Evidence of 210Po on Martian dust at Meridiani Planum

Details Evidence of 210Po on Martian dust at Meridiani Planum Evidence of 210Po on Martian dust at Meridiani Planum

Sep 2006

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2006jgre..11109012m&link_type=abstract

Journal of Geophysical Research, Volume 111, Issue E9, CiteID E09012

Physics

Planetary Sciences: Solar System Objects: Mars, Geochemistry: Radiogenic Isotope Geochemistry, Atmospheric Composition And Structure: Aerosols And Particles (0345, 4801, 4906), Atmospheric Processes: Land/Atmosphere Interactions (1218, 1631, 1843), Planetary Sciences: Solid Surface Planets: Instruments And Techniques

Scientific paper

Since the Surveyor and Apollo missions and up to the recent Lunar Prospector mission, 222Rn and 210Po have been key isotopes for understanding gas release events and their spatial and temporal variations on the Moon. Comparatively, these isotopes have drawn much less attention on Mars, if any, despite the wealth of information it could bring on the uppermost meters of the regolith, the exchange of volatiles at the surface, and the atmospheric aerosol cycle. Here we present a statistical analysis of the high-energy end of alpha spectra obtained by the alpha particle X-ray spectrometer onboard Mars Exploration Rover Opportunity and report evidence of 210Po, a decay product of 222Rn, attached to atmospheric dust. The 210Po surface activity on rocks and soils at the landing site is lower than 3.1 × 10-4 Bq cm-2, but analysis of spectra obtained on the dust capture magnet reveals a 210Po activity of (4.6 +/- 2.4) × 10-3 Bq cm-2 (+/-2σ). This difference is due to the very low dust cover index at the landing site. Owing to frequent dust devils, regional and global dust storms that mobilize substantial amounts of dust and homogenize the dust surface layer, we infer that the global average 222Rn exhalation rate is significantly greater on Mars than on the Moon. This comparison supports the hypothesis that on Mars, radon emanation could be comparatively enhanced by the presence of water in the surficial soil. Analysis of atmospheric spectra yields a radon activity upper limit of 16 +/- 5 Bq m-3 during nighttime at the landing site.

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