Rings of Neptune

The planet Neptune has a planetary ring system that is not very bright. It is made up of a few rings and some "ring arcs". The "ring arcs" are part of the outer ring called the Adams ring and are not to be seen anywhere else. The ring particles (small parts) are weirdly dark colored, and have large amounts of microscopic dust. Neptune has fourteen moons. Four of them orbit the planet inside the outermost rings.

 Discovery and observations 
The rings around Neptune could not be seen from Earth with strong telescopes. The evidence that they were there was first seen when scientists were watching the planet as it passed between the Earth and a star. (When this happens, the light of the star is blocked. This is called "stellar occulation".) Scientists watched this happen 50 times, and on five of those times in the early 1980s they saw the star give a little "blink" just before or after the planet covered it. This meant that rings around the planet were blocking the light, but the rings were not complete.

In 1989 the unmanned spacecraft Voyager 2 flew by Neptune. Voyager 2 sent back pictures that gave most of the information that scientists now have about the rings of Neptune. The pictures also help scientists to know why the rings looked incomplete. Not only did the pictures give a closer view, but they also showed the rings in a way that cannot ever be seen from earth. From earth the rings are always seen with the light of the sun shining towards them. When the spacecraft went past the planet, it took pictures with the sun shining behind the rings, as well. Big particles in the rings looked dark against the sunlight, but all tiny dust particles (microscopic dust) shone brightly when the sun was behind it. This allowed the scientists to work out what the rings were made of, and how all the particles were arranged.

As better types of telescopes have been developed, scientists can now see some of the rings from earth. The brightness of Neptune makes it hard to see the rings, which are much dimmer and the faintest rings still cannot be seen, even with vey powerful telescopes.

 Adams ring and the Ring Arcs 

The most famous of Neptune's rings is the thin outer Adams ring, although by comparison with the rings of the planets Saturn or Uranus, it is very hard to see. It was originally named as 1989 N1R. It is famous because it has a feature that has not been seen on any other planetary rings. These are three long narrow "arcs" which are much brighter and look more solid than the rest of the ring system. Each one spans from 4-10° of the whole ring. All the arcs are close to each other, spanning under 40° of longitude, only about 1/8th of the edge of the ring. It has been a puzzle to understand why the stuff in these arcs does not spread out evenly through the whole ring.

The three arcs have been named with French names Liberté, Égalité, and Fraternité. These names came from the famous saying of the French Revolution, which translates into English as "Liberty, Equality and Brotherhood!".  These names were suggested by the scientists who discovered them during stellar occultations in 1984 and 1985.

Four of Neptune's 13 moons are inside the ring system. The one that is nearest to the Adam's ring is called Galatea. It is a lumpy mass of rock that orbits around the planet at about the same speed as the planet is rotating. It is about 1000 kilometers inside the ring. It is the effect of the moon Galatea that is causing the three arcs in the Adam's ring. The ring also has 42 wiggles, which are like waves 30 kilometers high. Scientists are able to use this information to work out the mass of the moon Galatea. .

The best photos that came back from Voyager 2 showed that there are clumps of particles in the rings, but no-one can tell whether they are made of fine dust, or if there may be bigger particles in the clumps as well. All of Neptune's rings have a lot of microscopic dust but particularly the arcs of the Adam's ring. They looked very bright in the photos that Voyager 2 took with the sun shining behind them.
 There is much more dust in the rings of Neptune than there is in the rings of Saturn.

The Adams ring is very red. The background particles that make up the ring look twice as bright near the three arcs as they do on the side of the ring that is opposite the arcs.

 Arc dynamics 
With the arrival of the Hubble Space Telescope and adaptive optics ground-based telescopes the ring arcs have been re-examined several times, starting in July 1998.

  This has showed that they are amazingly active, changing a lot over only a few years: Fraternité and Égalité have been exchanging material and changing their lengths noticeably. Even more dramatically, Liberté appears to be fading away, being only 30% of its original 1989 brightness in 2003, and hardly visible in Hubble Space Telescope images from June 2005. In the meantime, it seems to have a split two-humped profile, and is now several degrees closer to the more stable Égalité. Courage, a very small and dim arc during the Voyager flyby, was seen to flare in brightness in 1998, while more recently it was back to its usual dimness but had advanced by an additional 8° ahead of the other arcs. That is, it appears to have jumped over to the next stable corotation resonance position. There were also some suggestions that the ring arcs may have been normally fading away.  Visible light observations show that the total amount of material in the arcs has remained about the same, but they are dimmer in the infra-red where previous observations were taken.  This activity of the ring arcs is not currently understood.

 Inner rings 
In addition to the outer Adams Ring, the other ring arrangements in the direction of Neptune's surface are:

 An unnamed, unclear, clumpy ring of dust in the orbit of Galatea.
 The large Lassell Ring (1989 N4R), is a thin sheet extending for 4000 km inwards of about 59,200 km radius. It is dusty but less than some of the other rings, being comparable in this situation to the continuous piece of the Adams ring. There is a brightness enhancement on its outer edge which has been called the Arago Ring (1989 N5R), and the Lassell Ring's inner edge is next to the LeVerrier Ring.IAUC 4867
 The narrow LeVerrier ring (1989 N2R) is the second most famous of Neptune's rings, and lies just outside the orbit of the moon Despina by about 700 km. It is very dusty, and very similar to the ring arcs.
 The innermost Galle Ring (1989 N3R) is very small and not well known. It is deep inside the orbit of the innermost of Neptune's moons, Naiad. The Galle Ring is very dusty similarly to the ring arcs.

Voyager pictures appear to also suggest a wide disc of scattered material extending inside of the 50,000 km radius which surrounds the Galle ring, but is difficult to tell apart from Neptune's brightness, and for this reason its existence is uncertain.

 List of rings 
+ Full rings Nasa Neptunian rings factsheet Name  orbitalradius (km) Width (km)  Optical depth  Dust fraction  Named after Galle  41,900  2000  0.00008  0.4 - 0.75  Johann Galle uncertain  < ≈ 50,000  wide    LeVerrier 53,200  110  0.002  0.4 - 0.8 Urbain Le Verrier Lassell  53,200 — 57,200  4000  0.00015  0.13 - 0.45  William Lassell Arago  57,200  <100    François Arago unnamed  61,950  narrow     Adams  62,933  50  0.0045  0.17 - 0.55  John Couch Adams

+ Arcs in Adams Ring Name  Width (km) 1989  Relative Longitude  Length  Strength  Notes198920031989 20031989 2003 Fraternité  15  ~0°  ~0°  10°  ~8°   strong     strong  "Trailing" arc Égalité  15  ~11°  ~13°  ~5°  ~8°  strong  strong  "Middle" arc Liberté  15  ~26°  ~25°  4°  ~4°  strong  weak  "Leading" arc Courage  15  ~33°  ~41°  ~2°  ~4°  weak  weak  All arcs have optical depths of the order of 0.12 and Dust fractions 0.4 − 0.8

The rings are named after astronomers who made important discoveries to the study of Neptune.

Four of Neptune's moons: Naiad, Thalassa, Despina, and Galatea orbit inside the ring system.

 References 

 Other websites 
 Neptune's Rings by NASA's Solar System Exploration

Category:Neptune