Predictions of MESSENGER Neutron Spectrometer measurements for Mercury's north polar region |
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| Authors: | David J Lawrence John K Harmon William C Feldman John O Goldsten David A Paige Patrick N Peplowski Edgar A Rhodes Christina M Selby Sean C Solomon |
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| Institution: | aJohns Hopkins University Applied Physics Laboratory, Laurel, MD 20723, USA;bNational Astronomy and Ionosphere Center, Arecibo Observatory, Arecibo, PR 00612, USA;cPlanetary Science Institute, Tucson, AZ 85719, USA;dDepartment of Earth and Space Sciences, University of California, Los Angeles, CA 90095, USA;eDepartment of Terrestrial Magnetism, Carnegie Institution of Washington, Washington, DC 20015, USA |
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| Abstract: | From radar images of Mercury's poles and MESSENGER Neutron Spectrometer (NS) measurements obtained during the spacecraft's flybys of Mercury, predictions of neutron count rates and their uncertainties are calculated for Mercury's north polar region as of the end of the MESSENGER primary orbital mission. If Mercury's poles contain large amounts of water ice, as has been suggested on the basis of the radar data, then during the one-year-long orbital mission the NS should detect signals indicative of excess polar hydrogen with a significance of at least 4σ, where σ is the standard deviation derived from Poisson counting statistics. If the polar deposits are not enriched with hydrogen, but are dominated by other elements, such as sulfur, then the MESSENGER neutron measurements should be able to confirm the absence of deposits having surface concentrations in excess of 50 wt% H2O on permanently shadowed floors of craters near Mercury's north pole. Because of the large spatial footprint of the NS data, individual polar deposits will not be spatially resolved, but longitudinal asymmetries may be detected if residual systematic uncertainties are sufficiently low. |
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| Keywords: | Mercury Polar deposits Neutron spectroscopy MESSENGER |
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