Redistribution of subsurface neutrons caused by ground ice on Mars
The purpose of this study is to build on that of Squyres and Evans to approach the specific problem of the buried ice deposits explored by Mellon and Jakosky. Therefore, we calculated the depth dependence of equilibrium neutron energy spectra and related neutron-capture gamma ray production rates for a semi-infinite layer of regolith having a Chryse-fines composition containing 5, 10, and 18 wt percent of water. This high water-content layer was buried beneath the same regolith containing 1 percent water at depths of 20, 40, and 80 g/ sq. cm. A 16-g/sq. cm atmosphere having the abundances measured by Owen et al. was included throughout. We also calculated the effects of a 30-g/sq. cm-thick layer containing 18 percent water embedded within a semi-finite regolith containing 1 percent water, at depths of 20, 40, and 80 g/sq. cm below the atmosphere-surface interface.