Low thermal inertia (9-20 J m^{-2} K^{-1} s^{-0.5}) on icy moons requires >80% porosity, <1 mm grains, and unconsolidated ice regolith, with deeper compaction indicated by higher inertia values.
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The Physical Nature of Regolith on Icy Moons
Low thermal inertia (9-20 J m^{-2} K^{-1} s^{-0.5}) on icy moons requires >80% porosity, <1 mm grains, and unconsolidated ice regolith, with deeper compaction indicated by higher inertia values.