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Astronomy 171
Solar System Astronomy
Prof. Paul Martini
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Lecture 39: The Outer Solar System
Key Ideas:
- Trans-Neptunian Objects
- KBOs, SDOs, the Oort Cloud
- Orbits and Resonances
- Outer Dwarf Planets
- Pluto and its moons
- Eris and Dysnomia
- Comets
Trans-Neptunian Objects
- Class of icy bodies that orbit beyond Neptune
- Divided into various sub-classes
- Kuiper Belt Objects
- Scattered Disk Objects
- Oort Cloud
- Distinguished by their orbits
Kuiper Belt Objects (KBOs)
- Most Trans-Neptunian Objects are found in the Kuiper Belt
- Flattened region 30-50 AU from the Sun
- Scattered KBOs have long, elliptical orbits
- First KBOs discovered in 1992
- Many hundreds now known
- ~70,000 objects > 100km across
- Largest are >1000 km
Plutoinos ("little Plutos")
- KBOs in a 3:2 orbital resonance with Neptune:
- Complete 2 orbits for every 3 Neptune orbits
- Comprise ~25% of Trans-Neptunian Objects
- Orbits are similar to Pluto's
- About the same period and semimajor axis
- Different eccentricities, tilts, and orientations
Leftover Raw Materials
- Trans-Neptunian Objects are the icy planetesimals leftover from the formation of the Solar System
- New Horizon's Mission
- Launched January 2007
- July 14, 2015 Pluto fly-by
- Explore Kuiper Belt 2016-2020
Frozen Pluto
- Pluto is a cold, icy world:
- 1/1600th the sunlight received by Earth
- Temperature of 35-45 K
- Density is ~2g/cc with a rocky core and icy mantle
- Thin atmosphere:
- Surface covered with frozen N2 mixed with CH4
and traces of CO and H2O.
- Thin N2 atmosphere
- Moons:
- Pluto and Charon are tidally locked in a 1:1 tidal resonance
- Hydra and Nix are two new, smaller moons of Pluto discovered in 2005
How big is Eris?
- Too small to measure angular size
- Instead, the size is estimated based on reflectivity
- Perfect mirror? Albedo = 100% and Size = 2210km
- Fresh snow? Albedo = 90% and Size = 2330km
- Antarctica? Albedo = 80% and Size = 2475km
- Pluto-like? Albedo = 60% and Size = 2860km
- Charon? Albedo = 38% and Size = 3550km
- The lower the albedo, the large Eris must be to reflect the same (observed) amount of light
Comets
- Small chunks of ices and dust
- As they approach the Sun:
- The ices sublimate into gas
- Gas and dust are swept by sunlight into a luminous tail
- Many faint comets per year
- Bright, naked-eye comets every 10 years or so
- Comet McNaught is the "Great Comet of 2007"
- Comets are "dirty snowballs" that have fallen in from the outer solar system
Structure of Comets
- Nucleus:
- Dirty snowball of ices and dust a few kilometers across
- Contains >99% the mass of the comet
- Source of the gas and dust in the coma and tails
- Very low density ~0.2 g/cc
- Dark and heavily cratered
- Coma:
- Low-density cloud of gas and dust sublimed off the nucleus
- >100,000 km in size
Comet Tails
- Dust Tail:
- Dust particles swept back by sunlight pressure
- 1-10 million km long
- White color is reflected sunlight
- Ion Tail:
- Ionized atoms and molecules swept back by the solar wind
- 100 million km long
- Blue color is from CO+ emission lines
Comet Sample Return
- STARDUST - NASA Mission to return material from a comet
- Launched February 7, 1999
- Collected samples from the tail of "Wild 2"
- Returned to Earth on January 15, 2006
- Discovered many organic compounds and silicates
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: 2007 March 4
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