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Astronomy 161
Introduction to Solar System Astronomy
Prof. Paul Martini
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Lecture 37: Moons of Saturn
Key Ideas:
- Most diverse moon system of any planet
- Trojan and co-orbital moons
- Large moons
- Cratered Hyperion
- Two-toned Iapetus
- Cryo-geysers on Enceladus
- Saturn's Giant Moon Titan
- Only moon with a thick atmosphere
- Prospects for Life
Trojan Moons
- Tethys has two trojan moons: Telesto and Calypso
- Located at the L4 and L5 lagrange points
Co-orbital Moons
- Epimetheus and Janus are the only examples known
- Orbital separation is less than their diameters
- Exchange happens every four years
- Works because their masses are similar
Large Moons
- Tethys, Dione, and Rhea
- Densities of ~1 g/cc
- Spherical due to gravity
- Flattened craters
- Mimas
- Responsible for the Cassini Division
- Herschel Crater is 140km across
- Egg-shaped by tidal forces
Hyperion
- Covered in deep, sharp-edged craters
- Main constituent is dirty water ice
- Porosity is about 40%
- Craters may form by melting around darker material or compression upon impact
Iapetus
- Leading hemisphere has a 3-5% albedo
- Trailing hemisphere has a 50-60% albedo
- Has a 1300 km equatorial ridge that rises 20 km above the surface
- Likely the leading surface is polluted by Phoebe, which may be an object captured from the Kuiper Belt
Titan: Saturn's Giant Moon
- Discovered in 1655 by Christian Huygens
- Second largest moon in the Solar System
- 50% larger than our Moon
- Larger than Mercury (but less massive)
- Composition similar to Pluto
- Only moon with a thick atmosphere
Huygens Lander
- Part of the Cassini mission to Saturn
- The Huygens probed separated from Cassini and parachuted to the surface of Titan on January 14, 2005
- Goal to measure surface composition and conditions
Titan's Atmosphere
- Composition:
- 98% N2 (Nitrogen)
- 2% CH4 (Methane)
- Argon, hydrocarbons like Ethane
- Cold, dense atmosphere:
- Temperature: 94 K (-290 F)
- Pressure: ~1.6 Earth atmospheres
- Clouds of Nitrogen and methane ices
- Hydrocarbon "smog"
Titan's Surface
- Young surface with very few impact craters
- Varied terrain:
- Smooth, dark plains (methane mud flats?)
- Rugged highlands
- Drainage channels
- Impact basins
Is Methane Titan's "Water?"
- Methane (CH4) may play the same role on Titan that water does on the Earth:
- 94 K is between the boiling and freezing points of Methane
- Get gaseous methane in the atmosphere
- Methane condenses into clouds that rain liquid methane
- Signs of drainage flows
- Huygens landed in soft methane/water ice mud
- Water ice is like sand on Titan
Life in the Outer Solar System?
- Europa and Titan are considered the most promising sites to search for life in the Solar System after Mars
- Jupiter's Giant Moon Europa
- Liquid ocean under the ice?
- Life could be present
- Saturn's Giant Moon Titan
- Methane-based, rather than water-based, life could be present
- Enceladus may also harbor microbial life
See A Note about Graphics to learn
why some of the graphics shown in the lectures are not reproduced with
these notes.
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Updated: 2010 February 14
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