The mystery of how the moon got its surface water has just got deeper, following the failure of an attempt to replicate the mechanism that was thought to produce it.
Three separate space missions last year reported detecting a sheen of water only molecules thick over large parts of the moon鈥檚 surface. Many planetary scientists assumed the water was created when particles from the solar wind hit lunar soils, but this idea has now been thrown into doubt.
鈥淭he solar wind cannot produce water in sufficient quantities to account for the results of the three missions that observed it,鈥� says , a member of the team at University of Virginia, Charlottesville, that tried to reproduce this effect in the lab.
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For years, theorists have believed that protons from the solar wind could produce water on the moon by prying oxygen atoms away from minerals in the lunar soil and combining with them to form hydroxyl radicals (OH) or water (H2O). This hypothesis gained credibility recently with the observations of hydroxyl and water by NASA Deep Impact and Cassini missions, and the Indian probe Chandrayaan-1.
Bone dry
Baragiola and colleagues tested the idea by blasting protons at crystals of ilmenite and anorthite, two of the most common lunar minerals, in a high vacuum. They found no sign that water or hydroxyl radicals were produced. In fact, they found the opposite: the protons destroyed any traces of water that had remained in the minerals after 24 hours of baking prior to the experiment.
of Brown University in Providence, Rhode Island, who was lead author of last year鈥檚 report from Chandrayaan-1, admits to being puzzled by the results.
But Jeffrey Gillis-Davis, a planetary geologist at the University of Hawaii, thinks the established hypothesis might yet be correct. 鈥淭his does not put the final nail in the coffin鈥� of the solar wind hypothesis, he says. True lunar soil could behave differently from the crystals tested, as it consists of about 60 per cent agglutinated glass.
Gillis-Davis says texture is important in promoting chemical reactions that might produce water in lunar soil. 鈥淪pace weathering鈥� processes like this are more likely to occur in powdery soils than in crystals, he says.
Baragiola is planning to repeat his experiments with real lunar soil.
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