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Journal ArticleDOI

Detection of Water in the LCROSS Ejecta Plume

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TLDR
The Lunar Crater Observation and Sensing Satellite (LCROSS) mission was designed to provide direct evidence that water ice may be presented in permanently shadowed craters of the Moon, and spectral bands of a number of other volatile compounds were observed.
Abstract
Several remote observations have indicated that water ice may be presented in permanently shadowed craters of the Moon. The Lunar Crater Observation and Sensing Satellite (LCROSS) mission was designed to provide direct evidence. On 9 October 2009, a spent Centaur rocket struck the persistently shadowed region within the lunar south pole crater Cabeus, ejecting debris, dust, and vapor. This material was observed by a second "shepherding" spacecraft, which carried nine instruments, including cameras, spectrometers, and a radiometer. Near-infrared absorbance attributed to water vapor and ice and ultraviolet emissions attributable to hydroxyl radicals support the presence of water in the debris. The maximum total water vapor and water ice within the instrument field of view was 155 ± 12 kilograms. Given the estimated total excavated mass of regolith that reached sunlight, and hence was observable, the concentration of water ice in the regolith at the LCROSS impact site is estimated to be 5.6 ± 2.9% by mass. In addition to water, spectral bands of a number of other volatile compounds were observed, including light hydrocarbons, sulfur-bearing species, and carbon dioxide.

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References
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Journal ArticleDOI

High spectral resolution reflectance spectroscopy of minerals

TL;DR: In this article, the reflectance spectra of minerals are studied as a function of spectral resolution in the range from 0.2 to 3.0 microns, and selected absorption bands were studied at resolving powers as high as 2240.
Journal ArticleDOI

Fluxes of fast and epithermal neutrons from Lunar Prospector: evidence for water ice at the lunar poles.

TL;DR: Maps of epithermal- and fast-neutron fluxes measured by Lunar Prospector were used to search for deposits enriched in hydrogen at both lunar poles, and data are consistent with deposits of hydrogen in the form of water ice that are covered by as much as 40 centimeters of desiccated regolith within permanently shaded craters near both poles.
Journal ArticleDOI

Ice in the lunar polar regions

TL;DR: In this paper, the stability of the traps and the trapping mechanism are verified, and four potential sources of trapped H2O are identified: solar wind reduction of Fe in the regolith, meteoroids, cometary impact, and degassing of the interior.
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