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Astronomy 171
Solar System Astronomy
Prof. Paul Martini

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 Copyright © Paul Martini All Rights Reserved.