Abstract
The composition and evolutionary history of Mercury's crust are not well determined1,2. The planet as a whole has been predicted3 to have a refractory, anhydrous composition: rich in Ca, Al, Mg and Fe, but poor in Na, K, OH, and S. Its atmosphere is believed to be derived in large part from the surface materials. A combination of effects that include impact vaporization (from infalling material), volatile evaporation, photon-stimulated desorption and sputtering releases material from the surface to form the atmosphere. Sodium and potassium have already been observed in Mercury's atmosphere4,5,6, with abundances that require a volatile-rich crust7. The sodium probably results from photon-stimulated desorption8,9, and has a temperature of 1,500 K (ref. 10). Here we report the discovery of calcium in the atmosphere near Mercury's poles. The column density is very low and the temperature is apparently very high (12,000 K). The localized distribution and high temperature, if confirmed, suggest that the atmospheric calcium may arise from surface sputtering by ions, which enter Mercury's auroral zone. The low abundance of atmospheric Ca may indicate that the regolith is rarefied in calcium.
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Acknowledgements
The data presented here were obtained at the W.M. Keck Observatory, which is operated as a scientific partnership between the California Institute of Technology, the University of California and the National Aeronautics and Space Administration. The observatory was made possible by the generous financial support of the W.M. Keck Foundation. We are grateful to the WMKO Observing Assistants for their help while conducting the observations. R.M.K. acknowledges the support of a NASA grant.
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Bida, T., Killen, R. & Morgan, T. Discovery of calcium in Mercury's atmosphere. Nature 404, 159–161 (2000). https://doi.org/10.1038/35004521
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DOI: https://doi.org/10.1038/35004521
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