I was reading a science-fiction novel, Limit, by Frank Shätzing. It depicts a near-future with useful helium-3 fusion, and the Americans and Chinese are bumping elbows mining helium-3 on the moon, large robots scooping up and processing lunar soil. At one point, one of the characters did some calculations assuming a certain rate of population growth and a certain increasing energy demand, and decided that if the entire surface of the moon were processed it would last for 700 years. Then we would have to find another supply.

It was discussed as a non-renewable resource. But the sun is still shining, blowing out the solar wind. And whatever helium-3 is bound up on the surface, I assume it must be diffusing away and has to be continually replenished anyway. It seemed like it should be renewed eventually. But I haven't found any discussion of that.

  • $\begingroup$ If the answer given below satisfies your needs, don't forget to accept it by clicking the check mark. $\endgroup$
    – DrSheldon
    Commented Jul 5, 2019 at 5:58
  • $\begingroup$ @uhoh I certainly did. Looks like a bit of work went into it, too! $\endgroup$
    – Greg
    Commented Jul 6, 2019 at 9:38

2 Answers 2


Interesting question!

A quick check of Wikipedia's Helium-3 introduction says:

The abundance of helium-3 is thought to be greater on the Moon than on Earth, having been embedded in the upper layer of regolith by the solar wind over billions of years, though still lower in abundance than in the solar system's gas giants.

but let's not assume that Wikipedia is the last word on the topic.

According to NASA's Elemental and Isotopic Abundances in the Solar Wind; An invited review by Johannes Geiss:

                     Apollo 11              Apollo 12
                           flux in cm^-2 sec^-1

He4 - Flux      6.2 +/- 1.2 × 10^6     8.1 +/- 1.0 × 10^6
He3 - Flux      3.3 +/- 0.7 × 10^3     3.3 +/- 0.4 × 10^3 

3300 atoms/sec/cm^2 is 0.0005 mole/sec over the Moon's surface, which is about 16,000 moles/year or about 49 kg/year.

According to the abstract of Global inventory of Helium-3 in lunar regoliths estimated by a multi-channel microwave radiometer on the Chang-E 1 lunar satellite:

The global inventory of 3He was estimated as being 6.6×10⁸ kg; 3.7×10⁸ kg for the lunar nearside and 2.9×10⁸ kg (660 million kilograms) for the lunar farside.

At a rate of 49 kg/year assuming 100% capture efficiency, it would take about 13 million years to reach a total of 6.6×10⁸ kg. A nominal solar wind velocity of order 100 km/sec for example corresponds to a helium-3 kinetic energy of about 50 eV, so we can think of the captured atoms as being "implanted" a few nanometers or more down into whatever surface it first hits, which is a fairly shallow and delicate location for a noble gas atom.

Therefore, thinking that it would only take of the order of 13 million years to replenish the Moon's helium-3 would be naive because there are several competing processes. The far higher flux of protons in the solar wind, cosmic rays, and micrometeorites all can disturb the regolith and release trapped noble gasses like helium, and atoms with escape velocity can return to space.

So the answer is probably between tens of millions and the canonical, Sagan-esque "billions" of years.

  • 2
    $\begingroup$ Wow! So it really is non-renewable. But speaking of gas giants, a standard maneuver in the Traveller role-playing game is to send a dedicated shuttle from your starship to refine fuel from local gas giants. They were vague about what that involved, but you know, it's just a game. A little more in the "hard" direction, they didn't want it to be as easy as in Star Wars. How long the helium-3 reserves in Jupiter would last us would be, well, I suppose a challenging question because it matters how much is accessible. $\endgroup$
    – Greg
    Commented Jul 4, 2019 at 20:17
  • 1
    $\begingroup$ All this makes me wonder how deeply into the lunar regolith has He-3 penetrated & are the reported estimates of quantities of lunar He-3 accurate, particularly given the sparsity of deep drilling data from the Moon. $\endgroup$
    – Fred
    Commented Nov 15, 2020 at 23:55
  • 1
    $\begingroup$ @Fred yes indeed. The penetration depth will be microscopic, however there may be significant churning and/or overturn of regolith by micro- and not-so-micro meteor impacts over these timescales. It's an interesting and not-so-simple problem. $\endgroup$
    – uhoh
    Commented Nov 16, 2020 at 0:01

Man Made Production

It's worth pointing out that He-3 is also a decay product of H-3, and that H-3 can be produced from neutron bombardment of various common elements with various energy neutrons. (notably Lithium, Boron, and H-2)

Since high energy x-rays can produce photoneutrons, there's the possibility for producing He-3 on the Moon that looks something like:

  1. Solar Panels collect abundant solar energy
  2. Solar Energy is used to produce high energy X-rays
  3. X-rays are used to produce neutrons
  4. Neutrons transform Lithium, Boron, and/or H-2 into H-3
  5. H-3 decays into He-3
  6. He-3 is stable, and is exported to places where solar is not feasible

Is it economical? Probably not. H-3 has a 12 year half-life, so this whole plan is something of an investment just from time involved.

But H-2 and Solar Energy are probably the two most abundant resources in the solar system, so this feels pretty "renewable." And it would be sensible to do this on the Moon where Solar is more effective, and storing radioactive materials for a couple decades is less scary.


Your Answer

By clicking “Post Your Answer”, you agree to our terms of service and acknowledge you have read our privacy policy.

Not the answer you're looking for? Browse other questions tagged or ask your own question.