Terrestrial Planet Formation: Dynamical Shake-up and the Low Mass of Mars

被引:24
作者
Bromley, Benjamin C. [1 ]
Kenyon, Scott J. [2 ]
机构
[1] Univ Utah, Dept Phys & Astron, 115 S 1400 E,Rm 201, Salt Lake City, UT 84112 USA
[2] Smithsonian Astrophys Observ, 60 Garden St, Cambridge, MA 02138 USA
关键词
planetary systems; planet-disk interactions; planets and satellites: dynamical evolution and stability; planets and satellites: formation; GAS-GIANT PLANETS; PROTOPLANETARY DISK STRUCTURES; PICTORIS CIRCUMSTELLAR DISK; PRIMORDIAL SOLAR NEBULA; BODY-COAGULATION CODE; KUIPER-BELT OBJECTS; BINARY STAR SYSTEMS; SECULAR RESONANCE; ASTEROID BELT; BETA-PICTORIS;
D O I
10.3847/1538-3881/aa6aaa
中图分类号
P1 [天文学];
学科分类号
0704 ;
摘要
We consider a dynamical shake-up model to explain the low mass of Mars and the lack of planets in the asteroid belt. In our scenario, a secular resonance with Jupiter sweeps through the inner solar system as the solar nebula depletes, pitting resonant excitation against collisional damping in the Sun's protoplanetary disk. We report the outcome of extensive numerical calculations of planet formation from planetesimals in the terrestrial zone, with and without dynamical shake-up. If the Sun's gas disk within the terrestrial zone depletes in roughly a million years, then the sweeping resonance inhibits planet formation in the asteroid belt and substantially limits the size of Mars. This phenomenon likely occurs around other stars with long-period massive planets, suggesting that asteroid belt analogs are common.
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页数:17
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