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How water is formed on the Moon | Data from the Moon Mineralogy Mapper (M3), an instrument aboard India's recently ended Chandrayaan-1 spacecraft,
along with the Deep Impact spacecraft, has confirmed the existence of water on the surface of the Moon, with scientists explaining the process of its formation.
"Water ice on the moon has been something of a holy grail for lunar scientists
for a very long time," said Jim Green, director of the Planetary Science Division
at NASA Headquarters in Washington. "This surprising finding has come about through
the ingenuity, perseverance and international cooperation between NASA and the
India Space Research Organization," he added. From its perch in lunar orbit, M3's
state-of-the-art spectrometer measured light reflecting off the moon's surface
at infrared wavelengths, splitting the spectral colors of the lunar surface into
small enough bits to reveal a new level of detail in surface composition. When
the M3 science team analyzed data from the instrument, they found the wavelengths
of light being absorbed were consistent with the absorption patterns for water
molecules and hydroxyl. "For silicate bodies, such features are typically attributed
to water and hydroxyl-bearing materials," said Carle Pieters, M3's principal investigator
from Brown University. "When we say 'water on the moon,' we are not talking about
lakes, oceans or even puddles. Water on the moon means molecules of water and
hydroxyl that interact with molecules of rock and dust specifically in the top
millimeters of the moon's surface," he added. The M3 team found water molecules
and hydroxyl at diverse areas of the sunlit region of the moon's surface, but
the water signature appeared stronger at the moon's higher latitudes. According
to University of Maryland astronomer Jessica Sunshine and co-authors, "The Deep
Impact observations of the Moon not only unequivocally confirm the presence of
OH/H2O on the lunar surface, but also reveal that the entire lunar surface is
hydrated during at least some portions of the lunar day." "Our findings suggest
a solar driven cycle in which layers of water only a few molecules thick form,
dissipate and reform on the surface each lunar day," she said. "We postulate that
hydrogen ions from the Sun are carried by the solar wind to the Moon and there
interact with oxygen rich minerals in lunar soil to produce the water (H20) and
hydroxyl (OH) molecules that spectral analysis unequivocally show us is there.
In a cycle that occurs entirely in daylight, this water is formed in the morning,
substantially lost by lunar mid-day, and re-formed as the lunar surface cools
towards evening," she added. |
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