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Uranus

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No close-up images of Pluto's surface, but should be similar to Triton's ... Pluto and Charon must have lots of water ice. Water ice covered by N2 ice on Pluto, ... – PowerPoint PPT presentation

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Title: Uranus


1
Uranus
  • Discovery
  • All previous planets known since antiquity
  • Easily visible to the naked eye.
  • Uranus is at limit of best human eyesight from
    darkest sights
  • Uranus discovered
  • On March 13, 1781
  • By William Herschel
  • With telescope

2
Uranus Interior Structure
  • Composition
  • Contains less H and He than Jupiter
  • By percentage contains more volatiles, especially
    water
  • Surface composition is mostly H and He with
    traces of NH3, CH4, and water
  • Differentiated with silicates and metals in
    central core

3
Uranus Interior Structure
  • Core
  • Contains iron/nickel, silicates
  • Solid form due to the high pressure and
    composition
  • Inner Mantle
  • High pressure liquid water with dissolved
    minerals and/or NH3 and CH4
  • Solution is very good electrical conductor

4
Uranus Interior Structure
  • Outer Mantle
  • High pressure liquid hydrogen and helium

5
Uranus Interior Structure
  • Atmosphere
  • Top layer gaseous due to pressure
  • Mostly H and He with traces of NH3 and CH4
  • Appears generally featureless due to low
    temperatures (haze) and low UV flux for organic
    colorations
  • High contrast images show belt-zone structure
    similar to Jupiter and Saturn
  • Parallel to equator
  • Overall blue-green color due to methane
    absorption of yellow/red light

6
Uranus Magnetic Field
  • Little weaker than Earths
  • Not at the center of planet
  • Produced 30 of way from center in the liquid
    water inner mantle
  • Tipped 60 to the rotation axis
  • Interacts with solar wind

7
Uranus Rings
  • Very tenuous set of 9 rings
  • Composed of very dark dust particles
  • Either darkened ice or rocky particles
  • Extremely narrow, so must have shepherd
    satellites like Saturn
  • Voyager 2 detected two inside and outside
    outermost ring
  • Origin of rings unknown, but are inside Uranus
    Roche limit, so may be disrupted satellite

8
Uranus Satellites
  • 20 satellites plus ring particles
  • Satellites range from 1550 km to 20 km in size
    with a composition of ice and rock
  • Satellites orbit in plane of Uranus equator
  • Impact which tipped Uranus must have occurred
    early in protoplanet phase so that material out
    of which satellites formed was also tipped.

9
Neptune
  • Discovery
  • not bright enough to see with naked eye ? not
    known it ancient times
  • Unlike Uranus, existence and position was
    predicted
  • discovered Sept 23, 1864

10
Neptunes Interior Structure
  • Almost identical to Uranus
  • likely contains a bit more water, NH3, and CH4 by
    percentage (or less H and He)
  • rocky iron/nickel core
  • liquid water inner mantle
  • liquid hydrogen outer mantle
  • gaseous atmosphere composed mostly of H and He
    with some CH4 and NH3
  • Has a belt/zone structure, but is generally bland
    blue color
  • Occasional spots on surface

11
Neptunes Magnetic Field
  • Half as strong as Earths
  • Produced in liquid water mantle
  • Offset from center of planet, about halfway to
    the surface
  • Inclined 47 to axis of rotation

12
Neptunes Rings
  • Composed of very dark dust particles
  • Either darkened icy particles or rocky particles
  • Similar to Uranus ring particles
  • Distribution of particles in each ring is not
    uniform
  • Believed to be arcs
  • Voyager 2 showed that they were continuous

13
Neptunes Satellites
  • 8 known satellites not counting ring particles
  • Two largest have strange characteristics
  • Nereid is an icy and rocky moon about 300 km in
    diameter
  • In a very elliptical orbit with a period of
    almost 1 Earth year
  • Triton, 3/4 size of Moon

14
Triton
  • On retrograde orbit
  • Tenuous atmosphere
  • Composed of N2 and CH4
  • 1/100,000 density of Earths atmosphere
  • N2 seems to have seasonal cycles of vaporizing at
    one pole and solidifying at the other

15
Triton
  • Relatively young surface
  • Very few craters
  • Evidence of geologic activity
  • Heat source may be tidal heating (if orbit was
    more elliptical in past)
  • OR Triton may have a solid state version of the
    greenhouse effect (transparent solid nitrogen)
  • Composed of ices of N2, CH4, CO2, and CO

16
Pluto
  • Discovered 2/18/1930
  • Too dim to see even with small telescope
  • By Clyde Tombaugh
  • Blink comparator plates
  • Position predicted by Percival Lowell based on
    predictions from Neptunes orbit
  • Deviations were not gravitational, but
    observational error

17
Charon
  • Plutos only known satellite
  • About half the size of Pluto
  • ? 1.8 g/cc
  • More ice and less rock than Pluto
  • Pluto and Charon tidally locked to each other
  • Period of Charons orbit rotation period of
    both bodies 6.4 days

18
Plutos Atmosphere and Surface
  • Very tenuous atmosphere of N2 and CO
  • Similar to Tritons
  • No close-up images of Plutos surface, but should
    be similar to Tritons
  • Composed mostly of N2 ice with traces of CO
  • Poles are brighter than equatorial regions
  • N2 gas ? N2 ice cycle

19
Charons Atmosphere and Surface
  • Composed mostly of water ice
  • Pluto and Charon must have lots of water ice
  • Water ice covered by N2 ice on Pluto, whereas
    Charon has no atmosphere

20
Ice Dwarfs
  • Formed in outer solar system
  • 20 small (a few 100 km) icy objects have been
    detected between the orbit of Saturn (10AU) and
    60AU.
  • Probably planetesimals leftover from formation of
    solar system
  • If more abundant in past, could explain some
    collisions (Uranus, Titan)
  • May be the inner edge of the Kuiper Belt of
    comets
  • Pluto Charon possible examples
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