I took my first aeronautical engineering class in 1975 and I still know the formula for lift. Not because I have a head for formulas and not because I have a good memory. (I don't.) I have this knowledge because I once heard the story about The Man Who Invented Lift.
But before we get to Bernoulli, we need to consider Sir Isaac Newton. I think the best way to understand what lift really is, begins with an engineering consideration of energy, which leads to Bernoulli's Equation for Subsonic Air Flow, and ends with an equation for the generation of lift.
Everything here is from the references shown below, with a few comments in an alternate color.
Consider for a moment a metal ball traveling at a constant speed on a flat surface approaching a dip, as shown in the drawing. As we did in freshman engineering class, we say the ball and the surface are both frictionless and there is no air resistance for the sake of this academic exercise.
We know that as the ball goes down the dip in the surface, its speed will increase until it gets to the bottom where it will trade that extra speed to climb the ramp. When it ends up back at the original level, since we are discounting the effect of friction, it will again be at its original speed.
Before it hits the slope, the energy of the ball can be described as the Kinetic Energy (KE) that comes from its motion and the Potential Energy (PE) due to its higher elevation.
[Dole, pg. 19] Consider the flow of air through a pipe of varying cross section, as shown [in the figure]. There is no air flow through the sides of the pipe; air only flows through the ends. As the air flown through the pipe, the mass of air entering the pipe, in a given unit of time, equals the mass of the air leaving the pipe, in the same unit of time. The mass flow throughout the pipe must remain constant. The mass flow at each station is equal. Constant mass flow is called steady-state flow. The mass airflow is equal to the volume of air multiplied by the density of the air. The volume of air, at any station, is equal to the velocity of the air multiplied by the cross sectional area of the station. The mass airflow, then, is the product of the density, the area, and the velocity.
The continuity equation states that the mass airflow is constant.
[where station 1 is the inlet, station 2 is the midpoint, and station 3 is the outlet.]
The continuity equation is valid for steady-state flow, both in subsonic and supersonic flow. For subsonic flow, however, the air is considered to be incompressible, and its density remains constant. The density can be cancelled out and thus:
[Dole, pg. 20] The energy of an airstream is in two forms. It has a potential energy, which is its static pressure, and a kinetic energy, which is its dynamic pressure. The total pressure in the airstream is the sum of the static pressure and the dynamic pressure. The total pressure remains constant, according to the law of conservation of energy, and so an increase in one form of pressure must result in a decrease of the other.
Static pressure is an easily understood concept. Dynamic pressure q corresponds to kinetic energy in mechanics and is expressed by the formula:
The units of q are:
which is psf.
Pilots are much more familiar with velocity measured in knots, rather than in feet per second, so a new formula for dynamic pressure is used.
Bernoulli's formula can now be expressed as:
It can now be seen that air flowing into a reduced area section of a venturi tube will increase in velocity, according to the continuity equation, and will have a decrease in static pressure, according to Bernoulli's equation.
If you split the experimental venturi tube in half, you end up with what looks like the cross section of an airfoil which behaves like the tube. This can be verified in wind tunnel tests.
[Dole, pg. 29] The air approaching the leading edge of an airfoil is first slowed down. It then speeds up again as it passes over or beneath the airfoil. [The figure] shows a comparison of two local velocities with the flight path velocity V1 and with each other.
As the velocity changes, so does the dynamic pressure and, according to Bernoulli's principle, so does the static pressure. Air near the stagnation point has slowed down, and thus the static pressure in this region is higher than the ambient static pressure. Air that is passing above and below the airfoil, and thus has speeded up to a value higher than the flight path velocity, will produce static pressures that are lower than ambient static pressure. At a point near maximum thickness, maximum velocity and minimum static pressure will occur. Because air has viscosity, some of its energy will be lost to friction and a "wake" of low velocity, turbulent air exists near the trailing edge, resulting in a small, high pressure area.
The shape of the wing directly impacts the airflow. While the science of wing shape has become very complicated, a few basic terms will help us understand how the airfoil produces lift and, more importantly, when it stops.
If we take a cross section of a wing we can define the shape with some airfoil terminology:
Looking at the wing from the top, the shape is called the planform of the wing. Because wings have become very complicated, it is helpful to simplify a drawing to help define the appropriate terms.
