Aero 1 Flashcards
(40 cards)
Standard Lapse Rate
2°C per 1000 feet.
Static Pressure
Result of the weight of the column of air supported above that elevation. (S=p/p0)
Density
Mass of air per unit volume
Sigma = p/p0
What affects density?
Pressure and Temperature
Humidity Corrections
10% Rule: For every 10% of relative humidity add 100 feet to your density altitude.
40% Rule Same as 10% rule, but subtract 40% RH to apply. (don’t go negative)
Name three varying components of the atmosphere
*Pressure
*Density
*Temperature
What components of the atmosphere are constant
*78% N2
*21%O2
*1% Other
Ideal Gas Law
P = pRT
Continuity Principle
A1V1 = A2V2
As area is decreased, velocity will increase
Bernoulli Equation
PTotal = Ps + ½ p V
T = PE + KE
Stagnation Point
Point on an airfoil when velocity of an air particle reaches zero
Front of leading edge and end of tip (vortices come together)
Airspeed Conversion
Indicated –> Calibrated –> Equivalent –> True
Indicated –> Calibrated via NATOPS
Calibrated –> Equivalent via compression correction (N/A)
Calibrated –> True via Rule of thumb (add 2% for every 1000’ PA)
Error Sources for Airspeed
*Calibrated A/S - Position/Location; Installation; Downwash
*Equivalent A/S - Compressibility
*True A/S - DA/Air density
Lift
Lift is the force perpendicular to the Relative Wind
Drag
Drag is the force parallel to the Relative Wind.
Generation of Lift
Lift results from a change in STATIC PRESSURE relative to the airfoil
Lower pressure on top leads to higher velocity, higher static pressure on the bottom causes force to lift airfoil
3 types of Drag
*Induced - air swirling over the airfoil
*Parasitic - air curling around itself on back of airfoil
*Profile - other things on aircraft (stores, gear, etc)
Chordline
Imaginary line moving through the middle of the airfoil
Camber
Measure of the chord from the chordline to top of airfoil
AOA
Angle between chordline and realitve wind
Blade Pitch
Angle between chordline and horizon
Induced Velocity
Vertical component of relative wind
Rotational velocity
Horizontal component of relative wind
Induced drag
Force pushing Lift vector away from perpendicular to the horizon; equal to induced velocity