Dynamical evolution of planetesimals in protoplanetary disks
arXiv:astro-ph/0306244 · doi:10.1086/378609
Abstract
The current picture of terrestrial planet formation relies heavily on our understanding of the dynamical evolution of planetesimals -- asteroid-like bodies thought to be planetary building blocks. In this study we investigate the growth of eccentricities and inclinations of planetesimals in spatially homogeneous protoplanetary disks using methods of kinetic theory. We explore disks with a realistic mass spectrum of planetesimals evolving in time, similar to that obtained in self-consistent simulations of planetesimal coagulation. We calculate the behavior of planetesimal random velocities as a function of the planetesimal mass spectrum both analytically and numerically; results obtained by the two approaches agree quite well. Scaling of random velocity with mass can always be represented as a combination of power laws corresponding to different velocity regimes (shear- or dispersion-dominated) of planetesimal gravitational interactions. For different mass spectra we calculate analytically the exponents and time dependent normalizations of these power laws, as well as the positions of the transition regions between different regimes. It is shown that random energy equipartition between different planetesimals can only be achieved in disks with very steep mass distributions (differential surface number density of planetesimals falling off steeper than m^{-4}), or in the runaway tails. In systems with shallow mass spectra (shallower than m^{-3}) random velocities of small planetesimals turn out to be independent of their masses. We also discuss the damping effects of inelastic collisions between planetesimals and of gas drag, and their importance in modifying planetesimal random velocities.
arXiv comment20 pages, 17 figures, 1 table, submitted to AJ
References in corpus (6)
- Accretion in the Early Kuiper Belt I. Coagulation and Velocity Evolution
- Planet Formation in the Outer Solar System
- The growth of planetary embryos: orderly, runaway, or oligarchic?
- Termination of planetary accretion due to gap formation
- Planetesimal disk evolution driven by embryo-planetesimal gravitational scattering
- Planetesimal disk evolution driven by planetesimal-planetesimal gravitational scattering
Cited by in corpus (24)
- Planet Formation by Coagulation: A Focus on Uranus and Neptune
- Fast accretion of small planetesimals by protoplanetary cores
- Terrestrial Planet Formation I. The Transition from Oligarchic Growth to Chaotic Growth
- Rocking the Lighthouse: Circumpulsar Asteroids and Radio Intermittency
- Tidal Truncation of Circumplanetary Discs
- Detecting the Dusty Debris of Terrestrial Planet Formation
- The Mass Budget of Planet Forming Discs: Isolating the Epoch of Planetesimal Formation
- Brownian Motion in Planetary Migration
- Where Did The Moon Come From?
- Formation and accretion history of terrestrial planets from runaway growth through to late time: implications for orbital eccentricity
- Circumplanetary disks around young giant planets: a comparison between core-accretion and disk instability
- Production of trans-Neptunian binaries through chaos-assisted capture
- Dynamical evolution of thin dispersion-dominated planetesimal disks
- 2007 TY430: A Cold Classical Kuiper Belt Type Binary in the Plutino Population
- Planet formation in stellar binaries: Global simulations of planetesimal growth
- Forming the Cold Classical Kuiper Belt in a light Disk
- Formation and Collisional Evolution of Kuiper Belt Objects
- Onset of oligarchic growth and implication for accretion histories of dwarf planets
- A particle-based hybrid code for planet formation
- N-body simulations of terrestrial planet growth with resonant dynamical friction
- After Runaway: The Trans-Hill Stage of Planetesimal Growth
- Conglomeration of kilometre-sized planetesimals
- Hybrid methods in planetesimal dynamics: Formation of protoplanetary systems and the mill condition
- Runaway Growth of Planetesimals Revisited: Presenting Criteria Required for Realistic Modeling of Planetesimal Growth