The Exchange of Mass and Angular Momentum in the Impact Event of Ice Giant Planets: Implications for the origin of Uranus
arXiv:1811.05234 · doi:10.3847/1538-3881/aaf165
Abstract
Uranus has a tilted rotation axis, which is supposed to be caused by a giant impact. In general, an impact event also changes the internal compositional distribution and drives mass ejection from the planet, which may provide the origin of satellites. Previous studies of the impact simulation of Uranus investigated the resultant angular momentum and the ejected mass distribution. However, the effect of changing the initial condition of the thermal and compositional structure is not studied. In this paper, we perform hydrodynamics simulations for the impact events of Uranus-size ice giants composed of a water core surrounded by a hydrogen envelope using two variant methods of the smoothed particle hydrodynamics. We find that the higher entropy target loses its envelope more efficiently than the low entropy target. However, the higher entropy target gains more angular momentum than the lower entropy target since the higher entropy target has more expanded envelope. We discuss the efficiency of angular momentum transport and the amount of the ejected mass and find a simple analytical model to roughly reproduce the outcomes of numerical simulations. We suggest the range of possible initial conditions for the giant impact on proto-Uranus that reproduces the present rotation tilt of Uranus and sufficiently provides the total angular momentum of the satellite system that can be created from the fragments from the giant impact.
arXiv comment16 pages, 14 figures, accepted for publication in ApJ
References in corpus (17)
- Interior Models of Uranus and Neptune
- Reformulation of Smoothed Particle Hydrodynamics with Riemann Solver
- Merging Criteria for Giant Impacts of Protoplanets
- Planet formation with envelope enrichment: new insights on planetary diversity
- Formation of Phobos and Deimos via a Giant Impact
- Implementation and performance of FDPS: A Framework Developing Parallel Particle Simulation Codes
- Self-Consistent Model Atmospheres and the Cooling of the Solar System's Giant Planets
- Collisional Stripping and Disruption of Super-Earths
- Uranus evolution models with simple thermal boundary layers
- Consequences of Giant Impacts on Early Uranus for Rotation, Internal Structure, Debris, and Atmospheric Erosion
- Ring Formation around Giant Planets by Tidal Disruption of a Single Passing Large Kuiper Belt Object
- Kelvin-Helmholtz instabilities with Godunov SPH
- Resolution Dependence of Disruptive Collisions between Planetesimals in the Gravity Regime
- Fortran interface layer of the framework for developing particle simulator FDPS
- Acceleration of Cooling of Ice Giants by Condensation in Early Atmospheres
- On the Impact Origin of Phobos and Deimos II: True Polar Wander and Disk Evolution
- An Extension of Godunov SPH: Application to Negative Pressure Media
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- Proxima Centauri b is not a transiting exoplanet
- Atmospheres on Nonsynchronized Eccentric-tilted Exoplanets I: Dynamical Regimes
- The EOS/Resolution Conspiracy: Convergence in Proto-Planetary Collision Simulations
- Could Uranus and Neptune form by collisions of planetary embryos?
- Did Uranus' regular moons form via a rocky giant impactor?