The leading theory for the formation of Earth's Moon invokes a collision between a Mars-sized body and the proto-Earth to produce a disk of orbiting material that later condenses to form the Moon. We show that the disk opacity is large, and cooling is therefore inefficient (tcoolΩ ≫ 1). In this regime, angular momentum transport in the disk leads to steady heating unless α < (tcoolΩ)-1 ≪ 1. Following earlier work by Charnoz and Michaut, and Carballido et al., we show that once the disk is completely vaporized it is well coupled to the magnetic field. We consider a scenario in which turbulence driven by magnetic fields leads to a brief, hot phase where the disk is geometrically thick, with strong turbulent mixing. The disk cools by spreading until it decouples from the field. We point out that approximately half the accretion energy is dissipated in the boundary layer where the disk meets the Earth's surface. This creates high entropy material close to the Earth, driving convection and mixing. Finally, a hot magnetized disk could drive bipolar outflows that remove mass and angular momentum from the EarthMoon system.
- planets and satellites: formation
- planets and satellites: magnetic fields
ASJC Scopus subject areas
- Astronomy and Astrophysics
- Space and Planetary Science