Abstract
THE study of γ-ray emission from planets with a thin atmosphere allows a rough estimation of the chemical composition of their surface to be made. The first attempt to make orbital measurements of the -γ-ray flux from Mars was made by the Soviet spacecraft Mars 5 (ref. 1). Here we present results from the -γ-ray APEX experiment on board Phobos 2. We have measured the y-ray albedo of the martian surface. This albedo appears as a large continuum between a few hundred keV and 8 MeV corresponding to a source intensity of 5 photons cm-2 s-1 2Φ-l (estimated in the 150–1500 keV energy range). There is also evidence for a 511-keV annihilation emission and for a broad contribution of probable nuclear lines between 4 and 7 MeV.
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d'Uston, C., Atteia, JL., Barat, C. et al. Observation of the γ-ray emission from the martian surface by the APEX experiment. Nature 341, 598–600 (1989). https://doi.org/10.1038/341598a0
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DOI: https://doi.org/10.1038/341598a0
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