Subsystem 03 of 12 · Thermal control
Lunar Habitat ACT, the Autonomous Construction Testbed·Thermal control·Concept definition, revision A·August 2026·See it in the tour

Cold ground, colder sky, and no air to carry the heat

There is no air to carry heat away, so every watt the base generates has to be radiated into the sky. At the Shackleton rim the sun never climbs more than about 1.5 degrees above the horizon, the sunlit ridge averages near 200 K in summer, with Diviner's summer maximum map reaching 220 to 300 K along it, and falls to 50 to 70 K in winter, and a dark spell of a day or more can come at any point in the month. So the design is two loops, water inside and ammonia outside, vertical radiators on every module, and a salt hydrate buffer that holds the lines liquid for eleven hours without power.

220 to 300 Ksunlit ridge, summer maximum
50 to 70 Kthe same ridge, winter minimum
46 kWpeak heat rejection
Contents
  1. Why vacuum makes this hard in both directions
  2. The heat budget
  3. The loop
  4. Radiators
  5. Surviving the night
  6. Phase change buffer
  7. Dust, and why it matters more here than anywhere else
  8. Failure modes
  9. What is not yet known
  10. Increment plan
  11. Sources and further reading
Section 01

Why vacuum makes this hard in both directions

On Earth almost all waste heat leaves a building by convection. In vacuum there is no convection, so the only path out is radiation, and radiation scales with the fourth power of absolute temperature. That sounds generous until you notice it also means a radiator running near room temperature is a very poor emitter.

The base has to reject about 46 kW at peak. A radiator at 20 °C with an emissivity of 0.92 radiating into a 3 K sky sheds about 385 W per square metre, before you subtract what it absorbs back from the ground and from the low sun. That is why the radiators on this design are large, vertical, and pointed at the sky rather than at the surface.

The other direction is worse. Whenever the sun drops behind the rim, and through the polar winter when the ridge itself sits at 50 to 70 K, every square metre of habitat skin is a heat leak. Survival heating through a dark spell costs power the array is not making.

385 W/m²radiator at 20 °C, emissivity 0.92
46 kWpeak rejection
118 m²radiator area installed
6.2 kWnight survival heating
Section 02

The heat budget

Where the heat comes from, at peak ISRU plant 13.1 kW process heat, the largest single source Greenhouse lighting 12.6 kW almost all of it ends as heat in the bay Crew and metabolic 0.5 kW 4 people at about 144 W each, NASA BVAD Avionics and comms 2.4 kW Life support machinery 3.1 kW Power conversion losses 4.4 kW the price of a 120 V DC bus Solar absorbed on the hull 9.9 kW what the shielding does not stop 46.0 kW at peak. Two thirds of it is process and lighting, both of which can be throttled.
The crew are almost irrelevant thermally, at a little over half a kilowatt between them; NASA's baseline document puts the total metabolic heat load at 12.4 MJ per crew member per day, about 144 W. Modern horticultural diodes turn 40 to 90 percent of their electricity into photons, but the plants store only a small fraction of what lands on them and the rest ends as heat in the bay, so the lighting line is nearly the whole 14 kW. What actually drives the radiator sizing is the plant, the grow lights, and sunlight landing on the hull.
Section 03

The loop

Modules internal loop, water ISRU plant high grade, 320 °C Interface HX water to ammonia Pump package dual string Heat pump lifts to 45 °C Radiators 118 m² vertical Phase change salt hydrate buffer water ammonia reject buffer
Two fluids, deliberately. Water inside the pressure vessel because a leak of ammonia into a crew module is a fatal event, and ammonia outside because it stays liquid across the range the external loop sees and water in an external line would freeze in the first dark spell.
The single most important design rule here

No ammonia inside the pressure boundary, ever. The interface heat exchanger (HX) sits in the connector, outside the habitable volume, and is the only place the two fluids meet. This is the same rule the International Space Station follows, for the same reason.

Section 04

Radiators

The radiators are mounted vertically on the flanks of each module. At the equator a horizontal radiator spends the day looking at ground near 120 °C and loses much of its output to it. Here the ground is cold, near 200 K on the sunlit ridge on a summer average and 220 to 300 K at the Diviner summer maximum, and far colder in shadow, so a vertical panel sees sky and cold ground and works well. The catch is the sun. It sits within about 1.5 degrees of the horizon and circles the whole sky once a lunation, so no fixed vertical face is edge on to it all month. Keeping the sun off the panels is an open design point, listed below.

Each module carries a pair sized for its own load, rather than a single central farm. That costs about 15 percent more area in total and buys the ability to lose any one module without losing the cooling for the rest.

