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Entry trajectory, Sutton–Graves heating, and multi-layer conduction to size a capsule heat shield.

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Reentry Heating & TPS Thermal Model

▶ Try it in your browser — interactive version that runs the same model live. Includes temperature profiles through the wall, parameter studies with CSV export, published validation figures, and controls for layer thicknesses, initial temperature, grid, time step, soak-back window and the hot-wall correction.

How thick does a capsule's heat shield have to be? This project answers that by coupling three models — an entry trajectory, a stagnation-point heating correlation, and a transient multi-layer conduction model of the wall — and searching for the thinnest heat shield that keeps the bondline (the adhesive between the tiles and the aluminium structure) below its temperature limit, including the heat that keeps soaking inward long after the heating has stopped.

Result. Sized to a 430 K bondline, the baseline entry needs 7.0 cm of LI-900 (16.0 kg/m² for the whole wall). The surface still reaches 1721 K, above LI-900's 1533 K reuse limit. FRCI-12 is the lightest of the three tiles that stays inside its own limit.

Why this matters

Aerothermodynamic heating is the defining constraint of entry-vehicle design. A capsule returning from low Earth orbit converts roughly 30 MJ of kinetic energy per kilogram of vehicle into heat in the shock layer; most of it is carried away by the flow, but the fraction that reaches the surface still drives the vehicle's mass. Thermal-protection mass is paid for on every flight, so sizing it accurately — not just conservatively — matters.

The three coupled models

1. Trajectory — planar point mass over a non-rotating spherical Earth (src/tps/trajectory.py):

$$\dot V = -\frac{D}{m} - g\sin\gamma,\qquad \dot\gamma = \frac{1}{V}\Big[\frac{L}{m} - \Big(g - \frac{V^2}{R_E+h}\Big)\cos\gamma\Big],\qquad \dot h = V\sin\gamma$$

with $D/m = \rho V^2/2\beta$, $L = (L/D),D$, $g = g_0 (R_E/(R_E+h))^2$ and an exponential atmosphere $\rho = \rho_0 e^{-h/H}$ ($H$ = 7.2 km). Integrated with RK45 (rtol 1e-8) from the 120 km entry interface to $V$ = 500 m/s; skip-out is detected.

2. Stagnation-point heating — Sutton–Graves (src/tps/heating.py):

$$q_{conv} = k,\sqrt{\rho/R_n},V^3,\qquad k = 1.7415\times10^{-4}\ \mathrm{kg^{1/2}/m}$$

with an optional hot-wall correction $q(1 - h_w/h_0)$, and re-radiation from the surface: $-k,\partial T/\partial x|0 = q{conv} - \varepsilon\sigma(T_s^4 - T_\infty^4)$, where $T_\infty$ comes from the 1976 U.S. Standard Atmosphere (checked against the printed tables at six altitudes).

3. Wall conduction — $\rho c_p(T),\partial T/\partial t = \partial_x(k(T),\partial_x T)$ through [heat shield | bondline | structure] (src/tps/conduction.py):

  • implicit finite volume (backward Euler, Crank–Nicolson option), tridiagonal solve per step;
  • cells never straddle a layer boundary; series (harmonic-mean) conductance at interfaces;
  • geometric stretching clusters cells at the hot surface;
  • energy-conserving enthalpy form with temperature-dependent $k$ and $c_p$; the $T^4$ boundary condition is Newton-linearized and iterated to 1e-6 K each step;
  • the run continues after heating ends (soak-back) until the bondline peak has passed.

If the peak remains unconfirmed at the maximum soak time, sizing stops with an error rather than using an incomplete temperature maximum. The default maximum is four hours after heating ends; set numerics.max_soak_time (seconds) in the baseline YAML for cases needing a longer cooling run. The browser app applies the same check and reports when it cannot confirm a sizing result.

Sizing (src/tps/sizing.py): Brent's method on the heat-shield thickness, such that the peak bondline temperature equals the limit minus a margin. The result is never thinner than needed and at most 0.1 mm thicker.

Assumptions

  • Non-ablating wall: a reusable conduction/re-radiation system (ceramic tiles), no pyrolysis or surface recession.
  • No shock-layer radiative heating (valid below about 10 km/s, i.e. for low-Earth-orbit returns).
  • Stagnation point only, one-dimensional conduction through the wall.
  • The tile coating is represented only by its emissivity; the strain-isolation pad used on the Space Shuttle between tile and adhesive is not modelled.
  • Tile conductivity at 1 atm (the highest value in the tables, conservative for the bondline; the bondline peaks during soak-back, low in the atmosphere).

