Naiad ( , , or as in Greek
Ναϊάδ-ες),
also known as
Neptune III, is the
innermost satellite of
Neptune named after the
Naiads
of
Greek legend.
Naiad was discovered sometime before mid-September, 1989 from the
images taken by the
Voyager 2
probe. The last moon to be discovered
during the flyby, it was designated
S/1989 N 6. The discovery was announced
on September 29, 1989 in the IAU Circular No. 4867, but the text
only talks of "25 frames taken over 11 days", giving a discovery
date of sometime before
September 18.
The name was given on 16 September 1991.
Naiad is irregularly shaped and probably has not been modified by
any internal geological processes after its formation. 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.
Naiad orbits about 23,500 km above Neptune's cloud tops. Since
this is below the
synchronous
orbit radius, its orbit is slowly decaying 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. Naiad orbits Neptune well
within its fluid Roche limit, and its density is expected to be low
enough that it may be very close to its actual Roche limit
already.
Since the
Voyager 2 flyby, the Neptune system has been
extensively studied from ground-based
observatories and the
Hubble Space Telescope as well.
In 2002-03
Keck
telescope
observed the
system using adaptive optics and
detected easily the largest four inner satellites. Thalassa
was found with some image processing, but Naiad was not located.
Hubble has the ability to detect all the known satellites and
possible new satellites even dimmer than
Voyager 2. Still,
Naiad has not been found. It is suspected that this is due to
considerable errors in Naiad's
ephemeris.
References
External links