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, soσy/σx = κ/2Ω = 1/2for free particles. - Collisions: hard spheres,
vn' = -ε vn; optical depthτ = N π a2/(Lx Ly). - Resonance:
a = am ((m-1)/m)2/3; Roche limit2.456 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.