Fluxes of fast and epithermal neutrons from Lunar Prospector: evidence for water ice at the lunar poles.
@article{Feldman1998FluxesOF, title={Fluxes of fast and epithermal neutrons from Lunar Prospector: evidence for water ice at the lunar poles.}, author={William Charles Feldman and Sylvestre Maurice and Alan B. Binder and Bruce L. Barraclough and Richard Elphic and David J. Lawrence}, journal={Science}, year={1998}, volume={281 5382}, pages={ 1496-500 } }
Maps of epithermal- and fast-neutron fluxes measured by Lunar Prospector were used to search for deposits enriched in hydrogen at both lunar poles. Depressions in epithermal fluxes were observed close to permanently shaded areas at both poles. The peak depression at the North Pole is 4.6 percent below the average epithermal flux intensity at lower latitudes, and that at the South Pole is 3.0 percent below the low-latitude average. No measurable depression in fast neutrons is seen at either pole…
508 Citations
Global Distribution of Neutrons from Mars: Results from Mars Odyssey
- Geology, Environmental ScienceScience
- 2002
Global distributions of thermal, epithermal, and fast neutron fluxes have been mapped during late southern summer/northern winter using the Mars Odyssey Neutron Spectrometer, and portions of the low to middle latitudes indicate subsurface deposits of chemically and/ or physically bound H2O and/or OH.
Improved modeling of Lunar Prospector neutron spectrometer data: Implications for hydrogen deposits at the lunar poles
- Geology, Physics
- 2006
[1] New models have been computed for the Lunar Prospector (LP) thermal and epithermal neutron counting rates using the particle transport code MCNPX. This work improves upon previous studies by…
Evidence for water ice near the lunar poles
- Physics, Geology
- 2001
Improved versions of Lunar Prospector thermal and epithermal neutron data were studied to help discriminate between potential delivery and retention mechanisms for hydrogen on the Moon. Improved…
Evidence for the sequestration of hydrogen-bearing volatiles towards the Moon's southern pole-facing slopes
- Physics, Environmental Science
- 2015
Polar hydrogen deposits on the Moon
- Geology
- 2000
Neutron and gamma-ray data measured using the Lunar Prospector spectrometers were analyzed to define the enhanced hydrogen deposits near both poles of the Moon. Combining the new low-altitude neutron…
Reanalysis of Lunar Prospector neutron spectrometer observations over the lunar poles
- Physics, Geology
- 2002
[1] Components of the neutron energy spectrum measured by instruments on the Lunar Prospector (LP) spacecraft have been optimistically interpreted as indicating massive deposits of water ice or other…
The Local-time variations of Lunar Prospector epithermal-neutron data
- Physics, Geology
- 2015
We assess local-time variations of epithermal-neutron count rates measured by the Lunar Prospector Neutron Spectrometer. We investigate the nature of these variations and find no evidence to support…
Spatial distribution of lunar polar hydrogen deposits after KAGUYA (SELENE)
- Physics
- 2010
Although controversial in its physical form, there is mounting evidence of hydrogen enhancements at the lunar poles. The permanently shadowed locales are potential sites for significant…
Major compositional units of the moon: lunar prospector thermal and fast neutrons
- GeologyScience
- 1998
There appears to be a smooth transition between the most mafic and feldspathic compositions, which correspond to low and high surface altitudes, respectively.
References
SHOWING 1-10 OF 35 REFERENCES
Lunar neutron leakage fluxes as a function of composition and hydrogen content
- Physics
- 1991
Areas of the Moon that might have enhanced concentrations of hydrogen are discussed. The fluxes of thermal, epithermal, and fast neutrons escaping from the lunar surface were calculated for eight…
Major compositional units of the moon: lunar prospector thermal and fast neutrons
- GeologyScience
- 1998
There appears to be a smooth transition between the most mafic and feldspathic compositions, which correspond to low and high surface altitudes, respectively.
Redistribution of subsurface neutrons caused by ground ice on Mars
- Physics, Geology
- 1993
As part of an ongoing effort to understand data that will be returned by the Mars Observer Gamma Ray Spectrometer (MOGRS) experiment, we calculate neutron and gamma ray fluxes for simple models…
Arecibo Radar Mapping of the Lunar Poles: A Search for Ice Deposits
- Physics, Environmental Science
- 1997
The Arecibo 12.6-centimeter wavelength radar system was used to image the polar regions of the moon at a resolution of 125 meters in a search for ice deposits in areas of possible permanent shadow…
Evidence for a basalt-free surface on Mercury and implications for internal heat.
- GeologyScience
- 1995
Microwave and mid-infrared observations reveal that Mercury's surface contains less FeO + TiO2 and at least as much feldspar as the lunar highlands, suggesting a rock and soil composition that is devoid of basalt, the primary differentiate of terrestrial mantles.
Mercury Radar Imaging: Evidence for Polar Ice
- Physics, GeologyScience
- 1992
The first unambiguous full-disk radar mapping of Mercury at 3.5-centimeter wavelength, with the Goldstone 70-meter antenna transmitting and 26 antennas of the Very Large Array receiving, has provided…
The migration of volatiles on the surfaces of Mercury and the Moon
- Geology
- 1997
Radar observations of Mercury have provided the startling discovery of the probable existence of substantial deposits of ices in permanently shaded polar regions [Butler et al., 1993; Harmon et al.,…
Mercury: Full-disk radar images and the detection and stability of ice at the North Pole
- Environmental Science, Geology
- 1993
The first full-disk radar images of Mercury were obtained on August 8 and 23, 1991. These images were constructed using the Very Large Array (VLA) in Socorro, New Mexico, to receive and map radar…
The behavior of volatiles on the lunar surface
- Physics, Geology
- 1961
Volatiles, and water in particular, have been thought to be unstable on the lunar surface because of the rapid removal of constituents of the lunar atmosphere by solar radiation, solar wind, and…