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  • There is an intriguing phenomenon

  • when you closely examine the science behind airfoils.

  • Why does the air above the airfoil flow much faster than the air below?

  • How come the two never meet?

  • The answer is right there in the pressure gradient.

  • Before explaining the reason,

  • we will first describe how the pressure gradient is developed.

  • In the first part of the airfoil video

  • we learned that the flow gets curved as shown to the kiwanda effect.

  • You can explain the pressure distribution

  • by keeping in mind that in a curved flow pressure is higher at the outside.

  • There are three main flow curvatures in this flow.

  • The biggest is at the top of the airfoil.

  • Far away from the airfoil the pressure is atmospheric

  • so due to this high curvature

  • pressure will decrease as we move toward the airfoil.

  • The second curvature is at the bottom of the airfoil near the tail,

  • this is also curved downward

  • so here if we move toward the airfoil, the pressure should increase.

  • The last flow curvature is also at the bottom of the airfoil

  • close to the leading edge.

  • This is a very small curvature

  • this curvature, however, is curved slightly upward.

  • This means that the pressure should decrease in this region

  • as we move toward the airfoil.

  • Due to the very small curvature

  • there will be a very small drop in pressure.

  • We know that far away from the upstream and downstream

  • the pressure is atmospheric.

  • At the leading edge of the airfoil,

  • a high-pressure region is generated as the flow directly hits this portion

  • so we can easily construct the pressure distribution as shown

  • The CFD results could form exactly two are logical conclusions.

  • Now back to the initial question

  • to facilitate the analysis

  • we can neglect this very small drop in pressure.

  • You can see that at the top

  • the pressure decreases almost to the midpoint before it increases

  • at the bottom the pressure keeps on increasing

  • until it reaches the tail

  • only after that does it decrease.

  • Pause for a moment now

  • and consider two fluid particles starting at the same speed

  • but in different pressure gradients.

  • The top particle is surrounded by a decreasing pressure condition

  • while the bottom particle sits in an increasing pressure condition.

  • For the top particle pressure on the right side is less than at the left side

  • so there will be a net force in the same direction of the velocity

  • and the particle will speed up.

  • However, the reverse is true for the bottom particle

  • here the net forces against velocity direction

  • so it will decelerate.

  • In short, in a decreasing pressure filled the fluid particle will accelerate

  • and in an increasing pressure filled the fluid particle will decelerate.

  • This is exactly what happens in an airfoil also

  • the bottom particle will keep on decelerating

  • the top particle will accelerate up to the midpoint.

  • This means that the speed of the top particle

  • will be higher at any point in time

  • and the two particles will never meet.

  • The bottom particle also experiences of pressure decreasing scenario,

  • However, it is almost after the trailing edge and it happened suddenly

  • such a sudden drop in pressure will not considerably increase the particle speed.

  • In short for this particular problem

  • the pressure distribution makes the particles flow at different speeds

  • but the reverse argument does not hold

  • the different speeds of the particles are not what make the pressure distribution

  • because for the second textbook argument

  • there is no logical explanation for what causes this speed difference?

  • These two arguments are not too different ways of looking at the same thing.

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There is an intriguing phenomenon

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