Astronomy and Astrophysics – Astronomy
Scientific paper
Dec 1987
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1987jgr....9214877a&link_type=abstract
Journal of Geophysical Research (ISSN 0148-0227), vol. 92, Dec. 30, 1987, p. 14877-14883.
Astronomy and Astrophysics
Astronomy
21
Flyby Missions, Planetary Mass, Radio Astronomy, Uranus (Planet), Uranus Satellites, Voyager 2 Spacecraft, Deep Space Network, Density Distribution, Planetary Composition, Planetary Evolution, Spaceborne Photography
Scientific paper
The authors have analyzed radio Doppler data and star-satellite imaging data from Voyager 2 at Uranus, along with 8 years of ground-based astrometric data, and have obtained improved masses and densities for the satellites of Uranus as well as a new ratio of the mass of the Sun to the mass of the Uranian system of 22902.94±0.04. The mean density of Uranus is 1.285±0.001 g cm-3. The satellite densities are 1.25±0.33 for Miranda, 1.55±0.22 for Ariel, 1.58±0.23 for Umbriel, 1.685±0.068 for Titania, and 1.635±0.060 for Oberon. The mean uncompressed density of all five satellites is 1.48±0.06 g cm-3. This is 0.10 g cm-3 higher than the value expected for a homogeneous solar mix. In order to reconcile this difference, the authors suggest that the Uranian moons contain roughly 15% by mass of pure graphite, in addition to a normal solar component of rocks and ices. If so, at least 50% of the carbon within the nebular gases from which Uranus and its satellites condensed was in the form of graphite, the remaining being in CH4. The high thermal conductivity of graphite ensures that the Uranian moons have remained cold and undifferentiated since the time of their formation, despite heating caused by the decay of radioactive nuclides. Apparently, an alternative cometary origin for the satellites is ruled out.
Anderson John D.
Campbell James K.
Jacobson Abram R.
Sweetnam Donald N.
Taylor Harry A.
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