Materials

All properties are from NASA RP-1289, Thermal Protection Materials: Thermophysical Property Data (Williams & Curry, 1992), transcribed in their printed units with page citations in data/materials.yaml and converted to SI on loading.

Layer Material Density (kg/m³) Max use temperature (K)
Heat shield LI-900 silica tile 144 1533
Heat shield LI-2200 silica tile 352 1756
Heat shield FRCI-12 fibrous composite 192 1756
Coating RCG, emissivity 0.85 — —
Bondline RTV-560 silicone adhesive 1410 561
Structure Aluminium 2219 2813 450

Validation

Conduction solver vs. analytical solutions

Conduction validation

Case Reference Result
Semi-infinite solid, constant flux $T_s - T_i = (2q/k)\sqrt{\alpha t/\pi}$ within 0.5%; first order in time, second order in space, as designed
Finite slab, sudden surface temperature Fourier series within 0.2% of the temperature step
Two-layer steady state series thermal resistance exact to round-off; slope ratio = inverse conductivity ratio
$k(T) = a + bT$ steady state Kirchhoff transform second-order convergence
Constant heating with re-radiation radiative equilibrium $\varepsilon\sigma(T^4 - T_\infty^4) = q$ to 1e-6
Energy conservation with radiation and tabulated $k(T)$, $c_p(T)$ $\int(q_{in} - q_{rad} - q_{back}),dt = \Delta E_{stored}$ closes to 1e-13 (spec: 0.1%)

Trajectory vs. Allen–Eggers

Allen–Eggers validation

Allen & Eggers' ballistic solution assumes constant flight-path angle and no gravity. With gravity and curvature switched off, the integrated trajectory reproduces it to 1e-6. With full physics, on the steep ballistic case ($V_E$ = 7.5 km/s, $\gamma_E$ = −20°, $\beta$ = 500 kg/m²):

Allen–Eggers Simulation Difference
$V/V_E$ at peak deceleration $e^{-1/2}$ = 0.6065 0.6127 +1.0%
$V/V_E$ at peak heating $e^{-1/6}$ = 0.8465 0.8571 +1.25%
Peak deceleration 50.1 g 52.6 g +4.9%

The residual is the gravity component along the path, which Allen–Eggers neglects: it keeps the vehicle slightly faster at every altitude. Its size relative to drag at peak deceleration is $2eHg/V_E^2$, so doubling the entry speed should cut it about fourfold — the simulation shows exactly that (right panel). For shallow entries, path curvature takes over as the dominant effect.

Grid and time-step convergence

Bondline convergence

At the sized thickness, the bondline peak converges at second order in cell size and first order in time, which is what backward Euler should do. From 40 to 320 uniform cells the error falls from 0.38 K to under 0.02 K. The production run (60 cells, stretched toward the hot surface, Δt = 0.5 s) sits inside that band: the uniform-grid study is already within 0.1 K at 80 cells, and within 0.01 K at Δt = 0.5 s.

Baseline case

A representative low-Earth-orbit lifting capsule, stated as a design assumption in data/baseline.yaml:

Input Value Basis
Entry speed 7.8 km/s circular-orbit speed; keeps the no-radiation, non-ablating assumptions valid
Entry angle −1.5° shallow lifting corridor
Ballistic coefficient 400 kg/m² assumed
L/D 0.3 Apollo command-module trim
Nose radius 4 m assumed blunt capsule
Heat shield LI-900, sized NASA RP-1289
Bondline / structure 0.2 mm RTV-560, 2 mm Al 2219 assumed layup; thicknesses are not in RP-1289
Initial temperature 295 K wall at room temperature before entry
Bondline limit 450 K, sized to 430 K Al 2219 maximum-use temperature, RP-1289 p. 19-2; 20 K is a design margin

The aluminium limit governs. RTV-560's own limit is 561 K, and the adhesive sits on the skin.

Results

Time histories

Baseline time histories

Quantity Value
Sized LI-900 thickness 7.03 cm
Areal mass, all layers 16.04 kg/m² (10.1 kg/m² of tile, 5.9 kg/m² of adhesive and skin)
Peak heat flux 43.7 W/cm² at t = 299 s
Heat load 129 MJ/m²
Peak deceleration 2.63 g
Peak surface temperature 1721 K, above the 1533 K tile limit
Peak bondline temperature 429.9 K at t = 3464 s (target 430 K)

The entry is shallow enough to lift. The vehicle checks its descent, which puts a second peak on the deceleration and a shoulder on the heat pulse. Peak heating is at five minutes. The bondline does not peak until nearly an hour later, after convective heating has already ended: the heat soaks inward through the tile. That delay is why the conduction run continues past the trajectory.

