Spatial Structure and Coherent Motion in Dense Planetary Rings Induced by Self-Gravitational Instability
arXiv:astro-ph/9908057 · doi:10.1186/BF03351594
Abstract
We investigate the formation of spatial structure in dense, self-gravitating particle systems such as Saturn's B-ring through local -body simulations to clarify the intrinsic physics based on individual particle motion. In such a system, Salo (1995) showed that the formation of spatial structure such as wake-like structure and particle grouping (clump) arises spontaneously due to gravitational instability and the radial velocity dispersion increases as the formation of the wake structure. However, intrinsic physics of the phenomena has not been clarified. We performed local -body simulations including mutual gravitational forces between ring particles as well as direct (inelastic) collisions with identical (up to ) particles. In the wake structure particles no longer move randomly but coherently. We found that particle motion was similar to Keplerian motion even in the wake structure and that the coherent motion was produced since the particles in a clump had similar eccentricity and longitude of perihelion. This coherent motion causes the increase and oscillation in the radial velocity dispersion. The mean velocity dispersion is rather larger in a more dissipative case with a smaller restitution coefficient and/or a larger surface density since the coherence is stronger in the more dissipative case. Our simulations showed that the wavelength of the wake structure was approximately given by the longest wavelength $\hsλ{cr} = 4π^2 GΣ/κ^2$ in the linear theory of axisymmetric gravitational instability in a thin disk, where , , and are the gravitational constant, surface density, and a epicyclic frequency.
Accepted by Earth, Planets, and Space. 39 pages, 20 figures. PostScript files also available from http://www.geo.titech.ac.jp/nakazawalab/hdaisaka/works/
Cited by in corpus (20)
- Cassini Imaging of Saturn's Rings II: A Wavelet Technique for Analysis of Density Waves and Other Radial Structure in the Rings
- Lunar accretion from a Roche-interior fluid disk
- Long-term & large-scale viscous evolution of dense planetary rings
- Angular Momentum Transfer in Protolunar Disk
- Accretion of Saturn's Inner Mid-sized Moons from a Massive Primordial Ice Ring
- -body Simulation of Planetesimal Formation Through Gravitational Instability of a Dust Layer
- The Validity of the Super-Particle Approximation during Planetesimal Formation
- What confines the rings of Saturn?
- Simulating the Smallest Ring World of Chariklo
- Constraints on the initial mass, age and lifetime of Saturn's rings from viscous evolutions that include pollution and transport due to micrometeoroid bombardment
- N-Body Simulation of Planetesimal Formation through Gravitational Instability of a Dust Layer in Laminar Gas Disk
- N-Body Simulation of Planetesimal Formation through Gravitational Instability and Coagulation. II. Accretion Model
- Formation of a Propeller Structure by a Moonlet in a Dense Planetary Ring
- Experimental study of clusters in dense granular gas and implications for the particle stopping time in protoplanetary disks
- Particle Number Dependence of The -Body Simulations of Moon Formation
- Dynamics of Self-Gravity Wakes in Dense Planetary Rings I. Pitch Angle
- Multi-Particle Collisions in Microgravity: Coefficient of Restitution and Sticking Threshold for Systems of Mm-Sized Particles
- A Weakly Nonlinear Model for the Damping of Resonantly Forced Density Waves in Dense Planetary Rings
- Planetary Ring Dynamics -- The Streamline Formalism -- 2. Theory of Narrow Rings and Sharp Edges
- The dynamics of self-gravity wakes in the Mimas 5:3 bending wave: modifying the linear theory