Abstract
We investigated the effects of a tidal interaction with a gas disk and the dynamical friction with a planetesimal disk on the orbital instability of a protoplanet system. Both effects are expressed as the drag force, which is proportional to the random velocity of a protoplanet. We calculated numerically the orbits of 5 protoplanets with the same separation distance under the drag-force effect and examined the orbital instability time under the drag force, Tinstdf. We found that Tinstdf can become much larger than the instability time under the drag-free condition, and that the onset of the orbital instability is prevented when the separation distance exceeds a critical value. We obtained a relation between the critical separation distance and the surface density of the gas or planetesimal disk. By applying this relation, we found that, for the formation of terrestrial planets from a protoplanet system with a typical orbital separation (i.e., ∼ 10 Hill radii), the surface density of the nebular gas must be reduced to about one-thousandth of that in the minimum-mass nebula model. Terrestrial planets would be formed after such a depletion of the solar nebula.
Original language | English |
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Pages (from-to) | 471-479 |
Number of pages | 9 |
Journal | Publications of the Astronomical Society of Japan |
Volume | 54 |
Issue number | 3 |
DOIs | |
Publication status | Published - 2002 |
Externally published | Yes |
Keywords
- Earth
- Instabilities
- Solar system: formation
- Stokes-type drag force
ASJC Scopus subject areas
- Astronomy and Astrophysics
- Space and Planetary Science