Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
1775592 | Icarus | 2007 | 4 Pages |
Abstract
Gravity results are available from radio Doppler data acquired by the Deep Space Network during the encounter of the Cassini spacecraft with Enceladus in February 2005. We report the mass of Enceladus to be (1.0798±0.0016)×1020 kg(1.0798±0.0016)×1020 kg, which implies a density of 1608.9±4 kgm−3. For a core made of hydrated silicates with a density of 2500 kg m−3 the core radius is ∼190 km∼190 km and the quadrupole moment C22∼1.4×10−3C22∼1.4×10−3. If Enceladus is in hydrostatic equilibrium, the larger than previously anticipated density implies that the recently proposed secondary spin–orbit resonance cannot be present. Therefore, the source of endogenic activity of Enceladus remains unexplained.
Keywords
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Space and Planetary Science
Authors
Nicole J. Rappaport, Luciano Iess, Paolo Tortora, Aseel Anabtawi, Sami W. Asmar, Lucia Somenzi, Francesco Zingoni,