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Reentry Heat Flux⚠ unverified

Aerospace / Structures · Compute the approximate stagnation-point convective heat flux on reentry

Parameters

InputSymbolUnitDefaultDescription
rhoρkg/m^31.0Free-stream atmospheric density
VVm/s1.0Vehicle velocity
R_nRnm1.0Nose radius
OutputSymbolUnitDescription
resultqW/m^2Stagnation-point heat flux, in watts per square metre (W/m^2)

The science & history

Understanding the Parameters

Derivation (Approaching a Proof)

Stagnation-point convective heating comes from boundary-layer theory in the shock layer at the nose. The seminal Fay–Riddell analysis (1958) solved the stagnation-point boundary layer to give the heat flux in terms of the enthalpy difference across it and the velocity gradient at the wall. The key results are:

Combining these boundary-layer scalings gives $q \propto \sqrt{\rho/R_n}\,\cdot\,(\text{function of }h_0)$. Sutton and Graves (1971) reduced the Fay–Riddell physics to a compact engineering power-law fit for air,

$$q = k\,\sqrt{\frac{\rho}{R_n}}\;V^{N}, \qquad k = 1.83\times10^{-4}\ \tfrac{\text{kg}^{1/2}}{\text{m}},\quad N \approx 3.05,$$

with the exponent $3.05$ (rather than exactly $3$) capturing the mild departure from the ideal enthalpy scaling across the real-gas regime. $\blacksquare$ The constant $k$ is specific to Earth air; other atmospheres (Mars CO₂, Venus, the gas giants) use different Sutton–Graves constants.

Dimensional check. The constant $k$ carries the units needed to make $\sqrt{\rho/R_n}\,V^{3.05} = \sqrt{(\text{kg}/\text{m}^3)/\text{m}}\cdot(\text{m}/\text{s})^{3.05}$ resolve to $\text{W}/\text{m}^2$; $k$ is an empirical dimensional constant ($1.83\times10^{-4}$ in SI). $\checkmark$

History and Development

Related Concepts: ISA Density, Density Altitude, Mach Number, Speed Of Sound, Thermal Stress, Combustion Chamber Temperature

Notes: Registry calculator reentry-heat-flux (unverified; lives in the structures module but is an aerothermal/reentry calc). Sutton–Graves stagnation-point convective heating — correct as shipped; the constant $1.83\times10^{-4}$ is Earth-air specific. Heating $\sim V^3$ (velocity-dominated); $1/\sqrt{R_n}$ is the blunt-body effect (blunter = cooler). A radiative term adds at the highest entry speeds. All defaults $1.0$.

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