Astronomy 340 Fall 2005 17 November 2005 Class #22.

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Presentation transcript:

Astronomy 340 Fall 2005 17 November 2005 Class #22

Review & Announcements HW #3, #4 due today Projects due Dec 22  send me your topics! Titan Thick atmosphere – N2 + hydrocarbons Methane ocean? Methane sludge? Variation in surface characteristics Tidal Forces Zero-order approximate  eccentric orbits yield tidal heating  goes as R-6

Cassini Trajectory

Titan’s Atmosphere

Surface Liquid on Titan? Hydrocarbon lake? Old river beds?

Structure of Titan Surface landing site was firm  possible liquid below Evidence of some liquid on surface Surface pressure is sufficient (1.5 bar)

Planetary Rings A Little History 1610  Galileo discovered rings; they disappeared in 1612 1659  Christian Huygens discovered disk-like nature 1977  Uranus’ rings discovered during occultation 1979  Voyager 1 discovered Jupiter’s rings 1980s  Neptune’s arc-like rings discovered via occulation

Cassini-Huygens Science - Rings Study configuration of the rings and dynamic processes responsible for ring structure Map the composition and size distribution of ring material Investigate the interrelation of Saturn’s rings and moons, including imbedded moons Determine the distribution of dust and meteoroid distribution in the vicinity of the rings Study the interactions between the rings and Saturn’s magnetosphere, ionosphere, and atmosphere

Basic Properties Solid disk vs particles Too big to rotate as solid body Maxwell  rings are particles 100m thick vs 105 km wide (Saturn) Just one ring? No All reside within Roche limit of planet

Ring Comparison Jupiter Uranus Main ring – bigger particles, more scattering Halo – interior component, orbits scattered by interaction with Jupiter’s magnetic field Gossamer – very low density, farther out  more inclined orbit so its fatter Uranus 6 identified rings Thickness ~10 km, width ~250000 km Very close to being in circular orbit

Rings: Uranus & Neptune Uranus’ rings Neptune rings

Particle Size Distribution Power law  n(r) = n0r-3  number of 10 m particles is 10-9 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

Measuring Composition Poulet et al 2003 Astronomy & Astrophysics 412 305

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

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: 66900-74510 C ring: 74568-92000 Titan ringlet 77871 Maxwell Gap: 87491 B ring: 92000-117580 Cassini division A ring: 122170-136775 F ring: 140180 (center) G ring: 170000-175000 E ring: 181000-483000

Structure in the Rings Let’s look at some pictures and see what there is to see….

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