Energy
Radioisotope Thermoelectric Generator
Decay heat into electricity, with no moving parts, for decades
A radioisotope thermoelectric generator (RTG) turns the decay heat of plutonium-238 directly into electricity through solid-state thermocouples — no moving parts, powering spacecraft like Voyager and Curiosity for decades. It is a nuclear battery, not a reactor: there's no chain reaction, just heat harvested from a steadily decaying isotope and converted by the Seebeck effect.
- FuelPlutonium-238 dioxide (PuO₂)
- ConversionSeebeck thermocouples (solid state)
- Fuel half-life87.7 years
- Efficiency~6 to 7%
- Moving partsZero
- Flown onVoyager, Cassini, Curiosity, New Horizons
Interactive visualization
Press play, or step through manually. The visualization is yours to drive — try it before reading on.
Watch the 60-second explainer
A condensed visual walkthrough — narrated, captioned, under a minute.
How an RTG works
Strip an RTG down to its idea and it is almost insultingly simple: a hot lump of metal on one side, cold space on the other, and a wall of thermocouples in between converting the temperature difference into a trickle of electricity. There is nothing to spin, nothing to pump, nothing to ignite. The "battery" inside is a brick of plutonium-238 dioxide that pours out heat simply because it is radioactive, and it will keep doing so for a human lifetime whether you ask it to or not.
The heat comes from alpha decay. A plutonium-238 nucleus spits out an alpha particle (a helium nucleus) and becomes uranium-234. That alpha particle slams to a stop within microns inside the fuel pellet, and its kinetic energy becomes heat. One gram of Pu-238 releases about 0.54 watts continuously — a thumb-sized pellet glows a dull red on its own. A full General Purpose Heat Source (GPHS) module holds four PuO₂ pellets (~600 g of fuel) and produces ~250 W of heat; stack 8 of them and you have the ~2000 W thermal source of a Mars-rover RTG.
Turning that heat into volts is the job of the thermocouple, exploiting the Seebeck effect: hold a junction of two dissimilar conductors at different temperatures and a voltage appears across it. An RTG wires hundreds of these couples electrically in series and thermally in parallel, sandwiched between the hot fuel core and a finned radiator facing cold space.
HOT side (~1000 °C, plutonium-238 core)
┌───────────────────────────────────────────┐
│ n-leg │ p-leg │ n-leg │ p-leg │ n-leg ... │ ← thermocouples
│ ▲ e⁻ │ ▼ h⁺ │ ▲ │ ▼ │ ▲ │ in series
└───────────────────────────────────────────┘
COLD side (~300 °C, fin radiator → space)
│
└──► DC out (~28–30 V bus)
Electrons diffuse from hot to cold in the n-type legs, holes do the same in the p-type legs, and because the legs alternate p-n-p-n in series, all those tiny voltages add up to a usable DC bus. No part of this moves. The only "motion" is charge carriers drifting down a temperature gradient — which is exactly why an RTG can run unattended for 40+ years.
The governing physics
Two equations carry almost everything you need to size an RTG. The first is the Seebeck voltage of a single couple, and the second is the thermoelectric figure of merit that decides how good your materials are.
Seebeck voltage of one couple:
V = (S_p − S_n) · (T_hot − T_cold) = S_pn · ΔT
S = Seebeck coefficient (V/K), material property
ΔT = hot-side minus cold-side temperature (K)
Dimensionless figure of merit (per material):
ZT = (S² · σ / κ) · T
σ = electrical conductivity (S/m) — want HIGH
κ = thermal conductivity (W/m·K) — want LOW
T = absolute temperature (K)
Maximum thermoelectric efficiency:
η_max = (ΔT / T_hot) · ( √(1+ZT) − 1 ) / ( √(1+ZT) + T_cold/T_hot )
└── Carnot ──┘ └──── material penalty ────┘
The first bracket is the Carnot ceiling — you can never beat it. The second bracket is the material tax: it would equal 1 (perfect) only if ZT were infinite. Real space-grade thermoelectrics have ZT ≈ 0.6–1.0, which is why even a 700 K temperature drop yields only ~6–7% device efficiency. Notice the tension baked into ZT: you want high electrical conductivity but low thermal conductivity in the same material, and in most solids those two move together (the Wiedemann–Franz law). Decades of materials work — silicon-germanium for high temperature, lead telluride and skutterudites for mid-range — has been a hunt for the rare "phonon-glass, electron-crystal" material that conducts charge well but heat poorly.
