Water ice ‘detected on Moon’s surface’

Water ice on the MoonImage copyright NASA
Image caption The distribution of surface water-ice at the Moon’s south pole (left) and north pole (right)

Scientists say they have definitive evidence for water-ice on the surface of the Moon. The ice deposits are found at both the north and south poles, and are likely to be ancient in origin.

The result comes from an instrument on India’s Chandrayaan-1 spacecraft, which explored the Moon between 2008 and 2009.

Details of the work have been published in the journal Proceedings of the National Academy of Sciences (PNAS).

The distribution of the ice deposits is patchy. At the lunar south pole, most of the ice is concentrated in craters. At the northern pole, the water-ice is both more sparse and more widely spread.

The Moon Mineralogy Mapper (M3) instrument aboard Chandrayaan identified three specific signatures of water-ice at the lunar surface.

M3 not only picked up the reflective properties one would expect from ice, but was able to directly measure the distinctive way its molecules absorb infrared light. This meant that it could differentiate between liquid water and vapour and solid ice.

Kaguya Moon South PoleImage copyright JAXA/NHK
Image caption This picture of the Moon’s south polar region was captured by Japan’s Kaguya spacecraft

Temperatures on the Moon can reach a searing 100C in daytime, which doesn’t provide the best conditions for the survival of surface ice.

But because the Moon is tilted on its axis by about 1.54 degrees, there are places at the lunar poles that never see daylight.

Scientists estimate that temperatures in permanently shadowed craters at the Moon’s poles do not rise above -157C (-250F). This would create an environment where deposits of water-ice could remain stable for long periods.

The result supports previous indirect detections of surface ice at the Moon’s south pole. However, those results could potentially be explained by other phenomena – such as unusually reflective lunar soil.

If there’s enough ice sitting at the surface – within the top few millimetres – the water might be accessible as a resource for future human missions to the Moon.

It could potentially be turned into drinking water for the occupants of a lunar base, or “split” into hydrogen and oxygen for rocket fuel. The split oxygen could also be used by astronauts for breathing.

Surface water ice has also been found on other Solar System bodies, such as at the north pole of the planet Mercury and on the dwarf planet Ceres.

Read more at www.bbc.co.uk

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Comments (4)

  • Avatar

    K. Kaiser

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    I beg to differ:
    The claim that at “This [low temperature of ~160 K] would create an environment where deposits of water-ice could remain stable for long periods” misses consideration of the vapor pressure of ice, even at that low temperature. While that may be very small too, there is NIL water vapor pressure in the (non-existing) atmosphere that would prevent continuous sublimation of such ice.

    Therefore, I conclude that the “finding” is based on “wishful thinking.”

    Reply

    • Avatar

      Joseph A Olson

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      @K.Kaiser

      “Water has a number of triple points. Many of the crystalline forms remain metastable in much of the low temperature phase space at lower pressure.”

      “Water Phase Diagram” by London South Bank University > LBSU.AC.uk

      Reply

      • Avatar

        K. Kaiser

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        @ J A Olson

        Yes, water ice has many phases, triple points, etc.

        The critical question though is:
        Is there is any vapor pressure of whatever ice is claimed to exist at the Moon’s poles in the absence of any atmosphere. The phase diagram (at http://www1.lsbu.ac.uk/water/water_phase_diagram.html ) only goes to 0.1 Pa which coincides with a temperature of 200 K.

        The temperature at the poles are said to be 170 K. Extrapolating the Solid/Vapor line down to 0.001 Pa would probably arrive at 170 K.

        With the absence of any atmosphere, I would think that any (gas) pressure at the Moon’s surface is essentially ZERO, say 10^(-6) Pa or even less. In other words, even at that low temperature, there would still be a significant vapor pressure gradient of the ice. That would mean that any surface ice would steadily sublime and be lost to outer space.

        Reply

    • Avatar

      Mervyn Sullivan

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      Excellent comment.

      Reply

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