Though NASA’s Lunar Prospector appeared to have struck ice in 1999, its findings proved inconclusive. Had they been supported, scientists predicted that any water would have come from gases emitted by meteorites striking the moon.
With so little reason to believe in native lunar water, said Saal, it took three years to secure the minimal funding necessary to take another look at the Apollo pebbles, gathered between 1969 and 1972.
But a high-powered imaging technique known as secondary ion mass spectrometry revealed a wealth of so-called volatile compounds, among them fluorine, chlorine, sulfur, carbon dioxide — and water.
SHOOT: Unless the moon rock that was 'brought back' by the Apollo missions was actually from some volcanic site on Earth.
Though the moon has many seas, scientists thought it was dry.
They were wrong.
In a study published today in Nature, researchers led by Brown University geologist Alberto Saal found evidence of water molecules in pebbles retrieved by NASA’s Apollo missions.
The findings point to the existence of water deep beneath the moon’s surface, transforming scientific understanding of our nearest neighbor’s formation and, perhaps, our own. There may also be a more immediately practical application.
"Is there water there? That’s important for lunar missions. People could get the water. They could use the hydrogen for energy," said Saal.
The pebbles were scattered by lunar volcanoes that erupted three billion years ago, when the moon was still a cooling hunk of magma cast into orbit by the collision of a Mars-sized asteroid with Earth.
That impact enveloped the Earth in temperatures reaching 7000 Kelvin — more than enough, it was thought, to obliterate all traces of hydrogen and oxygen.
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