Resources on physics related to aerodynamics
The List of elementary physics formulae on wikipedia is useful.
List of variables
Variable
|
Meaning
|
Unit (SI)
|
γ (gamma)
|
Surface tension
|
N.m-1 (Newton per meter)
|
μ (mu) or η (eta)
|
Viscosity
|
Pa·s (Pascal second) or P (Poise, 1 Poise is 0.1 Pa.s)
|
C, Cp, CV
|
Heat capacity, general, at constant pressure, at constant volume.
|
J.K-1 (Joule per Kelvin)
|
G
|
Gibbs free energy
|
J (Joule)
|
H
|
Enthalpy: total energy of a thermodynamic system.
|
J (Joule)
|
ΔHvap or L
|
Vaporization heat or Latent heat of vaporization: energy required to vaporize a mole of liquid at a given temperature.
|
J.mol-1 (Joule per mole)
|
Q
|
Amount of Heat
|
J (Joule)
|
T
|
Temperature
|
K (Kelvin)
|
S
|
Entropy
|
J.K-1 (Joule per Kelvin)
|
U
|
Internal energy of a system (see first law of Thermodynamics below)
|
J (Joule)
|
V
|
Volume
|
m3 (cubic meter)
|
W
|
Work: mechanical constraints on the system.
|
J (Joule)
|
n
|
Quantity of matter
|
mol (mole)
|
p
|
Pressure
|
Pa (Pascal)
|
List of constants
List of equations
Equation
|
Name
|
Meaning
|
|
Ideal gas equation
|
Relation between properties of an ideal gas (state equation). k is kB.
|
|
Clausius-Clapeyron relation
|
Relation between the pressure, latent heat of vaporization and temperature of a vapour at two temperatures (approximation, at low temperatures).
|
|
Heat at state change for an ideal gas.
|
The heat required to change the state of a some matter, L being the latent heat. Delta H equals Q only when pressure is constant (isobaric).
|
|
First law of Thermodynamics
|
Variations of internal energy of a system between two states is the sum of the received heat and work (minus the given work).
|
|
Enthalpy
|
Total amount of energy of a system, defined as the sum of the internal energy U and pressure * volume.
|
|
Work of gas expansion.
|
Work done by expanding an ideal gas.
|
|
Entropy
|
Internal energy related to entropy variation for a closed system in thermal equilibrium (fundamental thermodynamic relation).
|
ΔSuniverse = ΔSsurroundings + ΔSsystem
|
Entropy variation as a whole.
|
Entropy variation of a system is generally compensated by the inverse variation of the surroundings, not including losses.
|
|
Gibbs free energy / Free enthalpy
|
Useful work obtainable from a system at isobaric and isothermal conditions. Since H is U + pV, it can be replaced in the equation, making G = H - TS.
|
|
Gibbs free energy variation.
|
This derivation is only valid at constant temperature.
|