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Stagnation Heat Flux⚠ unverified

Aerospace / Reentry · Stagnation-point convective heat flux

Parameters

InputSymbolUnitDefaultDescription
rhoρkg/m^30.001Freestream density
vvm/s7000.0Velocity
RnRnm0.5Nose radius
OutputSymbolUnitDescription
qqW/m^2Heat flux

The science & history

Understanding the Parameters

Derivation (Approaching a Proof)

Stagnation-point heating comes from boundary-layer theory in the shock layer at the nose. The seminal Fay–Riddell analysis (1958) solved the stagnation boundary layer and found the wall heat flux scales with:

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

$$q = k\,\sqrt{\frac{\rho}{R_n}}\;V^{N}, \qquad k = 1.83\times10^{-4},\quad N \approx 3.05,$$

the exponent $3.05$ (rather than exactly $3$) capturing the mild real-gas departure from ideal enthalpy scaling. $\blacksquare$ The constant $k$ is specific to Earth air; Mars ($\mathrm{CO_2}$), Venus, and the gas giants use different Sutton–Graves constants.

Dimensional check. $k$ is an empirical dimensional constant ($1.83\times10^{-4}$ in SI) chosen so that $\sqrt{\rho/R_n}\,V^{3.05} = \sqrt{(\text{kg}/\text{m}^3)/\text{m}}\,(\text{m}/\text{s})^{3.05}$ resolves to $\text{W}/\text{m}^2$. $\checkmark$

History and Development

Related Concepts: Reentry Heat Flux, Peak Heating Altitude, Reentry Heat Load, Ablation Rate, Thermal Protection Thickness, Ballistic Coefficient, ISA Density

Notes: Registry calculator stagnation-heat-flux (unverified). Sutton–Graves stagnation-point convective heating — correct; duplicate of the Structures Reentry Heat Flux page (same law). Constant $1.83\times10^{-4}$ is Earth-air specific; exponent $3.05$ (code) not the generic $3$ shown in the latex. A radiative term adds at the highest speeds. Heating $\sim V^3$; $1/\sqrt{R_n}$ is the blunt-body effect.

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