Galatea (moon)

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Galatea (moon)

Galatea /ɡæləˈtə/, also known as Neptune VI, is the fourth-closest inner moon of Neptune, and fifth-largest moon of Neptune. It is named after Galatea, one of the fifty Nereids of Greek legend, with whom Cyclops Polyphemus was vainly in love.

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Galatea
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Galatea as seen by Voyager 2 (elongation is due to smearing)
Discovery
Discovered byStephen P. Synnott[1] and Voyager Imaging Team
Discovery dateJuly 1989
Designations
Designation
Neptune VI
Pronunciation/ɡæləˈtə/[2]
Named after
Γαλάτεια Galateia
AdjectivesGalatean[3]
Orbital characteristics[4][5]
Epoch 18 August 1989
61952.57 km
Eccentricity0.00022 ± 0.00008
0.42874431 ± 0.00000001 d
Inclination
  • 0.052 ± 0.011° (to Neptune equator)
  • 0.06° (to local Laplace plane)
Satellite ofNeptune
Groupring shepherd
Physical characteristics
Dimensions(204±10)×(184±16)×(144±8) km[6]
88±4 km[6]
Volume~2.8×106 km3[a]
Mass1.94×1018 kg[8]
Mean density
~0.69 g/cm3[b]
~0.012–0.025 m/s2[c]
~0.05–0.06 km/s[d]
synchronous
zero
Albedo0.08[6][9]
Temperature~51 K mean (estimate)
21.9[9]
    Close

    Discovery

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    Galatea inside of a faint ring arc near Neptune

    Galatea was discovered in late July 1989 from the images taken by the Voyager 2 probe. It was given the temporary designation S/1989 N 4.[10] The discovery was announced (IAUC 4824) on 2 August 1989, and mentions "10 frames taken over 5 days", implying a discovery date of sometime before July 28. The name was given on 16 September 1991.[11]

    Physical properties

    Galatea is irregularly shaped and shows no sign of any geological modification. It is likely that it is a rubble pile re-accreted from fragments of Neptune's original satellites, which were smashed up by perturbations from Triton soon after that moon's capture into a very eccentric initial orbit.[12]

    Compositionally, Galatea appears to be similar to other small inner Neptunian satellites, with a deep 3.0 micron feature attributed to water ice or hydrated silicate minerals. It has a 0.08 albedo at 1.4 and 2.0 microns, dropping to 0.04 at 3.0 microns, and increasing to 0.12 at 4.6 microns.[13]

    Orbit

    Galatea's orbit lies below Neptune's synchronous orbit radius, so it is slowly spiralling inward due to tidal deceleration and may eventually impact the planet or break up into a new planetary ring system upon passing its Roche limit due to tidal stretching.

    Galatea appears to be a shepherd moon for the Adams ring that is 1,000 kilometres (620 mi) outside its orbit. Resonances with Galatea in the ratio 42:43 are also considered the most likely mechanism for confining the unique ring arcs that exist in this ring.[14] Galatea's mass has been estimated based on the radial perturbations it induces on the ring.[15][7]

    Notes

    Summarize
    Perspective
    1. Volume derived from the long axis A, the medium axis B and the short axis C:
    2. Density derived from mass m and the volume V:
    3. Surface gravity derived from the mass m, the gravitational constant G and the radius r:
    4. Escape velocity derived from the mass m, the gravitational constant G and the radius r:

    Since Galatea is irregularly shaped, the actual surface gravity and escape velocity will vary significantly between different positions on the surface.

    References

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