ElementAreaRejectsRadiator temperatureNote
Core radiatorstwo wings34 m²13.2 kW20 °CSized for crew, avionics and galley
Greenhouse radiatorstwo wings32 m²12.6 kW22 °CMatched to the diode load
Laboratory radiatorstwo wings14 m²5.4 kW18 °CIncludes the freezer reject
Airlock and cupolaone wing each10 m²3.7 kW20 °C
ISRU plant radiatorstandalone28 m²13.1 kW95 °CHigh grade heat, so a smaller panel does more
Total118 m²48.0 kW4 percent margin on the 46 kW peak

The ISRU radiator, serving the in situ resource utilisation plant, is the interesting one. Because its loop runs at 95 °C rather than 20, it rejects nearly as much heat as the core does from a smaller panel. At 95 °C and the same emissivity a panel sheds about 960 W per square metre, so 28 square metres could carry roughly twice the 13.1 kW listed; the surplus is margin for dust and for sun on the face. Radiating at the highest temperature the process will tolerate is the cheapest thing you can do in a thermal design, and it is why the plant does not share the habitat loop.

Section 05

Surviving the night

Equatorial night, not this site minus 180 minus 120 minus 60 0 60 120 0 2 4 6 8 0 5 10 15 20 25 29.5 Days through one lunation Degrees C Kilowatts Surface temperature Survival heating
Upper panel, surface temperature. Lower panel, the heating the base draws to stay warm. This is the equatorial reference case, plus 120 to minus 170 °C across one lunation, kept because it is the one most readers know. It is not this site. On the Shackleton rim the sunlit ridge sits between about 220 and 300 K in summer and 50 to 70 K in winter, and the dark comes as spells of hours to a few days set by the local relief rather than one fourteen day night. In those spells the base spends 6.2 kW simply keeping fluid lines above freezing and the crew volume habitable. That heating load is the reason the fission unit is sized at 40 kWe rather than 30. For comparison, NASA's Lunar Terrain Vehicle project designs to a 150 hour night on the same ridge, chosen because a rover that chases the sun can cut its dark to about 36 hours but gives up too much science to do so.
The failure that ends the mission quietly

A frozen coolant line is unrecoverable in the field. Every external run is trace heated, the heaters are on the essential bus, and the phase change buffer holds enough energy to keep the lines liquid for eleven hours with no power at all. That eleven hours is the single number the night architecture is designed around.

Section 06

Phase change buffer

A salt hydrate buffer sits between the loop and the radiators. It absorbs the peaks so the radiators can be sized for the average rather than the maximum, and it holds the base through short losses of power without the lines freezing.

The material is Glauber's salt, sodium sulfate decahydrate. It melts at 32.4 °C and the literature puts its latent heat at 239 to 254 kJ per kilogram; the buffer is sized here at 180 kJ per kilogram, below that, which leaves margin. Even so it holds far more than the same mass of water would as sensible heat over the same range.

620 kgbuffer mass
112 MJlatent capacity
32.4 °Cmelt point
11 hhold with no power
Section 07

Dust, and why it matters more here than anywhere else

A radiator works by having a high emissivity and a low solar absorptivity. Regolith dust has the opposite of both. A dusted radiator absorbs more sunlight and emits less of its own heat, so contamination attacks the system from both ends at once.

On Apollo 16 and 17 the rover batteries ran over their temperature limits because dust on their radiators could not be brushed off, and John Young said afterwards that he regretted the time spent trying. On a ten year outpost that is not a nuisance, it is a design driver. The radiators here are vertical, which sheds most settling dust, and carry the same electrodynamic clearing the solar array uses, which NASA demonstrated on a radiator surface on Blue Ghost in March 2025. The table below is a design estimate anchored to the clean figure, not a measurement; the Apollo record gives the direction and the seriousness, not these numbers.

ConditionAbsorptivityEmissivityNet rejectionLoss
Cleanas installed0.090.92385 W/m²none
Light dustone lunation0.140.88353 W/m²8%
Moderatesix lunations, uncleared0.260.79283 W/m²27%
Heavytwo years, uncleared0.410.68203 W/m²47%
Section 08

Failure modes

FailureEffectTime to impactResponse
Pump package failsone of two stringsHalf the loop capacityHoursSecond string carries the habitat. ISRU and greenhouse shed.
Ammonia leakexternal loopLoss of external rejection2 hIsolate the affected branch. Phase change buffer holds while the crew reconfigure.
Radiator puncturemicrometeoriteLocal lossSlowEach wing isolates. Losing one wing costs about 12 percent of capacity.
Trace heater failurein a dark spellLine freezes40 minRedundant heaters on the essential bus. The line is drained if both fail.
Interface HX foulinggradualReduced transferMonthsScheduled flush. The reason the internal loop is water and not something exotic.
Section 09

