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Transcript
Trans-Neptunian Objects and
Pluto
Astronomy 311
Professor Lee Carkner
Lecture 21
Trans-Neptunian Region

Beyond Neptune is the region of small, icy,
Trans-Neptunian Objects



The region is populated by icy planetesimals
that either formed at the edge of the solar
system or were ejected out by the planets
Pluto -- God of the Underworld
Pluto is the God of the
Dead in Roman
mythology


The Discovery of Pluto
In the late 1800’s it was believed that Neptune’s
orbit was being perturbed by a 9th planet


In 1930 a young astronomer named Clyde
Tombaugh found a very faint planet near Lowell’s
predicted position

The Discovery of Pluto
Observing Pluto
Through most telescopes Pluto simply
appears as a faint star

Recent attempts to develop a spacecraft
have been curtailed



Pluto Facts
Size: 2300 km


Orbit: 39.5 AU

Description:
Pluto’s Orbit
Pluto has the most eccentric and most
inclined orbit in the solar system



Pluto’s orbit carries it inside the orbit of
Neptune

Pluto is tipped on its side like Uranus
Composition of Pluto
Pluto has a density of 2000 kg/m3

Pluto is probably composed of ice and rock
Spectra of Pluto reveal the presence of
methane, nitrogen and carbon monoxide


HST Images Pluto
Features of Pluto


The other bright regions may be areas
where impacts have gouged out fresh
ice
Pluto and Charon
Charon
Pluto’s moon Charon was discovered as a
small bulge in a high resolution image (1978)


Pluto and Charon are in a close, tidally locked
orbit


Where Do Comets Come From?
Comets are small (few km) icy bodies that
sometimes come in to the inner solar system on
highly elliptical orbits
Short period comets



Long period comets



The Kuiper Belt
Around 1950 Kuiper and Edgeworth
proposed a belt of comets out beyond
Neptune

In 1992 the first (besides Pluto) Kuiper
belt object was discovered (QB1)


The Kuiper Belt
Discovering
Kuiper Belt
Objects
The Known Kuiper Belt
 There are now hundreds of known Kuiper Belt
Objects (KBOs)

 Total population of large KBO’s may be 70000 (larger
than 100 km)
 Kuiper belt seems to end at about 50 AU

 Larger and larger KBO’s being detected

 Larger than Pluto

Large KBO Sizes
Known KBOs as of 10/2003
Plutinos and Plutos

These orbits tend to minimize perturbations from
Neptune

Some KBO’s have fairly large sizes

2003 UB313 is probably larger than Pluto

Some may have dark surfaces and be hard to see
Is Pluto a Planet?
Pro




Con




What Makes Something a
Planet?
Planets used to be obvious

Needed new definition when rest of solar system
was discovered with telescopes

The International Astronomical Union (which has
authority over these things) calls Pluto a planet


The Oort Cloud
In 1950 Dutch astronomer Jan Oort
postulated a spherical shell of comets
surrounding the solar system at about
50,000 AU



Population of the Oort Cloud
The Oort cloud is the source of the long
period comets

They are too far away to see, so we only
have indirect methods of studying them

Diagram of the Oort Cloud
Summary
Past the orbit of Neptune the solar
system is made up of many small icy
bodies
Kuiper Belt
extends from 30-500 AU
formed from left over planetesimals at the
edge of the solar system
Oort Cloud
extends from 1000-100,000 AU
formed from ejected icy planetesimals
Summary: Pluto
Description: small, cold , distant
Pluto resembles a large Kuiper belt
object more than a planet
Has a closely orbiting large moon
Charon
Properties
Thin atmosphere
Very cold (~50 K)
Bright surface features possibly composed
of fresher ice