uranus and neptune astronomy 311 professor lee carkner lecture 19
Post on 19-Dec-2015
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TRANSCRIPT
Discovery of Uranus
The other planets can only be seen with a telescope
Uranus was discovered in 1781 by William Herschel while surveying the sky Herschel had built a very high quality telescope
and was systematically observing the brighter stars when he found Uranus
Observing Uranus
Most of our information about Uranus comes from Voyager 2 and HST
No future missions planned
The Rotation of Uranus The tilt of Uranus’s axis is 98 degrees
Extreme tilt may be due to a large
impact when Uranus was forming
The large tilt produces seasons where half of the planet is in sunlight and half in darkness for long periods of time
Composition of Atmosphere
Hydrogen: 84 % Helium: 14 % Methane (CH4): 2%
The large amount of methane gives Uranus its bluish color
Structure of Atmosphere
Ammonia, Ammonium hydrosulfide and water have frozen out in the lower atmosphere where we can’t see them
Careful observations have determined that Uranus does not have alternating zones and bands Winds mostly blow east
Uranus’s Rings
As Uranus moved past a star, the star dimmed several times before being occulted by the planet
Rings are composed of dark material They reflect very little light and are difficult to
observe at optical wavelengths
The Moons of Uranus Uranus has 5 major moons and 22 minor
moons
Moons are composed of mixture of ice and rock
Two of the moons shepherd the Epsilon ring
The other rings may also have shepherd moons that are too small to see
Radiation Darkening Why are the moons and rings of Uranus
(and Neptune) so dark?
Impacts by high energy electrons from the magnetosphere break off the carbon atoms Carbon soot builds up on the ice
making it dark
Magnetic Fields Fields on Uranus and Neptune
May be formed by motions of a liquid water mantle containing ions
The centers of the magnetic fields are offset from the center of the planet How can the dynamo effect produce an off-centered
field?
Determining Mass
How are the masses of planets determined?
We can measure the period and the orbital radius of a moon or spacecraft The relationship between them depends
on mass
The Discovery of Neptune
Was an undiscovered planet altering the orbit?
In 1846 J. G. Galle used Le Verrier’s calculations to find Neptune after a 30 minute search
Observing Neptune
Neptune shows no detail from ground-based telescopes
Best images from Earth from the Hubble Space Telescope
Neptune’s Atmosphere
Neptune has visible storms like Jupiter, but they appear to be short lived
The white features in Neptune’s atmosphere are high altitude methane clouds
All seem to be moving east rather than in opposite directions
The Rings of Neptune
But stars were dimming by different amounts
Caused by the gravity of a near-by moon Inner narrow ring has shepherd moons
The Moons of Neptune
Triton’s orbit is unstable, in 100 million years it will be inside of the Roche limit giving Neptune a spectacular ring system
Triton may be a captured Kuiper Belt object
Interiors We can model each planet with a similar interior
Mantle of water and ammonia (Windex)
The two planets have relatively more heavy elements and less hydrogen than Jupiter and Saturn They also do not have enough gravity to produce
liquid metallic hydrogen
The Formation of Uranus and Neptune
At 20-30 AU the planetesimals were fewer and more widely dispersed than at 5-10 AU
By the time they formed much of the hydrogen and helium was dispersed
Summary Information comes from Voyager and HST Blue-green in color with white clouds
Caused by methane Radiation darkening produces dark, soot colored rings
and moons Interior composed of rocky core, water and ammonia
mantle and hydrogen atmosphere Offset magnetic field Formed more slowly than Jupiter and Saturn and so
captured less gas
Summary: Uranus
Discovered by survey (1781) Faint cloud patterns
Due to low internal heat Tilted on its axis
Causing non-uniform solar illumination