I've always been surprised to hear that the moon is a dead world with no water at all on its surface.
Now, the recent finding of water radically changes our approach of the moon.
If there is water in the soil, that implies that water has the ability to infiltrate into the dusty soil of the moon instead of vanishing into outerspace.
You see what I mean!
The prospect of a network of caves carved by liquid water beneath the surface of the moon can be envisaged.
You may find a similar pressure to that of the Earth at sea level about 30 meters beneath surface level on the Moon.
What are the thermal conditions at this depth? Can water appear in its liquid form?...
No. This is what I think based on existing data.
Sorry, but I would call that unlikely to the point of impossibility. Even a pond-sized, very localized underground aquifier would produce a global water signature many orders of magnitude greater than that observed due to transpiration through bedrock cracks & the loose regolith and subsequent diffusion through what passes for the lunar atmosphere.
Transient lunar phenomena (TLP) have been documented occasionally over the years, and some (esp. in the Aristarchus region) do seem to be related to gas emissions, the rest probably being meteor impacts. However, the only spectrum (hastily!) obtained for a TLP reportedly did not show H2O or OH.
Mike, just to be clear I was thinking about the detectability of an underground liquid reservoir as postulated in the first post. Could be wrong, but it seems to me that such a thing would be emitting water vapor like crazy even via diffusion through many meters of soil, so I sincerely doubt that any exist.
Subsurface ice, now....wouldn't that be nice?
The paper on concentrations of salts in soil on Mars should give the clue that this will not work on the Moon. There is, as far as we can see now, no evidence in samples or orbital chemical data of solution of salts from one place and deposition in another. That's the proof that water on the Moon is not behaving as it does on Earth or Mars. Caves eroded by flowing water are out of the question. The recent findings are very different from active aquifers and masses of ground ice. Even at the poles the ice is not active in the landscape as it is on Mars.
Phil
Lunar water is present only in regions of incredible cold. As a rule I can't imagine subsurface regions that would accumulate water being warm enough for it to melt.
I can imagine liquid water forming in the subsurface as a very rare and short lived event, for example if a subsurface volatile resevoir were close enough to a major impact to be warmed above freezing without being totally driven off or disrupted. But this would be more like a short lived pond of subsurface slurry, and would either quickly re-freze or, if there was enough impact heat to keep the subsurface warm over a longer period, be driven from the regolith as vapour.
There have been studies of impact induced hydrothermalism on Mars I believe- perhaps these might provide some further insight? There may be enough similarities for the two situations to be meanigfully compared.
Even if it transpires that impact induced hydrothermalism could work on the moon such events are likely to be rare in its history and therefore it is unlikely that such a body of water would be currently present.
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