[Dole, pg. 50]
The formulas, of course, are generalized and would have to be tailored for the exact shape of an aircraft's wing but the simplified formula will come in handy when constructing lift / drag curves.
[Dole, pg. 26] There are four main variables in the geometry of an airfoil:
[Hurt, pg. 22]
[Dole, pg. 30] Aerodynamic Force (AF) is the resultant of all static pressures acting on an airfoil in an airflow, multiplied by the planform area that is affected by the pressure. The line of action of the AF passes through the chord line. at a point called the center of pressure (CP).
AF is resolved into two components, one parallel to the relative wind and called drag, and the other perpendicular to the relative wind and called lift.
The forces you see on a conventional "Lift / Weight / Thrust / Drag" drawing include two fictitious forces: lift and drag do not really exist as shown. While they are useful for the sake of discussion, they are not real.
Lift and drag are actually components of Aerodynamic Force.
The aerodynamic force includes:
[Hurt, pg. 20] The generation of lift by an airfoil is dependent upon the airfoil being able to create circulation in the airstream and develop the lifting pressure distribution on the surface. In all cases, the generated lift will be the net force caused by the distribution of pressure over the upper and lower surfaces of the airfoil. At low angles of attack, suction pressures usually will exist on both upper and lower surfaces but the upper surface suction must be greater for positive lift. At high angles of attack near that for maximum lift, a positive pressure will exist on the lower surface but this will account for approximately one-third of the net lift.
[Hurt, pg. 23] Lift has been defined as the net force developed perpendicular to the relative wind. The aerodynamic force of lift on an airplane results from the generation of a pressure distribution on the wing. This lift force is described by the following equation:
|=||½ ρ V2|
|S||=||wing surface area|
[Hurt, pg. 27] Airfoil section properties differ from wing or airplane properties because of the effect of the planform. Actually the wing may have various airfoil sections from root to tip with taper, twist, sweep back and local flow components in a span wise direction. The resulting aerodynamic properties of the wing are determined by the action of each section along the span and the three-dimensional flow and the force coefficients are given a notation of lower case letters. For example, a wing or airplane lift coefficient is CL while an airfoil section lift coefficient is termed cl.
I think many aero texts get sloppy in this regard, many switching between section and whole wing equations with little or no notice. I think we can simplify things, for a pilot's perspective, if we call CL the coefficient of lift for the entire wing, which allows us to remove the "S" from the L = CL q S equation. We can also substitute ½ ρ V2 for q and end up with the equation we learned in basic aero:
Do you need to know this equation to fly an airplane? No, of course not. But it does teach the relative importance of the variables. You can control the CL with leading and trailing edge devices, flaps and slats. You can control the ρ only indirectly by virtue of the altitude and temperature. Finally, you can control the V and its impact is magnified by the 2.
Portions of this page can be found in the book Flight Lessons 1: Basic Flight, Chapters 2 and 8.
14 CFR 25, Title 14: Aeronautics and Space, Federal Aviation Administration, Department of Transportation
Air Training Command Manual 51-3, Aerodynamics for Pilots, 15 November 1963
Connolly, Thomas F., Dommasch, Daniel 0., and Sheryby, Sydney S., Airplane Aerodynamics, Pitman Publishing Corporation, New York, NY, 1951.
Davies, D. P., Handling the Big Jets, Civil Aviation Authority, Kingsway, London, 1985.
Dole, Charles E., Flight Theory and Aerodynamics, 1981, John Wiley & Sons, Inc, New York, NY, 1981.
FAA-H-8083-15, Instrument Flying Handbook, U.S. Department of Transportation, Flight Standards Service, 2001.
Gulfstream G450 Airplane Flight Manual, Revision 35, April 18, 2013.
Gulfstream G450 Aircraft Operating Manual, Revision 35, April 30, 2013.
Hage, Robert E. and Perkins, Courtland D., Airplane Peformance Stability and Control, John Wiley & Sons, Inc., 1949.
Hurt, H. H., Jr., Aerodynamics for Naval Aviators, Skyhorse Publishing, Inc., New York NY, 2012.
Technical Order 1T-38A-1, T-38A/B Flight Manual, USAF Series, 1 July 1978.
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