Saturn
 
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    Saturn is the sixth planet from the Sun and the second largest:

            orbit:    1,429,400,000 km (9.54 AU) from Sun
            diameter: 120,536 km (equatorial)
            mass:     5.68e26 kg

    In Roman mythology, Saturn is the god of agriculture. The associated Greek god, Cronus, was the son of
    Uranus and Gaia and the father of Zeus (Jupiter). Saturn is the root of the English word "Saturday".

    Saturn has been known since prehistoric times. Galileo was the first to observe it with a telescope in 1610;
    he noted its odd appearance but was confused by it. Early observations of Saturn were complicated by the
    fact that the Earth passes through the plane of Saturn's rings every few years as Saturn moves in its orbit. A
    low resolution image of Saturn therefore changes drastically. It was not until 1659 that Christiaan Huygens
    correctly inferred the geometry of the rings. Saturn's rings remained unique in the known solar system until
    1977 when very faint rings were discovered around Uranus and shortly thereafter around Jupiter and
    Neptune).

    Saturn was first visited by Pioneer 11 in 1979 and later by Voyager 1 and Voyager 2.

    Saturn is visibly flattened (oblate) when viewed through a small telescope; its equatorial and polar diameters
    vary by almost 10% (120,536 km vs. 108,728 km). This is the result of its rapid rotation and fluid state. The
    other gas planets are also oblate, but not so much so.

    Saturn is the least dense of the planets; its specific gravity (0.7) is less than that of water.

    Like Jupiter, Saturn is about 75% hydrogen and 25% helium with traces of water, methane, ammonia and
    "rock", similar to the composition of the primordial Solar Nebula from which the solar system was formed.

    Saturn's interior is similar to Jupiter's consisting of a rocky core, a liquid metallic hydrogen layer and a
    molecular hydrogen layer. Traces of various ices are also present.

    Saturn's interior is hot (12000 K at the core) and Saturn radiates more energy into space than it receives
    from the Sun. Most of the extra energy is generated by the Kelvin-Helmholtz mechanism as in Jupiter. But
    this may not be sufficient to explain Saturn's luminosity; some additional mechanism may be at work,
    perhaps the "raining out" of helium deep in Saturn's interior.

    The bands so prominent on Jupiter are much fainter on Saturn. They are also much wider near the equator.
    Details in the cloud tops are invisible from Earth so it was not until the Voyager encounters that any detail of
    Saturn's atmospheric circulation could be studied. Saturn also exhibits long-lived ovals and other features
    common on Jupiter. In 1990, HST observed an enormous white cloud near Saturn's equator which was not
    present during the Voyager encounters; in 1994 another, smaller storm was observed.

    Two prominent rings (A and B) and one faint ring (C) can be seen from the Earth. The gap between the A
    and B rings is known as the Cassini division; the much fainter gap in the A ring is known as the Encke Gap.
    The Voyager pictures show four additional faint rings. Saturn's rings, unlike the rings of the other planets, are
    very bright (albedo 0.2 - 0.6).

    Though they look continuous from the Earth, the rings are actually composed of innumerable small particles
    each in an independent orbit. They range in size from a centimeter or so to several meters. A few
    kilometer-sized objects are also likely.

    Saturn's rings are extraordinarily thin: though they're 250,000 km or more in diameter they're no more than
    1.5 kilometers thick. Despite their impressive appearance, there's really very little material in the rings -- if
    the rings were compressed into a single body it would be no more than 100 km across.

    The ring particles seem to be composed primarily of water ice, but they may also include rocky particles with
    icy coatings.

    Voyager confirmed the existence of puzzling radial inhomogeneities in the rings called "spokes" which were
    first reported by amateur astronomers. Their nature remains a mystery, but may have something to do with
    Saturn's magnetic field.

    Saturn's outermost ring, the F-ring, is a complex structure made up of several smaller rings along which
    "knots" are visible. Scientists speculate that the knots may be clumps of ring material, or mini moons. The
    strange braided appearance visible in the Voyager 1 images is not seen in the Voyager 2 images perhaps
    because Voyager 2 imaged regions where the component rings are roughly parallel.

    There are complex tidal resonances between some of Saturn's moons and the ring system: some of the
    moons, the so-called "shepherding satellites" (i.e. Atlas, Prometheus and Pandora) are clearly important in
    keeping the rings in place; Mimas seems to be responsible for the paucity of material in the Cassini division,
    which seems to be similar to the Kirkwood gaps in the asteroid belt; Pan is located inside the Encke Gap.
    The whole system is very complex and as yet poorly understood.

    The origin of the rings of Saturn (and the other jovian planets) is unknown. Though they may have had rings
    since their formation, the ring systems are not stable and must be regenerated by ongoing processes,
    probably the breakup of larger satellites.

    Like the other jovian planets, Saturn has a significant magnetic field.

    When it is in the nighttime sky, Saturn is easily visible to the naked eye. Though it is not nearly as bright as
    Jupiter, it is easy to identify as a planet because it doesn't "twinkle" like the stars do. The rings and the larger
    satellites are visible with a small astronomical telescope.
 
