Motivation
The moon is rich in a few important natural resources, namely:1 2
Stuff |
Context |
Amount |
Utility |
Challenges |
water |
data from orbiters indicate that the poles – particularly the South Pole – are rich in ice water. the water may have evolved on the moon naturally or deposited through bombardment by water-rich meteor strikes. |
31,059 km2 of permanently shaded areas may be covered by thin ice coatings |
can be used for rocket bi-propellant fuel |
1. thick ice sheets might not exist, 2. it's an exhaustible resource. |
sunlight |
certain areas of the polar South Pole receive nearly constant light, while still being close to water ice sources. |
virtually unlimited supply |
solar cell arrays can capture the sunlight, establishing permanent crewed bases on the surface |
|
3He isotope |
solar winds have implanted this isotope onto the regolith |
1m tonnes, but that's still 10-20 ppb |
can be used for nuclear fusion |
1. extraction might not be feasible, 2. extraction, if feasible, requires tonnes of processed regolith in order to acquire 1 g of 3He, 3. current fusion reactor prototypes use more energy than produced, 4. it's an exhaustible resource |
N |
- |
5 ppm in the regolith |
nutrient required for farming in a biosphere |
1. very limited quantities, 2. it's an exhaustible resource |
C |
originates from solar winds and micrometeorite impacts |
82 ppm in the regolith |
required for farming; production of lunar steel |
1. very limited quantities, 2. it's an exhaustible resource |
Si |
the three most common minerals on the moon – plagioclase feldspar (usually anorthite), pyroxene, and olivine – all have Si in them. |
21% of lunar surface materials by mass |
glass, fiberglass, and ceramics; solar cells; perhaps as semiconductive material if it can be purified enough |
1. achieving purity to be used in solar cells and electronic chips could be challenging, 2. would require breaking down the minerals listed. |
Al |
it's in anorthite |
13% of the highlands by mass / 5% of the masa |
it's a good electrical conductor; it can also be burned for propulsion fuel |
1. would require breaking down plegioclase |
Ca |
it's in anorthite |
10% of the highlands / 8% in the masa |
ceramics; it's a good electrical conductor in some situations; can be used to help make solar cells |
1. would require breaking down plegioclase |
Fe |
the iron in pyroxene, olivine, and iron-titanium minerals like ilmenite is all in the ferrous (2+) oxidation state, compared to iron on Earth which is also sometime in (3+) state. some of the iron on the moon is metal, often Fe-Ni, deriving from meteorite impacts. |
5% of the highlands / 15% of the masa; also, 0.5% of the regolith by mass |
steels and alloys; dust: parts made through powder metallurgy |
1. would require breaking down the minerals listed. |
Mg |
nearly all is in pyroxene and olivine. for (+2) Mg, the same is true about what was said of (+2) Fe. |
5.5% |
applications as an alloy in aerospace, automotive, and electrical applications |
1. would require breaking down the minerals listed. |
Ti |
there are basalts that contain a massive quantity of Ti, in the form of ilmenite, which it is 5-8% by mass. this is 10x as much Ti as Earth rocks. |
< 1% in highlands and between 1-5% in the masa |
alloys for lightweight spacecraft |
1. would require breaking down ilmenite; 2. it's an exhaustible resource |
REM / lanthanides |
rare earth elements, though common, are often very dispersed on our planet, and mineral deposits are rare; as a result, China extracts the vast majority of REM. |
rare |
depends on the element, but various industrial uses, including optical and ferromagnetic ones; automotive industry; "green technologies". extraction on the moon could end pure dependence on China |
1. identifying deposits; 2. extraction |
Note that many of these are in very small supply by mass, and effectively acquiring them completely would not alter the moon's mass materially. Much of the ppm and percentages I provided are for the surface-level only; the deeper layers may never be touched at all.
Helium
The last person to walk the moon was a geologist named Jack Schmitt, who studied the composition on the moon. He's essentially the only natural or physical scientist who's stepped foot on the moon. He has since written a book, Back to the Moon (2007), which he proposes long-term renewed exploration and expedition to the moon, revolving around the nucleus of mining 3-He for energy production purposes as socioeconomic justification for such return. Demonstrating a political bias, he also delved into the goriness of a pro/con analysis of various private or public methods of achieving this, positing that some are better than others, and arriving at the dubious result that the private sector was the superior solution to this. In order for the detailed plans for lunar mining to be successful, it would need to attract significant private-sector investment, according to him,3 and the legality of who has claim over hypothetical mining operations remains unclear (theoretically nothing seems to prevent private ownership; the 1967 UN Outer Space Treaty only prevents political ownership).3 4
Either way, assuming that we could extract and find a way to use the Helium for fusion as a solution to the eventual decline of fossil fuel quantities available, and as a way to stem the effects of greenhouse gas emissions, the amount of Helium that would be extracted would only be a few hundred thousand tonnes at most, which is insignificant w.r.t. to the mass of the moon.
Extracting other elements
The moon is 73q tonnes, so assuming 1 metric ton removed each day, it would take 220 million years to deplete just 1% of the mass.4
Source: 911 Metallurgist, as posted by JPL NASA4
Need to make a cost-benefit determination as to whether or not the risks involved in causing some level of altered orbit or affecting gravitational tides is worth the value produced from extracting the natural elements on the moon. It appears that the risk is very low, assuming the rate of removal is steady and slow. For some things, such as REM / lanthanides, the risk/reward ratio looks fairly attractive because they are valuable but only represent a trifling small proportion of the mass. But the same could be said about Titanium, Iron, and Silicon near the surface.