| |
Jump
to: Page 1: Intro,
Atmosphere,
Great White Spot, Weather, Page 2:
Composition,
Making Heat
COMPOSITION:
On the whole, Saturn is about 75% hydrogen and 25% helium, with
traces of water vapor, methane, ammonia, and primordial solar
nebula
material. Hydrogen and helium are two of the lightest gases in the
Universe. As a result, Saturn is the least dense planet in the solar
system. With a density of .7 g/cc. Saturn is actually less dense
than water! If Saturn were hollowed out, there would be enough space
for 833 Earths inside it. However, the mass of Saturn is only around
the mass of 95 Earths. If one could find an ocean big enough, Saturn
would float! Scientists
believe that Saturn has a solid core similar to the core
of Jupiter. Made up of rock, it is believed to be
surrounded by liquid metallic hydrogen and helium,
followed by a layer of molecular hydrogen in liquid
state. This layer of molecular hydrogen is considered
the "surface" of Saturn.
 |
The Voyager 1 took this
picture of Saturn with Tethys and Dione. |
top...
|
MAKING HEAT:
Temperatures on Saturn range from 2.5 x 10^4 Kelvin in the
interior to 85 Kelvin in the tropopause of the atmosphere. Saturn is
one of the few planets in the solar system that actually releases
more heat than it receives from the sun. It releases about twice as
much as it gets. Scientists believe the heat is the result of two
possibilities. The first possibility is the "raining" of helium or
differentiation (ah! Sounds like calculus!). The distribution of
hydrogen and helium usually remain constant. However, when the
temperature is less than 10^4 Kelvin, helium becomes insoluble
(solid). Helium "raindrops" form and fall down to the
surface of Saturn. But as they drop through the atmosphere, the
temperature rises causing the "raindrops" to dissolve.
Dissolving gives off heat. The
second possibility is gradual gravitational
compression,
like the Kelvin-Helmholtz mechanism on Jupiter.
top...
|
|