 

Planet Profile

    Mass (kg)                                               568.46 x (10^24)
    Volume (km3)                                        82,713 x (10^10)
    Radius (1 bar level) (km)
        Equatorial                                           60,268
        Polar                                                    54,364
    Volumetric mean radius (km)               58,232
    Ellipticity                                                  0.0980
    Mean density (kg/m^3)                          687
    Gravity (eq., 1 bar) (m/s^2)                   8.96
    Escape velocity (km/s)                          35.5
    GM (km^3/s^2)                                       37.931 x (10^6)
    Bond albedo                                           0.75
    Visual geometric albedo                       0.47
    Visual magnitude V(1,0)                      -8.88
    Solar irradiance (W/m^2)                      15.0
    Black-body temperature (K)                  63.9
    Moment of inertia (I/MR^2)                     0.210
    J2                                                             16,298 x (10^-6)
 

 That's great but what is this stuff?
 

Orbital parameters
 

    Semimajor axis (km)                             1,427.0 x (10^6)
    Sidereal orbit period (days)                 10,759.22
    Tropical orbit period (days)                  10,746.94
    Perihelion (km)                                       1,347.6 x (10^6)
    Aphelion (km)                                         1,506.4 x (10^6)
    Synodic period (days)                           378.09
    Mean orbital velocity (km/s)                  9.66
    Orbit inclination (deg)                            2.489
    Orbit eccentricity                                    0.05565
    Sidereal rotation period (hours)           10.500*
    Obliquity to orbit (deg)                           26.73

    * Saturnian System III coordinates
 
 

Saturnian Magnetosphere

     Dipole field strength:                                                            0.210 gauss-Rs^3
     Dipole tilt to rotational axis:                                                 < 1 degree
     Dipole offset (planet center to dipole center) distance:    0.04 to 0.05 Rs northward

    Note: Saturn's magnetic field has significant quadrapole and octapole moments, making approximation of
    the central field as an offset dipole difficult.
 
    Rs denotes Saturnian radii, 60,330 km
 

Saturnian Atmosphere

    Surface Pressure: >>100 bars
    Average temperature: ~97 K
    Temperature at 1 bar: ~134 K
    Density at 1 bar: ~0.19 kg/m3
    Wind speeds
       Up to ~400 m/s (<30 degrees latitude)
       Up to ~150 m/s (>30 degrees latitude)
    Scale height: 59.5 km
    Mean molecular weight: 2.07 g/mole
    Atmospheric composition
            Major:       Molecular hydrogen (H2) - 89%; Helium (He) - 11%

            Minor (ppm): Methane (CH4) - ~3000; Ammonia (NH3) - ~200;
                                   Ethane (C2H6) - ~2

            Aerosols:    Ammonia ice, water ice, ammonia hydrosulfide
 

 That's great but what is this stuff?
 

Saturn's Satellites

    Saturn has 18 named satellites, more than any other planet. There may very well also be several small ones
    yet to be discovered.

    Of those moons for which rotation rates are known, all but Phoebe and Hyperion rotate synchronously.
    The three pairs Mimas-Tethys, Enceladus-Dione and Titan-Hyperion interact gravitationally in such a way as
    to maintain stable relationships between their orbits: the period of Mimas' orbit is exactly half that of Tethys,
    they are thus said to be in a 1:2 resonance; Enceladus-Dione are also 1:2; Titan-Hyperion are in a 3:4
    resonance. In addition to the 18 named satellites, at least a dozen more have been reported and given
    provisional designations.
 
 
 
Satellite Distance 
(km)
Radius 
(km)
Mass 
(kg)
Discoverer Date
Pan 134,000 10 N/A Showalter 1990
Atlas 138,000 14 N/A Terrile 1980
Prometheus 139,000 46 2.70e^17 Collins 1980
Pandora 142,000 46 2.20e^17 Collins 1980
Epimetheus 151,000 57 5.60e^17 Walker 1980
Janus 151,000 89 2.01e^18 Dollfus 1966
Mimas 186,000 196 3.80e^19 Herschel 1789
Enceladus 238,000 260 8.40e^19 Herschel 1789
Tethys 295,000 530 7.55e^20 Cassini 1684
Telesto 295,000 15 N/A Reitsema 1980
Calypso 295,000 13 N/A Pascu 1980
Dione 377,000 560 1.05e^21 Cassini 1684
Helene 377,000 16 N/A Laques 1980
Rhea 527,000 765 2.48e^21 Cassini 1672
Titan 1,222,000 2575 1.35e^23 Huygens 1655
Hyperion 1,481,000 143 1.77e^19 Bond 1848
Iapetus 3,561,000 730 1.88e^21 Cassini 1671
Phoebe 12,952,000 110 4.00e^18 Pickering 1898
 
 

Saturn's Rings
 
 
 
Ring Distance 
(km)
Width 
(kg)
Mass 
(kg)
Surface Density 
(g/cm^2)
Albedo
D 67,000 7,500 N/A N/A N/A
C 74,500 17,500 1.1e^18 0.12 - 0.30 0.05 - 0.35
B 92,000 25,500 2.8e^19 0.4 - 0.6 0.4 - .25
A 122,200 14,600 6.2e^18 0.4 - 0.6 0.4 - 1.0
F 140,210 500 N/A 0.6 0.1
G 165,800 8000 1e^7 N/A 1.0 x (10^-6)
E 180,000 300,000 N/A N/A 1.5 x (10^-5)
    (distance is from Saturn's center to the ring's inner edge) This categorization is actually somewhat
    misleading as the density of particles varies in a complex way not indicated by a division into neat regions:
    there are variations within the rings; the gaps are not entirely empty; the rings are not perfectly circular.
 

 

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