The rotation rate of Uranus, its internal structure, and the process of planetary accretion

Astronomy and Astrophysics – Astronomy

Scientific paper

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Angular Velocity, Astronomical Models, Planetary Evolution, Planetary Geology, Planetary Structure, Uranus (Planet), Atmospheric Composition, Ice, Planetary Atmospheres, Planetary Rotation, Voyager 2 Spacecraft, Uranus, Rotation, Structure, Interior, Accretion, Computer Methods, Models, Atmosphere, Enrichment, Water, Ammonia, Methane, Abundance, Ice, Rock, Composition, Formation, Period

Scientific paper

It is investigated whether Uranus models with higher values of the total planetary ice to rock ratio (I/R) can be made consistent with the rotation period of 17.24 hr. measured by Voyager 2, and with the 16-pole moment of the gravitational field (J4) derived from the observations of French et al. (1986). An atmospheric enhancement of H2O, NH3, and CH4 of not more than about 30 times the solar value, and an I/R value of greater than 16, are implied by these models. A planetary accretion scenario whereby such I/R values are possible for a large range of planetesimal radii and initial velocities is discussed.

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