Decay sets the time axis. The thermal power of the fuel follows the exponential decay law:
P(t) = P₀ · (1/2)^(t / t½) = P₀ · e^(−λt), λ = ln2 / t½
For Pu-238, t½ = 87.7 yr → λ = 0.0079 /yr → ~0.79% thermal loss per year
Specific power of fresh PuO₂ fuel: ≈ 0.39 W/g (oxide form; 0.54 W/g for pure metal)
Worked example: sizing a Voyager-class RTG
Each Voyager carries three MHW-RTGs (Multi-Hundred-Watt). Let's reconstruct one from first principles.
Fuel: ~4.5 kg PuO₂ spheres, ~2400 W thermal at launch (1977)
Conversion: 312 silicon-germanium (SiGe) thermocouples in series
Hot junction: T_hot ≈ 1273 K (1000 °C)
Cold junction: T_cold ≈ 573 K (300 °C, radiator)
ΔT: 700 K
Carnot ceiling: ΔT / T_hot = 700 / 1273 = 55%
Material factor (ZT≈0.5): ≈ 0.12
Device efficiency: 0.55 × 0.12 ≈ 6.6%
Electrical output: 2400 W × 0.066 ≈ 158 W per RTG at launch
Three RTGs: ≈ 470 W total — matches the spec sheet ✓
Now run the clock forward. The fuel alone loses 0.79%/yr, so after 48 years (to 2025) the thermal source has dropped to 2400 × (0.5)^(48/87.7) ≈ 1640 W — a 32% fall. But Voyager's measured electrical output fell from 470 W to ~230 W, a 51% drop. The extra loss is the thermocouples degrading: SiGe legs sublime and their bonds grow resistive over decades. That gap between fuel decay and measured output is the single most important practical fact about RTGs — the converter ages faster than the fuel.
That declining budget is why Voyager's operators have spent the 2020s switching off instrument heaters and science instruments one by one: every watt the RTGs lose must be subtracted from somewhere, and the spacecraft is now running on roughly the power of a dim refrigerator bulb across 24 billion kilometres.
Real flown systems
| Generator | Mission(s) | Thermal / Electrical (BOL) | Thermoelectric material | Notes |
|---|---|---|---|---|
| SNAP-27 | Apollo 12–17 ALSEP | 1480 W / ~70 W | Lead telluride (PbTe) | Astronauts hand-loaded the fuel cask on the Moon |
| MHW-RTG | Voyager 1 & 2, LES-8/9 | 2400 W / ~158 W each | Silicon-germanium (SiGe) | Three per Voyager; still operating after 48 years |
| GPHS-RTG | Galileo, Ulysses, Cassini, New Horizons | ~4400 W / ~290 W | Silicon-germanium (SiGe) | The workhorse; uses stacked GPHS modules |
| MMRTG | Curiosity, Perseverance, Dragonfly | ~2000 W / ~110 W | PbTe / TAGS | Multi-Mission; runs in atmosphere or vacuum, ~14 yr design life |
| RHU (heater, not generator) | Many probes & rovers | 1 W / 0 W | None — pure heat | ~2.7 g pellet, keeps electronics from freezing |
RTG vs other space power sources
| RTG (Pu-238) | Solar PV array | Fission reactor (Kilopower) | Chemical battery | Fuel cell | |
|---|---|---|---|---|---|
| Works in deep space / no sun | Yes | No (inverse-square falloff) | Yes | Yes (short term) | Yes (short term) |
| Moving parts | None | Deploy/gimbal only | Pumps, turbine (Stirling) | None | Pumps/valves |
| Typical power class | 100 W – 300 W | 100 W – 30 kW | 1 – 10 kW | Wh, not continuous | 1 – 10 kW |
| Conversion efficiency | ~6–7% | ~30% (cell) | ~25–35% (Stirling) | n/a (storage) | ~50–60% |
| Operational lifetime | 14 – 45+ years | 10 – 20 years (degrades) | ~15 years | Hours – days | Days – weeks (reactant-limited) |
| Power decay cause | Decay + couple aging (~3%/yr early) | Radiation damage, dust | Fuel burnup (slow) | Self-discharge | Reactant depletion |
| Throttleable? | No — fixed heat output | Yes (point away) | Yes (control rods) | Yes | Yes |
| Best home | Outer planets, Mars night, lunar night | Inner solar system, Earth orbit | Surface bases, high-power probes | Launch, landers, buffering | Crewed short missions |
Design tradeoffs and failure modes
- Efficiency vs reliability. 6% efficiency looks terrible until you remember a Stirling converter at 25% efficiency adds a vibrating piston that must not fail for 14 years in a place no one can service it. NASA flew the Advanced Stirling Radioisotope Generator (ASRG) to TRL-6, then cancelled it in 2013 precisely because the moving-piston reliability risk outweighed the 4× efficiency gain. RTGs win by being boring.
