Presentation 6: Fundamentals of Aircraft Aerodynamics Flashcards
Perfect Gas Law
p = [rho] R T
R = 1716 ft*lb/slugs*R
R = 287.05 N*m/kg*K
Assumptions of the Standard Atmosphere
That the atmosphere is a homogeneous gas of uniform composition that satisfies the perfect gas law.
Effects of Water Vapor
Affects engine performance and supersonic aerodynamics
Standard Sea-Level Properties
g = 32.17 ft/s^2 = 9.806 m/s^2
p = 2116.2 lb/ft^2 = 1.013 x 10^5 N/m^2
T = 59 deg F = 518.7 deg R = 15 deg C = 288.2 K
rho = 0.002377 slug/ft^3 = 1.225 kg/m^3
Tropopause
Transition between the troposphere (negative temperature gradient) and the stratosphere (isotherm).
At 36,089 ft
Temperature is -69.7 deg F
Temperature Variation w/ Altitude
T = T1 + a(h-h1)
a = -0.00356616 deg F/ft
a is the “temperature lapse rate”
Temperature Ratio to S.L. Temp
(Theta)
Theta = 1-6.875 x 10^-6 (h)
Pressure Ratio to S.L. Pressure
(Delta)
Delta = [Theta]^5.2561
Density Ratio to S.L. Density
(Sigma)
Sigma = [Theta]^4.2561
Kinematic Viscosity
[nu] = [mu] / [rho]
Reynolds Number
Re = V*l / [nu]
Re = [rho]*V*L / [mu]
Indicated Airspeed (IAS)
The direct reading from the airspeed indicator. This represents the airplane’s speed through the air, not necessarily its speed across the ground.
Cailbrated Airspeed (CAS)
The indicated airspeed corrected for instrument position and instrument error.
Different for each uniqure aircraft and its position of the pitot tube.
No direct reading of CAS in the cockpit, pilot must refer to handbook for particular aircraft.
True Airspeed (TAS)
Corrects for the effect of change in altitude on airspeed.
The airspeed indicator is calibrated for sea-level, not altitude.
TAS can be approximated by increasing the IAS by 2% per thousand feet of altitude.
The Anatomy of an Airplane