THE STRUCTURE OF SATURN
Saturn is very similar to composition to
neighbouring Jupiter, about 96% hydrogen and 3% helium. The gaseous
make up gives the two planets low densities compared to the terrestrial
planets. However Saturn is much less than Jupiter, that of 0.7 times
that of water. With regards to its structure a rocky core is embedded
within an outer core of water, methane and ammonia. Above this is
a layer of liquid metallic hydrogen, , some 13,000 miles deep...over
which
lies a stratum of molecular hydrogen.
Again I comparison to Jupiter this planet
actually radiates more energy than it receives from the sun. The
continuous release of interior heat is more than likely to be responsible
for generating convection currents in the atmosphere, which in turn
gives rise to Saturn's high altitude clouds. The equatorial jet winds
at the cloud tops move faster than they do on Jupiter, around 1,100
feet per second, which amounts to two thirds the speed of sound
in the atmosphere there. This planet orbits much further from the
sun than Jupiter does, and therefore it is colder and experiences
less weather, and thus displaying fewer cloud features. However
telescopes have identified large bands of cloud, epitomized by the
recording of an enormous storm in 1990 by the Hubble Space Telescope.
THE RINGS
Saturn's rings remained unique within the
known solar system until 1977, when very faint rings were discovered
around Uranus.
Even now we are still not sure why this planet
has these rings, yet their mere presence and existence astounds
us all. I have long since looked towards answering such a question
myself, yet I too am left with the theories forwarded by others
to rely on. For me the best explanation is that the rings are in
actual fact the remains of a moon that strayed too close to the
planet and was pulled apart by Saturn's gravity. However there is
the possibility that a moon was smashed to pieces by a passing comet/asteroid
too. Another theory suggest that the rings are made of particles
that were unable to concentrate into a moon, again because of the
gravitational influence of the planet. However we can only theorize
as to the origins of the rings, and hope that some day some clue
will provide us with an answer.
Saturn's rings are immense, and very thin.
The measure approximately 170,000 miles in diameter, with a width
of 39,000 miles. However the big surprise is that they are less
than a mile and a half thick. whilst many illustrations, and indeed
the view from earth, would suggest that they are a solid disk, in
fact they consist of many smaller ringlets, each containing myriad
icy fragments and boulder size rocks. However despite their appearance
there is also a lot of empty space..if the rings were all packed
together to form a single body it would be no more than about 60
miles (100 km) across. Thus far there have been three main rings
recognized, which have been simply labeled A, B and C, with the
latter one being the fainter of the three (also called the crepe
ring). A gap called the 'Cassini Division' separates A and B, although
this is a little misleading as this 'gap region' contains four narrow
ringlets each measuring about 300 miles across. In the 1970s and
80s Voyager and Pioneer 11 images revealed a further four additional
faint rings. The innermost D ring consists of a few dusty and widely
spaced bands. The outermost E and G rings are, in essence, slight
concentrations of orbital debris and are very faint. Pioneer 11
detected the unusual F ring lying 2,200 miles outside the A ring.
This ring appears smooth in places but also has a set of knotted
and braided strands, shapes that arise partly from the gravitational
effects of the 'shepherd' satellites Pandora and Prometheus.
NAME
|
RADIUS
INNER
|
RADIUS
OUTER
|
WIDTH
|
D–Ring
|
67,000
|
74,500
|
7500
|
Guerin Division
|
|
|
|
C–Ring
|
74,500
|
92,000
|
17,500
|
Maxwell Division
|
87,500
|
88,000
|
500
|
B–ring
|
92,000
|
117,500
|
25,500
|
Cassini Division
|
115,500
|
120,600
|
4,800
|
Huygen's gap
|
117,680
|
|
285,440
|
A–Ring
|
122,200
|
136,800
|
14,600
|
Encke minima
|
126,430
|
129,940
|
3,500
|
Encke Division
|
133,410
|
133,740
|
|
Keeler Gap
|
136,510
|
136,550
|
|
F–Ring
|
140,210
|
|
30–500
|
G–Ring
|
165,800
|
173,800
|
8000
|
E–Ring
|
180,000
|
480,000
|
300,000
|
SATURN'S MOONS
Saturn has 34 named satellites, yet more
and more are being discovered all of the time (According to NASA
in 2006 there were 47 natural satellites). There are complex
tidal resonance's between some of Saturn's moons and the ring system.
Some of the moons, the so called 'shepherding satellites,' (Atlas,
Prometheus) are very important in keeping the rings in place by
herding Saturn's orbiting particles into distinct rings. Mimas
seems to be responsible for the paucity of material in the Cassini
division whilst Pan is located inside the Encke division.
SATELLITE
|
DISTANCE (KM)
|
RADIUS (KM)
|
MASS (KG)
|
Pan
|
134,000
|
10
|
Not known
|
Atlas
|
138,000
|
14
|
Not known
|
Prometheus
|
139,000
|
46
|
2.70e17
|
Pandora
|
142,000
|
46
|
2.20e17
|
Epimetheus
|
151,000
|
57
|
5.60e17
|
Janus
|
151,000
|
89
|
2.01e18
|
Mimas
|
186,000
|
196
|
3.80e19
|
Enceladus
|
238,000
|
260
|
8.40e19
|
Tethys
|
295,000
|
530
|
7.55e20
|
Telesto
|
295,000
|
15
|
Mass unknown
|
Calypso
|
295,000
|
13
|
Mass unknown
|
Dione
|
377,000
|
560
|
1.05e21
|
Helene
|
377,000
|
16
|
Mass unknown
|
Rhea
|
527,000
|
765
|
2.49e21
|
Titan
|
1,222,000
|
2575
|
1.35e23
|
Hyperion
|
1,481,000
|
143
|
1.77e19
|
Iapetus
|
3,561,000
|
730
|
1.88e21
|
Phoebe
|
12,952,000
|
110
|
4.00e18
|
|