Temperature profiles

At peak heating the gradient is confined to the outer tile. By the bondline peak the wall has evened out near 430 K. The adhesive and the skin are 2.2 mm combined, so they sit on top of each other at the right-hand edge of the plot.

What the thickness depends on

Sensitivity sweeps

For one tile material the areal mass moves with thickness (the adhesive and skin do not change), so the plots show thickness. The mass for every point is in results/sweeps.md.

  • Entry angle is the classic trade. From 0.9° to 4.5° the peak flux rises from 34 to 86 W/cm², the heat load falls from 146 to 79 MJ/m², and the tile thins from 7.9 to 4.8 cm. A steeper entry is a hotter, shorter pulse, and the bondline cares about the load, not the peak.
  • Entry speed, on this lifting path, does the opposite of a steep ballistic entry. From 7.2 to 8.0 km/s the vehicle rides higher, so the peak flux falls (60 to 35 W/cm²) while the pulse lasts longer. Heat load rises from 74 to 183 MJ/m² and the tile grows from 4.8 to 9.2 cm.
  • Ballistic coefficient. A heavier vehicle glides in denser air. Thickness grows from 6.0 cm at 200 kg/m² to 8.2 cm at 800 kg/m². Peak deceleration stays at 2.63 g: on this path the load factor is set by L/D, not by β.
  • Nose radius. Heating scales as 1/√Rₙ. Doubling the nose from 4 m to 8 m cuts the heat load from 129 to 91 MJ/m² and thins the tile from 7.0 to 6.0 cm.

Steep versus shallow

Which tile

Material comparison

All three coatings are the same RCG (ε = 0.85), so the surface temperature is set by re-radiation and is almost the same, about 1710–1720 K. What changes is whether that temperature is allowed.

Material Thickness Areal mass Peak surface Limit Usable here
LI-900 7.03 cm 16.0 kg/m² 1721 K 1533 K no
LI-2200 6.39 cm 28.4 kg/m² 1711 K 1756 K yes
FRCI-12 7.21 cm 19.8 kg/m² 1718 K 1756 K yes

LI-900 is the lightest wall and the one the bondline constraint would pick, and it overheats its surface. LI-2200 survives and is slightly thinner, but it is more than twice as dense, so the wall is the heaviest. FRCI-12 stays under its limit at 19.8 kg/m², 8 kg/m² lighter than LI-2200. For this entry it is the tile to fly.

Limitations and next steps

  • Stagnation point only. Next: Lees' laminar heating distribution around the blunt body, to size the shield away from the nose.
  • No ablation. Next: pyrolysis and surface recession for ablative heat shields (Avcoat, PICA), needed for faster lunar and Mars returns.
  • No shock-layer radiation, which becomes significant above roughly 10 km/s.
  • Simplified atmosphere for the trajectory (exponential).
  • A correlation instead of a flow solution. In blunt-body CFD, a resolved shock layer gives the wall heat flux directly; replacing Sutton–Graves with CFD heating at a few trajectory points is the natural link between this model and that work.

Running it

python -m venv .venv && source .venv/bin/activate
pip install -e ".[dev]"
pytest                          # validation suite
node --test tests/test_browser.cjs  # browser model regression checks (Node.js 22+)
python scripts/make_figures.py  # every figure and results table

Design inputs live in data/baseline.yaml and data/materials.yaml; the scripts refuse to run while any value is still marked TODO.

References

  • Allen, H. J.; Eggers, A. J.: A Study of the Motion and Aerodynamic Heating of Ballistic Missiles Entering the Earth's Atmosphere at High Supersonic Speeds, NACA Report 1381, 1958.
  • Sutton, K.; Graves, R. A.: A General Stagnation-Point Convective-Heating Equation for Arbitrary Gas Mixtures, NASA TR R-376, 1971.
  • Williams, S. D.; Curry, D. M.: Thermal Protection Materials: Thermophysical Property Data, NASA RP-1289, 1992.
  • U.S. Standard Atmosphere, 1976, NOAA-S/T 76-1562.
  • Anderson, J. D.: Hypersonic and High-Temperature Gas Dynamics, AIAA.
  • Incropera, F. P. et al.: Fundamentals of Heat and Mass Transfer, Wiley.
  • Patankar, S. V.: Numerical Heat Transfer and Fluid Flow, Hemisphere, 1980.

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Entry trajectory, Sutton–Graves heating, and multi-layer conduction to size a capsule heat shield.

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