimentally, shear stress is directly proportional to rate of shear strain rate of shear strain = u ⇒ τ = constant × y x u = ty y PROPERTIES OF FLUIDS • Viscosity, μ - Newton's law of viscosity • Proportionality constant is the viscosity, μ • In differential form du τ =µ dy τ = shear stress in N / m 2 du = velocity gradient dy µ = coefficient of dynamic viscosity PROPERTIES OF FLUIDS • COEFFICIENT OF DYNAMIC VISCOSITY • defined as the shear force per unit area, required to drag one layer of fluid with unit velocity past another layer a unit distance away du µ =τ / dy 2 • Units: Ns/m or Pa.s • Also Poise,P, 10P = 1Ns/m2 • Typical values: water, 1.14 x 10-3 Ns/m2, Air, 1.78 x 10-5 Ns/m2 PROPERTIES OF FLUIDS • KINEMATIC VISCOSITY • Kinematic viscosity, ν, is defined as the ratio of dynamic viscosity to mass density. µ ν = ρ • Units: square metres per second, m2/s • (Also expressed in stokes, st, where 104 st = 1 m2/s) • Typical values: water = 1.14 x 10-6 m2/s, Air = 1.46 x 10-5 m2/s, mercury = 1.145 x 10-4 m2/s, paraffin oil = 2.375 x 10-3 m2/s. Example 1 • The velocity distribution for flow over a plate is given by u = 2y – y2 where u is the velocity in m/s at a distance y metres above the plate. Determine the velocity gradient and shear stress at the boundary and 0.15m from it. Take dynamic viscosity of fluid as 0.9 Ns/m2. Example 2 • A hydraulic lift used for lifting automobiles has a 25 cm diameter ram which slides in a 25.018 cm diameter cylinder, the annular space being filled with oil having a kinematic viscosity of 3.7 cm2/s and relative density of 0.85. If the rate of travel of the ram is 15 cm/s, find the frictional resistance when 3.3 m of ram is engaged in the cylinder. NEWTONIAN AND NON-NEWTONIAN FLUIDS • NEWTONIAN FLUIDS ‒ Fluids which obey Newton’s law of viscosity. ‒ All gases and most liquids which have simpler molecular formula and low molecular weight such as water, benzene, kerosene and most solutions of simple molecules are Newtonian fluids. NEWTONIAN AND NON-NEWTONIAN FLUIDS • NON-NEWTONIAN FLUIDS • Fluids which do not obey Newton’s law of viscosity. • These include slurries, mud flows, polymer solutions, blood etc. NEWTONIAN AND NON-NEWTONIAN FLUIDS NEWTONIAN AND NON-NEWTONIAN FLUIDS Newtonian and nonNewtonian fluids can be represented by the equation du τ = A + B dy n NEWTONIAN AND NON-NEWTONIAN FLUIDS Examples of Non-Newtonian fluids 1. Pseudoplastic or Thixotropic: Examples of such fluids are blood plasma, syrups, adhesives, molasses, and inks. 2. Dilatant fluids: Examples are slurries with high concentrations of solids such as corn starch, starch in water etc. 3. Bingham fluids: Examples of Bingham fluids are chocolate, mayonnaise, toothpaste and sewage sludge. HYDROSTATICS • Hydrostatics is a branch of fluid mechanics which is concerned with fluid at rest • The fluid is not subjected to any tangential force or shear stress • In hydrostatics all forces act normally to a boundary surface and are independent of viscosity • Viscosity is a measure of fluid resistance to tangential force or shear stress HYDROSTATICS INTRODUCTION TO PRESSURE • Atmospheric pressure, gauge pressure and absolute pressure Absolute Pressure Gauge pressure (+ve pressure) Atmospheric Pressure (Patm = 0) Vacuum pressure (-ve pressure) Absolute zero Pabs = Pgauge + Patm INTRODUCTION TO