Galatea (moon)

From Infogalactic: the planetary knowledge core
Jump to: navigation, search

<templatestyles src="Module:Hatnote/styles.css"></templatestyles>

Galatea
Galatea moon.jpg
Galatea as seen by Voyager 2 (elongation is due to smearing)
Discovery
Discovered by Stephen P. Synnott[1] and Voyager Imaging Team
Discovery date July 1989
Orbital characteristics[2]
Epoch 18 August 1989
61 953 ± 1 km
Eccentricity 0.00004 ± 0.00009
0.42874431 ± 0.00000001 d
Inclination
  • 0.052 ± 0.011° (to Neptune equator)
  • 0.06° (to local Laplace plane)
Satellite of Neptune
Physical characteristics
Dimensions 204×184×144 km (±~10 km)[3][4]
Mean radius
88 ± 4 km[5]
Volume ~2.8×106km³
Mass 2.12 ± 0.08 ×1018 kg[6]
Mean density
~0.75 g/cm³ (estimate)[5]
~0.018 m/s2[lower-alpha 1]
~0.056 km/s[lower-alpha 2]
synchronous
zero
Albedo 0.08[3][5]
Temperature ~51 K mean (estimate)
21.9[5]
Galatea inside of a faint ring arc near Neptune

Galatea (/ˈɡæləˈtə/ GAL-ə-TEE; Greek: Γαλάτεια), also known as Neptune VI, is the fourth closest inner satellite of Neptune. It is named after Galatea, one of the Nereids of Greek legend, whom Cyclops Polyphemus was in love with.

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[7] The discovery was announced (IAUC 4824) on August 2, 1989, but the text only talks of "10 frames taken over 5 days", giving a discovery date of sometime before July 28. The name was given on 16 September 1991.[8]

It 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.[9]

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

Galatea appears to be a shepherd moon for the Adams ring that is 1000 km 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.[10] Galatea's mass has been estimated based on the radial perturbations it induces on the ring.[6]

Notes

  1. Surface gravity derived from the mass m, the gravitational constant G and the radius r: Gm/r2.
  2. Escape velocity derived from the mass m, the gravitational constant G and the radius r: 2Gm/r.

References

  1. Planet Neptune Data http://www.princeton.edu/~willman/planetary_systems/Sol/Neptune/
  2. Lua error in package.lua at line 80: module 'strict' not found.
  3. 3.0 3.1 Lua error in package.lua at line 80: module 'strict' not found.
  4. Lua error in package.lua at line 80: module 'strict' not found.
  5. 5.0 5.1 5.2 5.3 Lua error in package.lua at line 80: module 'strict' not found.
  6. 6.0 6.1 Lua error in package.lua at line 80: module 'strict' not found.
  7. Lua error in package.lua at line 80: module 'strict' not found.
  8. Lua error in package.lua at line 80: module 'strict' not found.
  9. Lua error in package.lua at line 80: module 'strict' not found.
  10. Lua error in package.lua at line 80: module 'strict' not found.

External links