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Could a Biocrust Harvest the Moon's Wandering Water?

There is water moving across the surface of the Moon right now. It's not something that would look familiar to us. The water moves as singular, isolated molecules sublimating, transitioning directly from a solid to a gas, from cold surfaces. They launch across the Moon's near vacuum in slow ballistic arcs, occasionally sinking a few centimetres into the soil before the temperature takes them permanently. It could be a resource that something might be able to intercept before it's destroyed.

That water exists as ice at the lunar poles

At some point the ice meets warmer temperatures and is slowly turned to a gas. This water vapour is in a constant slow transit. Some of it hops across the lunar surface, sailing for hundreds of kilometres, landing somewhere else until it's either destroyed by UV light or lands somewhere cold enough to stick.

Some of it sinks, diffusing down through the loosely packed grains of the lunar regolith, which experiences the daily heating and cooling cycle, until it reaches an area cool enough to freeze. Scientists call this vapour pumping.

Could a biological crust compete with physics?

Imagine a biocrust: a thin, resilient, biologically structured layer of lunar soil at the surface, similar to the crusts of cyanobacteria, lichen and fungi that carpet deserts on Earth and pull moisture out of humid air.

This biocrust could be better at catching the water vapour bouncing across the surface than the lunar regolith minerals are, and this could work in various ways. It could interrupt the hop by capturing the water on the large surface area of the crust. It could capture it with a specialised coating that is hygroscopic, basically sticky enough to hold on to the water molecule. Or it could be present at a specific depth so that it functions as a sink that actively draws moisture towards itself.

Why it's worth thinking about

New things are being discovered about the Moon all the time. A lot of what we treat as settled was actually decided decades ago. The main theories about lunar ice date back to 1961 and 1979, and right up to 2009 people were confident the Moon was completely dry. Then the LCROSS mission crashed into a crater near the pole, threw up a plume of debris, and found water in it. A certainty just dissolved.

In a different study carried out in the past few years, regarding a different process on the Moon, scientists from Manchester estimated that 270 billion tonnes of water are locked inside glass beads in the lunar soil alone.

It's worth taking a moment to think about. When we've ruled out the possibility of life somewhere for reasons such as "there's no water there," and that reason later turns out to be questionable, the response isn't to assume life is likely. It's to realise that the original thinking doesn't hold up the way it used to. At that point, the responsible step is to reopen the question.

References & further reading
Hu, S., He, H., Ji, J. et al. (2023). "A solar wind-derived water reservoir on the Moon hosted by impact glass beads."
Nature Geoscience. The Chang'e-5 study estimating that lunar soils may hold at least 270 billion tonnes of solar-wind-derived water within impact glass beads, cycling in and out over a few years. Led by Nanjing University and the Chinese Academy of Sciences, with co-authors at the University of Manchester and the Open University.
nature.com/articles/s41561-023-01159-6
NASA (2023). "NASA's LRO Sheds Light on Lunar Water Movement."
Describes how water molecules stay bound to the regolith until surface temperatures peak near lunar noon, then thermally desorb and hop to nearby colder locations, more common at higher latitudes.
nasa.gov · LRO lunar water movement
NASA (2009). "LCROSS Impacts Confirm Water in Lunar Crater."
The Lunar Crater Observation and Sensing Satellite impacted Cabeus crater near the south pole on 9 October 2009, and its instruments confirmed water in the ejecta plume, overturning the earlier view of a dry Moon.
lpi.usra.edu · LCROSS water found
Exploring the lunar water cycle (2024). PNAS.
A review of how water migrates across the lunar exosphere through ballistic hops, and the sink mechanisms, including cold trapping and burial by regolith, that remove it from the surface.
pnas.org/doi/10.1073/pnas.2321065121
Historical background on lunar ice theory.
The idea that water molecules migrate to polar cold traps by ballistic hopping traces back to Watson, Murray & Brown (1961), with later development by Arnold (1979). These early theoretical papers underpin the modern picture of lunar water transport.
Review: Space Science Reviews (2021)
Note: the biocrust concept in this post is a personal thought experiment and is not drawn from any of the papers above. Those are cited for the underlying physical facts about lunar water only.