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Figure 1. Aerodynamics: The science of the air flow around as well as the forces and moments acting on a structure in a moving airstream. Major aerodynamic forces on aircraft: Lift = L Drag = D Pitching Moment = M Thrust = T Weight = W. Steady level flight: Lift = Weight
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Figure 1. Aerodynamics: The science of the air flow around as well as the forces and moments acting on a structure in a moving airstream Major aerodynamic forces on aircraft: • Lift = L • Drag = D • Pitching Moment = M • Thrust = T • Weight = W Steady level flight: Lift = Weight Thrust = Drag M = 0
Airfoil Geometry • b = span • c = chord • S = planform area • Aspect Ratio = b2/S = A
Sail Geometry Camber = t/c Aspect Ratio: A = b2/SA SA = Sail Area
Forces on Wing & Sail Wing L = Lift D = Drag R = Resultant V = Relative Wind Sail
Forces on a Sailboat A 6-Metre yacht Equilibrium of forces in the close-hauled sailing condition, Vt = 12 knots LWL = 23.5 ft Beam = 6.5 ft Draft = 5.4 ft Displacement = 94 lb Sail Area = 600 sq ft Lateral Area (hull) = 70 sq ft Angle of heel = 20°
Basic properties of the atmosphere required • for sailing or winged flight • Density (function of p & T) • Viscosity • If air had density but no viscosity • Balloon flight is possible • No sailing or winged fight is possible • Early inviscid theory predicts no lift • Consequences of viscosity • Skin friction drag (unavoidable) • Boundary layer creation → lift
Boundary LayerVelocity Gradient in Viscosity of Surface of an Airfoil Laminar Flow: Relatively low skin friction drag B.L. separates at relatively low α Laminar separation → large pressure drag Turbulent Flow: Relatively large skin friction drag B.L. remains attached to higher α
Transition Laminar to Turbulence Determined by Reynolds number Re Re = VAl/ν = velocity x distance ÷ viscosity value v = called kinematic viscosity. It is basic property of air
Boundary Layer → Circulation ← Circulation: air velocity higher on top surface than bottom By Bernoulli’s theory, pressure on top surface > pressure on bottom surface Typical airfoil pressure distribution
Simplest (Quantitative) Theory of Lift & Drag(Based Upon Concept of Dynamic Pressure – q) Dynamic pressure = air density x airspeed2 q =ρv2/2 Sea level standard day ρ = .0024 slugs/ft3 = air density equivalent to .0768 lb/ft3 v must be in ft/sec v(ft/sec) = 1.47 x V(mph) Example: at 100 mph (SLSD) q = 26 lb/ft2
Actual Lift Produced by a Wing Depends Upon: • Dynamic pressure – q • Wing area – S • Angle of attack – α • L = qSCL • CL = lift coefficient • CLvaries with α
Drag Drag – retarding force D = q S CD CD = drag coefficient 3 Physical sources of drag Skin friction Pressure drage (due to separation) Induced drag (varies with lift)
Drag Coefficient • CD = CDo + CDi • CDo due to skin friction and pressure drag • CDi induced drag coefficient • CDo is nearly constant C (for a given aircraft) • CDi = C2L/πeA
Physical Origin of Induced Drag – Wing Tip Trailing Vortices Lifting line or bound vortex
Downwash at Wind Due to Trailing Vortices Tips Local Velocity Vector Down Downwash
Induced drag is a function of lift alone and has nothing to do with the angle of incidence except to modify it through the introduction of an induced angle