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Originally published in Science Express on 24 September 2009
Science 23 October 2009:
Vol. 326. no. 5952, pp. 562 - 564
DOI: 10.1126/science.1178105

Reports

Detection of Adsorbed Water and Hydroxyl on the Moon

Roger N. Clark

Data from the Visual and Infrared Mapping Spectrometer (VIMS) on Cassini during its flyby of the Moon in 1999 show a broad absorption at 3 micrometers due to adsorbed water and near 2.8 micrometers attributed to hydroxyl in the sunlit surface on the Moon. The amounts of water indicated in the spectra depend on the type of mixing and the grain sizes in the rocks and soils but could be 10 to 1000 parts per million and locally higher. Water in the polar regions may be water that has migrated to the colder environments there. Trace hydroxyl is observed in the anorthositic highlands at lower latitudes.

U.S. Geological Survey, Mail Stop 964, Box 25046 Federal Center, Denver, CO 80227, USA. E-mail: rclark{at}usgs.gov

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THIS ARTICLE HAS BEEN CITED BY OTHER ARTICLES:
Temporal and Spatial Variability of Lunar Hydration As Observed by the Deep Impact Spacecraft.
J. M. Sunshine, T. L. Farnham, L. M. Feaga, O. Groussin, F. Merlin, R. E. Milliken, and M. F. A'Hearn (2009)
Science 326, 565-568
   Abstract »    Full Text »    PDF »
A Lunar Waterworld.
P. G. Lucey (2009)
Science 326, 531-532
   Abstract »    Full Text »    PDF »
Character and Spatial Distribution of OH/H2O on the Surface of the Moon Seen by M3 on Chandrayaan-1.
C. M. Pieters, J. N. Goswami, R. N. Clark, M. Annadurai, J. Boardman, B. Buratti, J.-P. Combe, M. D. Dyar, R. Green, J. W. Head, et al. (2009)
Science 326, 568-572
   Abstract »    Full Text »    PDF »



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