- Thermocouple sublimation. At 1000 °C the SiGe legs slowly evaporate, thinning the conductor and raising resistance. Designers fight this with sealed cover gases (argon) and getters, but it remains the dominant electrical-degradation mechanism and the reason output falls faster than fuel decay.
- Fuel availability. Pu-238 is not a waste product; it must be deliberately bred by neutron-irradiating neptunium-237 in a reactor, then chemically separated. The US stopped production in 1988, ran down its stockpile, and only restarted at Oak Ridge in 2015 — now making roughly 400–500 g/yr against a goal of 1.5 kg/yr. A single GPHS-RTG holds 18 modules with roughly 7.8 kg of Pu-238 (about 10.9 kg as the dioxide). Fuel, not engineering, is the binding constraint on America's outer-planets program.
- Waste-heat management. Of ~4400 W thermal, ~4100 W is waste heat that must be radiated away — but that same waste heat is a feature, piped through the spacecraft to keep propellant and electronics from freezing. RTG missions design the thermal and electrical budgets together.
- Radiation to instruments. Pu-238 is a near-pure alpha emitter, but trace Pu-236 and spontaneous fission produce neutrons and gammas. Sensitive instruments (star trackers, particle detectors) are placed on a boom away from the RTG — the reason Voyager and Cassini have their generators on long arms.
- Launch-accident containment. The whole GPHS architecture exists to keep fuel contained if the rocket fails. Iridium cladding (ductile, high-melting, oxidation-resistant) around each pellet, carbon-carbon impact shells, and an aeroshell rated for reentry. This is also the source of most public controversy at every Pu-238 launch.
Why plutonium-238, specifically
The choice of fuel is the whole ballgame, and only a handful of isotopes even qualify. You want a long-ish half-life (so the mission outlives the fuel), high specific power (so the generator isn't enormous), and clean radiation (so you don't need a tonne of shielding). Those pull in opposite directions: high specific power means a short half-life, and a long half-life means low specific power. Pu-238 sits at the rare intersection.
| Isotope | Half-life | Specific power | Radiation | Verdict for an RTG |
|---|---|---|---|---|
| Plutonium-238 | 87.7 yr | 0.54 W/g | Alpha (clean) | The standard. Long life, modest shielding |
| Strontium-90 | 28.8 yr | 0.46 W/g | Beta → bremsstrahlung | Cheap (fission waste) but needs heavy shield; used in Soviet terrestrial RTGs |
| Polonium-210 | 138 days | 140 W/g | Alpha | Huge power density, but gone in months — short missions only |
| Curium-244 | 18.1 yr | 2.8 W/g | Alpha + neutrons | High power but neutron-noisy; needs more shielding |
| Americium-241 | 432 yr | 0.11 W/g | Alpha + gamma | ESA's pick — very long life, low power; bulkier generators |
Europe, lacking a Pu-238 supply, has invested in americium-241 RTGs and heater units: its 432-year half-life and availability from civil plutonium stockpiles outweigh its low 0.11 W/g specific power and the gamma shielding it demands. It's a reminder that the "best" fuel is partly a supply-chain question, not just a physics one.
Common misconceptions and pitfalls
- "An RTG is a tiny nuclear reactor." No fission, no chain reaction, no criticality. It cannot melt down or run away. It is a heat-emitting fuel slug wired to a thermopile — closer to a glow-stick than to a power plant.
- "You can throttle it like a reactor." You can't. The heat output is fixed by physics and falls only as the fuel decays. Spacecraft regulate the electrical side with a shunt regulator that dumps excess power as heat, and store surplus in a battery for peak loads.
