SpaceCarrier

GC-L1 · a Galaxy Campaign
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Ship yard

Engine
Engine count 6,750 kN total
3
8.89 km/sΔv with this cargo, tanks full
9.50 km/sΔv with no cargo
102 tDry mass
1,322 tTotal mass, full
Moon 3.2 · Mars 1.4Thrust / weight
Δv = Isp · g₀ · ln(m₀ / m₁)  ·  380 s × 9.81 × ln(1322 / 122)
propellant50 m
Length ≈ 38 m · diameter 9 mTank volume 1,446 m³ of liquid methane + oxygen

Methalox can be made on Mars from CO₂ and water, but not on the Moon: lunar ice holds almost no carbon.

Δv route map

EARTHMOONMARS→— ←0.1→3.1 ←0.10.81.9→3.2 ←0.10.10.6→0.3 ←2.1→0.7 ←4.1Earth surfaceLow Earth orbitdepot onEarth–Moon transferLow lunar orbit100 km+ depotLunar south poleg 1.62 · moonel site+ depotEarth escapeMars transferLow Mars orbitMars surface+ depot
Earth systemMoonMarsYour routeNumbers: Δv in km/s for this ship (→ outbound, ← inbound) · — = this ship can't fly that legClick a depot tag to switch refuelling on or off · click a stop to fly there

The lunar south pole is the moonel site: Campaign 01's outpost. Plan the outpost on moonel.com → (opens in a new tab)

Mission manifest

Mission worksDelivers 20.0 t to Lunar south pole, with 157 t of propellant left (13% margin).
5.80 km/s
Route Δv
1,043 t
Propellant burned
1,200 t
From Earth
0.00 t
Made in space
3.1 d
Travel time
full 1,200 tcumulative Δv →
LegΔv km/sBurned tLeft in tanks tShip mass tTime
Low Earth orbit → Earth–Moon transfer3.10746.5453.5575.32.5 d
Earth–Moon transfer → Low lunar orbit0.80111.1342.3464.112 h
Low lunar orbit → Lunar south pole1.90185.4157.0278.81 h
▼ Deliver 20 t of cargo157.0258.8

Δv values are typical figures from published Δv maps, rounded (patched conics, no gravity assists, no margins). Mars legs assume a Hohmann transfer (~259 days); launch windows open about every 26 months. Low-thrust legs use the Edelbaum approximation (Δv ≈ difference of circular speeds), and burn time = mass × Δv ÷ thrust. Engine classes are illustrative, based on published figures for RS-25, Raptor, NERVA and 100-kW-class Hall thrusters. Lunar water gives hydrogen and oxygen only; Mars air plus water gives methane, oxygen and hydrogen (Sabatier process). Sources for every figure →

How the calculator works

Moving cargo between worlds

What Δv means

Δv (delta-v) is the change in velocity a spacecraft has to produce with its engines to get from one place to another. It is the currency of spaceflight: every manoeuvre has a price in metres or kilometres per second, and the prices add up along a route. Reaching low Earth orbit costs about 9.4 km/s once air drag and gravity losses are included, even though the orbital speed at 400 km is only 7.7 km/s. From there, about 3.1 km/s more sends a ship towards the Moon, 0.8 km/s puts it into a low lunar orbit and 1.9 km/s brings it down to the surface.

The route map above shows those prices on each leg. They are typical values from published Δv maps, rounded to 0.1 km/s. Where a planet has an atmosphere, a heat shield lets the ship brake against the air instead of burning propellant: dropping from the Mars transfer into low Mars orbit falls from 2.1 km/s to about 0.3 km/s, and landing on Mars from 4.1 km/s to about 0.7 km/s.

How to read the rocket equation

The calculator turns Δv into propellant with the Tsiolkovsky rocket equation:

Δv = Isp · g₀ · ln(m₀ / m₁)

Isp is the engine’s specific impulse in seconds, a measure of how efficiently it uses propellant. Multiplied by standard gravity g₀ (9.81 m/s²) it gives the exhaust velocity. m₀ is the ship’s mass before the burn and m₁ its mass after. Because the masses sit inside a logarithm, each extra km/s costs more propellant than the last.

