Saturn Rings Closeup (2D)

Top-down ring plane with resonances and a local shearing box of colliding particles.

Switch to 3D

Presets

Playback

Moons and view

Choose which moons act, the mass multiplier and the zoom window.

Shearing box

Local patch of ring: optical depth and restitution.

Layers

Model checks

The science

What the 2D view shows

A top-down view of the ring plane (same particle swarm and integrator as the 3D page) and a local shearing box, a small patch of ring that follows Hill's equations. The box shows what the 3D view cannot: individual ring particles colliding while Keplerian shear drags neighbours past each other.

Equations

  • Kepler: Ω = √(GM/r3), shear |r dΩ/dr| = (3/2) Ω.
  • Hill's equations (rotating frame): x'' = 2Ω y' + 3Ω2 x, y'' = -2Ω x'; the exact epicycle solution is used between collisions, so σy/σx = κ/2Ω = 1/2 for free particles.
  • Collisions: hard spheres, vn' = -ε vn; optical depth τ = N π a2/(Lx Ly).
  • Resonance: a = am ((m-1)/m)2/3; Roche limit 2.456 R (ρp/ρ)1/3.

Honest simplifications

Test particles around Saturn with moons on circular orbits (no collisions or self-gravity in the ring-plane view); moon masses can be multiplied so effects show in seconds; the box is planar (no vertical motion), has no self-gravity and a fixed restitution coefficient, particle radius 1 m. The optical-depth profile is illustrative. Dissipative collisions in a real ring also damp eccentricities, which is why resonances clear gaps.

What to try
  • Load Mimas 2:1 resonance: particles near 116,900 km turn orange (eccentric).
  • Switch to the shearing box and lower the restitution to 0.2: the velocity dispersion collapses.
  • Raise tau to 1.0: the collision rate per orbit rises sharply.
  • Put the view centre at the Mimas 2:1 radius and read the orbital period (half of Mimas' period): graph 3.
Optical depth tau(r)
Rms e*a versus semi-major axis
Orbital period versus radius
Shearing-box velocity dispersion