PRESSURE • For example, if a pressure of 50 kN/m2 is measured with a gauge referenced to the atmosphere and the atmospheric pressure is 100 kN/m2, then the pressure can be expressed as either P = 50 kN/m2 (gauge) or P = 150 kN/m2 (absolute). • If on the other hand, a gauge indicates a vacuum pressure of 31 kN/m2, then this can be stated as 70 kN/m2 (absolute), or -31 kN/m2 (gauge), assuming that the atmospheric pressure is 101 kN/m2 (absolute). INTRODUCTION TO PRESSURE • Pressure intensity ‒ defined as the pressure force per unit area. P P ‒ Mathematically, P= F A h INTRODUCTION TO PRESSURE • Pressure intensity ‒ Or P = W = mg = ρVg = ρAhg = ρgh A A A A ‒ where ρ = density of the liquid g = acceleration of gravity = 9.81 m/s2 h = depth below the free surface or pressure head W P P h INTRODUCTION TO PRESSURE • Pressure intensity ‒ Units of pressure i. N/m2, kN/m2 ii. Pascal, abreviated Pa 1 Pa = 1 N/m2 iii. bar 1bar = 1 x 105 N/m2 W P P h INTRODUCTION TO PRESSURE • Pascal’s law for pressure at a point • Pascal’s law states as follows: “The intensity of pressure at any point in a liquid at rest is the same in all directions.” INTRODUCTION TO PRESSURE • Proof of Pascal’s law Force due to Px = Px × Area ABEF = Pxδyδz Horizontal component of force due to Ps = −(Ps × Area ABCD )sin θ = − Psδsδz δy / δs = − Psδyδz INTRODUCTION TO PRESSURE • Proof of Pascal’s law • Equating Force due to Px to Horizontal component of force due to Ps , we get Pxδyδz = Psδyδz ⇒ Px = Ps INTRODUCTION TO PRESSURE • Proof of Pascal’s law • Similarly in the y-direction Force due to Py = Py × Area CDEF = Pyδxδz Vertical component of force due to Ps = −(Ps × Area ABCD ) cos θ = − Psδsδz δx / δs = − Psδxδz force due to weight of element = − ρ (δxδyδz / 2 )g INTRODUCTION TO PRESSURE • Proof of Pascal’s law • Equating Force due to Px to Horizontal component of force due to Ps , we get Pxδyδz = Psδyδz ⇒ Px = Ps INTRODUCTION TO PRESSURE • Proof of Pascal’s law • δxδyδz is negligible, so weight of element is neglected • Equating Force due to Py to vertical component of force due to Ps , we get ⇒ Py = Ps • Hence, Px = Py = Ps (proving pascal's law) PRESSURE VARIATION IN A STATIC FLUID • Fundamental equation of fluid statics relates pressure, specific weight and vertical distance. • This equation may be derived by considering the static equilibrium of a typical differential element of fluid in the figure below PRESSURE VARIATION IN A STATIC FLUID • For equilibrium, the algebraic sum of the forces in any direction must be zero. Resolving in the direction QP ( p + δp )δA − pδA + ρgδAδl cos θ = 0 • But δl cos θ = δz ⇒ or δp + ρgδz = 0 δp = − ρg δz • The minus sign indicates that the pressure decreases upwards. PRESSURE VARIATION IN A STATIC FLUID • Integrating the equation ∫ p2 p1 i.e. z2 δp = − ρg ∫ δz z1 p2 − p1 = − ρg ( z 2 − z1 ) PRESSURE VARIATION IN A STATIC FLUID • Variation of pressure vertically in a fluid under gravity p2 − p1 = − ρgh • where h = z2 - z1 PRESSURE VARIATION IN A STATIC FLUID • Equality of pressure at the same level in a static fluid p2 − p1 = − ρg ( z 2 − z1 ) • But z1 = z2 ⇒ p2 − p1 = 0 or p1 = p2 PRESSURE VARIATION IN A STATIC FLUID • Equality of pressure at the same level in a continuous body of fluid • In a continuous body of liquid, pressure at the same level is the same i.e PP = PQ PR = PS