A worked example: a methane–oxygen engine with an Isp of 380 s has an exhaust velocity of 3.7 km/s. To fly the 5.8 km/s from low Earth orbit to the lunar south pole, m₀ / m₁ has to be e5.8 / 3.73 ≈ 4.7. In other words, about 79% of the ship’s mass at departure must be propellant, and only the remaining 21% can be structure, engines and cargo. A hydrogen–oxygen engine at 452 s needs a mass ratio of about 3.7 for the same trip, but liquid hydrogen is so thin (71 kg/m³) that its tanks are larger and heavier.

Why making propellant in space changes everything

If every tonne of propellant has to be launched from Earth, it first pays the 9.4 km/s toll to reach orbit. A depot that makes propellant where it is used breaks that chain. The calculator counts this as “made in space”: try the “refuel on the Moon” example and more than 800 t of the propellant burned comes from the lunar surface instead of from Earth.

What a depot can make depends on what is there. The Moon’s permanently shadowed polar craters hold water ice; at Cabeus crater, the LCROSS impact measured about 5.6% water by mass. Water splits into hydrogen and oxygen, so a lunar plant can supply hydrogen–oxygen ships and nuclear-thermal ships that run on pure hydrogen. It cannot supply methane, because there is very little carbon on the Moon.

Mars is different. Its atmosphere is 95.1% carbon dioxide. Combining that carbon dioxide with hydrogen from Martian water ice in the Sabatier reaction (CO₂ + 4 H₂ → CH₄ + 2 H₂O) produces methane, and splitting the water gives oxygen. NASA’s MOXIE experiment on the Perseverance rover has already made oxygen from Martian air, 122 g in total. That is why methane–oxygen ships make sense for Mars: they can refuel for the trip home on arrival.

Low thrust versus high thrust

Chemical engines are high-thrust. An RS-25 pushes with about 2,280 kN, enough to lift a heavy lander off the Moon in minutes. Their weakness is efficiency: Isp stays below about 460 s.

Electric thrusters are the opposite. A Hall thruster ionises xenon and accelerates it electrically to an Isp of 2,000–2,600 s, so the same Δv needs far less propellant. But thrust is tiny: NASA’s 100-kW-class X3 thruster produced 5.4 N. A cargo tug with a megawatt of power accelerates at a few hundred-thousandths of a g, so instead of a short burn it spirals outwards for months. That spiral also costs more Δv. The calculator uses the Edelbaum approximation, where the cost is roughly the difference between the two circular orbital speeds: about 7.7 km/s to escape Earth from low orbit, against 3.2 km/s for a chemical burn. Electric ships can never land or take off, so the calculator blocks those legs.

Nuclear-thermal engines sit in between. NASA’s NERVA engine was designed for about 825 s and 334 kN (75,000 lbf), and ground-tested reactors of the 1960s reached 825–850 s, but no nuclear rocket has flown.

Questions

How much Δv does it take to land on the Moon from Earth?

About 15.2 km/s in this model: roughly 9.4 km/s to reach low Earth orbit, then 3.1 km/s for trans-lunar injection, 0.8 km/s to enter low lunar orbit and 1.9 km/s to land. From a depot in low Earth orbit the remaining cost is 5.8 km/s. These are rounded Δv-map figures without margins.

Why can't a methane rocket refuel on the Moon?

Methane needs carbon. Lunar polar ice gives water, which splits into hydrogen and oxygen, but the Moon has very little carbon to make methane from. Mars has an atmosphere that is 95.1% carbon dioxide, so a plant there can combine it with hydrogen from water to make methane and oxygen (the Sabatier reaction). In the calculator only hydrogen–oxygen and pure-hydrogen ships can refuel at the lunar depots.

Why not use electric propulsion for everything?

Electric thrusters are five to six times as efficient as the best chemical engines, but they push with newtons rather than meganewtons. NASA's 100-kW-class Hall thruster produced 5.4 N in tests. That is enough to spiral a cargo tug between orbits over months, but far too little to take off from or land on any surface, so an electric ship always needs a chemical lander at each end.

How accurate are the results?

They are first-order estimates. Δv values are typical published figures rounded to 0.1 km/s, with no gravity assists, launch-window penalties or safety margins. Engine classes are based on real engines (RS-25, Raptor, NERVA, 100-kW-class Hall thrusters), but structure, tank and heat-shield masses are round assumptions. Use it to compare options, not to size a real vehicle.

Can I share a mission?

Yes. The ship design and route are stored in the page address, for example /carrier?eng=hydrolox&n=2&prop=900&cargo=80&from=leo&to=moon&depots=leo,moon&round=1. Copy the address or use the copy-link button and anyone who opens it sees the same mission.