20 NOVEMBER 2007 CLASS #23 Astronomy 340 Fall 2007.

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20 NOVEMBER 2007 CLASS #23 Astronomy 340 Fall 2007

Outgassing Model (Tobie, Lunine, Sotin 2006)

Measuring Composition Poulet et al 2003 Astronomy & Astrophysics

Particle Size Distribution Power law  n(r) = n 0 r -3  number of 10 m particles is times less than # of 1 cm particles Total mass distribution is uniform across all bins Collisions  Net loss of energy  flatten ring  Fracture particles  power law distribution of particle size  But, ring should actually be thinner and radially distribution should gradually taper off, not have sharp edges

Ring Composition Water ice plus impurities Color variation = variation in abundance of impurities What could they be?

Ring Composition Red slope arises from complex carbon compounds Variation in grain size included in model  90% water ice overall

Spectra of Saturn’s D ring 3 micron feature is water ice.

Comparative Spectroscopy olivine Ring particle

Ring Dynamics Inner particles overtake outer particles  gravitational interaction

Ring Dynamics Inner particles overtake outer particles  gravitational interaction  Inner particle loses energy, moves closer to planet  Outer particle gains energy, moves farther from planet  Net effect is spreading of the ring  Spreading timescale = diffusion timescale

Ring Dynamics Spreading stops when there are no more collisions Ignores radiation/magnetic effects that are linearly proportional to the size Exact distribution affected by  Differential rotation  Presence of moons and resonances with those moons

Saturn’s Rings D ring: C ring:  Titan ringlet  Maxwell Gap: B ring: Cassini division A ring: F ring: (center) G ring: E ring:

Structure in the Rings Let’s look at some pictures and see what there is to see….  Gaps  Ripples  Abrupt edges to the rings  Presence of small moons

Moons and Rings Perturb orbits of ring particles  Confine Uranus’ rings, create arcs around Neptune Shepherding – two moons on either side of ring  Outer one has lower velocity  slows ring particle, particle loses energy  Inner one has higher velocity  accelerates ring particle, particle gains energy  Saturn’s F ring is confined between Prometheus and Pandora

Shepherds in Uranus’ ring system

Moons and Rings Perturb orbits of ring particles  Confine Uranus’ rings, create arcs around Neptune Shepherding – two moons on either side of ring  Outer one has lower velocity  slows ring particle, particle loses energy  Inner one has higher velocity  accelerates ring particle, particle gains energy  Saturn’s F ring is confined between Prometheus and Pandora Resonances  Similar to Kirkwood Gap in asteroid belt  2:1 resonance with Mimas

Resonances ALMOST ALL STRUCTURE IN RINGS IS PROBABLY DUE TO DYNAMICAL INTERACTIONS WITH MOONS Orbits of the ring particles have:  Orbital frequency  Radial frequency  Vertical frequency Pattern speed of the perturbing potential vs. orbital frequency of the particles  when they match we get co- rotation Pattern speed vs radial frequency  Lindblad resonances

“Perturbing Potential”? Gravitational potential  Orbit about main planet  ring particles are in orbit  Potential due to moon that varies with same period as that of the moon  rotating reference frame Net effect  spiral density wave  Exists between inner and outer Lindblad resonances  Fluctuations in potential  fluctuations in the surface density  azimuthal variation, tightly wound, shows up looking like an old-fashioned LP

Vertical resonances – vertical structure

Moonlets?

Pan – density waves

Enceladus

Enceladus occultation

Enceladus