Physics
Scientific paper
May 1992
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1992jgr....97.7681b&link_type=abstract
Journal of Geophysical Research (ISSN 0148-0227), vol. 97, no. E5, May 25, 1992, p. 7681-7698. Research supported by Max-Planck-
Physics
31
Gamma Ray Spectrometers, Mars Observer, Neutron Counters, Scintillation Counters, Germanium Diodes, Radiant Cooling, Spacecraft Instruments
Scientific paper
The Mars Observer gamma ray spectrometer will return data related to the elemental composition of Mars. The instrument has both a gamma ray spectrometer and several neutron detectors. The gamma ray spectrometer will return a spectrum nominally every 20 s from Mars permitting a map of the elemental abundances to be made. The gamma rays are emitted from nuclei involved in radioactive decay, from nuclei formed by capture of a thermal neutron, and from nuclei put in an excited state by a fast-neutron interaction. The gamma rays come from an average depth of the order of a few tens of centimeters. The spectrum will show sharp emission lines whose intensity determines the concentration of the element and whose energy identifies the element. The neutron detectors, using the fact that the orbital velocity of the Mars Observer spacecraft is similar to the velocity of thermal neutrons, determine both the thermal and epithermal neutron flux. By combining the results from both techniques it is possible to map the depth dependence of hydrogen in the upper meter as well. These data permit a variety of Martian geoscience problems to be addressed including the crust and mantle composition, weathering processes, volcanism, and the volatile reservoirs and processes.
Arnold James R.
Bailey Sterling H.
Boynton Willam V.
Englert Peter A. J.
Feldman William C.
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