What is not yet known

The sun circles the horizon once a lunation within about 1.5 degrees of it, so no fixed vertical radiator is edge on to it all month; how the panels are shaded or turned has not been decided, and it bears on the 118 square metre figure. The longest dark spell at the site has not been computed for the exact position. The 240 m resolution Lunar Orbiter Laser Altimeter (LOLA) model gives the best Shackleton rim site about 1.5 days and the 20 m model gives the best rim clusters 65 to 66 hours, so the 11 hour buffer and the 6.2 kW survival load have to be shown to cover a spell of days on the fission unit alone. The dust table is a design estimate; the Apollo record gives the direction, not these numbers. The salt hydrate buffer assumes its latent heat holds over hundreds of cycles, which has not been shown in a flight unit. The power conversion loss here, 4.4 kW, does not match the 1.1 kW the power document carries, and the two have to be reconciled.

Section 10

Increment plan

Increment 1, habitat loop only

Water inside, ammonia outside, 90 square metres of radiator sized for the habitat alone, the four module rows in the table above. No ISRU load yet, so the peak is about 35 kW.

Increment 2, plant loop and buffer

The high grade ISRU loop at 95 degrees, its own radiator, and the phase change buffer that lets the whole system ride out a power interruption.

Increment 3, dust mitigation

Electrodynamic clearing on every radiator face. This is the step that stops the uncleared degradation the table above estimates.

Increment 4, capacity for construction

The sintering gantry adds 9 kW of intermittent load with a very high grade reject. It gets its own small panel rather than being plumbed into anything.

Sources

Sources and further reading

Every figure in this document traces to one of these. Agency documents and peer reviewed work first, reporting only where it is the primary record.

NASA, International Space Station active thermal control system overview nasa.govPrecedent for the two loop, water inside and ammonia outside architecture
Williams et al., Seasonal polar temperatures on the Moon, JGR Planets, 2019 https://doi.org/10.1029/2019JE006028Diviner seasonal maps of the poles: the Shackleton to de Gerlache ridge systematically high, near 200 K, in summer; the 1.54 degree spin axis tilt
NASA, Wheel module motor trade study for the Lunar Terrain Vehicle thermal control, 2024 https://ntrs.nasa.gov/citations/20240004621Reads the Diviner maps for the Shackleton to de Gerlache ridge: summer maximum 220 to 300 K along the ridge, winter minimum 50 to 70 K, a summer peak near 150 K on average at 89 degrees south, a polar average near 98 K outside shadow and about 25 K in the coldest shadow; also the 150 hour night the Lunar Terrain Vehicle is designed to survive
Mazarico et al., Illumination conditions of the lunar polar regions using LOLA topography, Icarus, 2011 https://ntrs.nasa.gov/citations/20120010094Shackleton rim site: longest dark spell about 1.5 days
Gläser et al., Illumination conditions at the lunar poles: implications for future exploration, Planetary and Space Science, 2018 https://ntrs.nasa.gov/api/citations/20170007365/downloads/20170007365.pdfLongest shadow 65 to 66 hours at the Shackleton rim clusters at 20 m per pixel
Gaier, The effects of lunar dust on EVA systems during the Apollo missions, NASA TM 2005 213610 https://ntrs.nasa.gov/citations/20050160460Rover battery overheating on Apollo 16 and 17 from dust on the radiators
NASA, dust shield successfully repels lunar regolith on the Moon, Blue Ghost, March 2025 nasa.govElectrodynamic clearing demonstrated on glass and on a thermal radiator surface
NASA, Life support baseline values and assumptions document, revision 2, 2022 https://ntrs.nasa.gov/citations/20210024855Table 3 31: total metabolic heat load 12.426 MJ per crew member per day
Kusuma, Pattison and Bugbee, From physics to fixtures to food: current and potential LED efficacy, Horticulture Research, 2020 https://pmc.ncbi.nlm.nih.gov/articles/PMC7105460/Electrical to photon conversion from 42 percent for green to 93 percent for blue diodes
Hirschey et al., Review of inorganic salt hydrates with phase change temperature in the range of 5 to 60 C, Purdue conferences, 2018 https://www.osti.gov/servlets/purl/1468092Sodium sulfate decahydrate at 32.4 C with 239 to 254 kJ per kilogram