- "More efficient is always better." On a 14-year unattended mission, an extra moving part that might seize is a worse bet than 18% of wasted heat. The ASRG cancellation is the textbook case: higher efficiency lost to reliability.
- "Output drops only because the fuel decays." The thermocouples degrade faster than the fuel early in life. Half of Voyager's lost power is converter aging, not decay.
- "It's dangerous because it's radioactive." Pu-238 is an alpha emitter; a sheet of paper or the fuel's own cladding stops the radiation. The genuine hazard is inhalation of dispersed fuel — which is exactly what the GPHS containment is engineered to prevent in an accident. The flown ceramic form (PuO₂) is designed to fracture into coarse, non-respirable chunks rather than fine dust.
- "RTGs are obsolete." The opposite — Dragonfly (launching to Titan) and the proposed enhanced MMRTG show the architecture is still the only proven option for the outer solar system. The bottleneck is Pu-238 supply, not the technology.
Frequently asked questions
Is an RTG a nuclear reactor?
No. A reactor sustains a controlled chain reaction (fission) and can be throttled or shut down. An RTG has no chain reaction and no criticality — it simply harvests the heat that plutonium-238 gives off as it naturally alpha-decays, and that heat output cannot be turned on or off. The fuel decays at a fixed rate set by its 87.7-year half-life whether or not you draw power. That is why an RTG needs no control rods, no coolant pumps, and no operator: it is a battery, not a power plant.
Why is RTG efficiency only about 6 percent?
Thermoelectric conversion efficiency is capped by the Carnot limit times the material figure of merit ZT. Even the GPHS-RTG runs a hot junction near 1000 °C against a radiator near 300 °C, a Carnot ceiling of about 55 percent, but real thermocouple materials (silicon-germanium, lead telluride) have ZT values around 0.6 to 1, so actual device efficiency lands near 6 to 7 percent. The rest of the ~4400 W of decay heat is radiated to space as waste. Engineers accept this because the trade — zero moving parts and 14+ years of unattended operation — is worth far more than efficiency on a deep-space mission.
Why does an RTG's power output drop over time?
Two reasons, and the second is the surprise. First, the plutonium-238 decays away with an 87.7-year half-life, so thermal power falls about 0.8 percent per year. Second, and usually larger early on, the thermocouples themselves degrade — sublimation of the thermoelectric legs, dopant migration, and bond resistance growth. Voyager's RTGs were specified at 470 W at launch in 1977 and put out roughly 230 W by 2025: far more loss than the fuel decay alone, because the SiGe couples aged.
Why plutonium-238 instead of a cheaper isotope?
Pu-238 hits a rare sweet spot. Its 87.7-year half-life is long enough for a decades-long mission yet short enough to give a high specific power of about 0.54 W per gram. It is almost a pure alpha emitter, so a few millimetres of cladding stops the radiation — no heavy gamma shielding needed. And as plutonium dioxide it is a stable, high-melting-point ceramic that won't disperse if the fuel capsule is breached. Strontium-90 is cheaper but a beta/gamma emitter needing heavy shielding; polonium-210 has far higher power density but a 138-day half-life, useless for a long mission.
What happens to an RTG if the launch rocket explodes?
Modern US RTGs use the General Purpose Heat Source (GPHS) module, engineered to contain the fuel through a launch accident. Each pellet of plutonium-238 dioxide sits inside an iridium alloy clad capsule, wrapped in carbon-bonded carbon-fiber impact shells and a fine-weave carbon-carbon aeroshell rated to survive reentry and ground impact. The 1997 Cassini launch and the 1968 Nimbus-B1 abort (whose fuel was recovered intact from the seafloor and reused) are the real-world stress tests of this containment philosophy.
Could a solar panel do the same job as an RTG?
Only close to the Sun. Sunlight intensity falls with the inverse square of distance, so at Jupiter (5.2 AU) a panel receives about 1/27th of Earth's irradiance, and at Pluto (39 AU) about 1/1500th. Juno reached Jupiter on solar power only with three 9-metre wings totaling ~60 m². Beyond Saturn, and on any mission needing power through a 14-day lunar night or a Martian dust storm, an RTG is the practical choice. New Horizons crossed to Pluto on a single RTG; no solar array could have done it.