One of the most spectacular sights in the Solar System has
got to be Saturn’s majestic rings. Over the years, NASA’s Cassini spacecraft
has captured the beauty of Saturn’s ring system in breathtaking detail. Less
prominent ring systems also exist around Jupiter, Uranus and Neptune. Apart
from the giant planets, no rings are known to exist around any other smaller
objects until the surprising discovery by F. Braga-Ribas et al. (2014) of two
narrow rings around a minor planet named Chariklo. With an estimated size of
~250 km, Chariklo is the largest known Centaur - a group of objects orbiting
the Sun in a region of space between Saturn and Uranus. Chariklo is believed to
be a former trans-Neptunian object that was recently (i.e. less than 10 million
years ago) gravitationally perturbed by Uranus into a closer orbit around the
Sun.
Figure 1: An artist’s impression showing a close-up of what
Chariklo and its rings might look like. Image credit: ESO/L. Calçada/M. Kornmesser/Nick
Risinger.
On 3 June 2013, the occultation of a faint background star
by Chariklo was predicted to be observable from South America. A number of
telescopes at various sites across South America took measurements of the
occultation event. A few seconds before, and again, a few seconds after the
main occultation, two additional tiny dips in the star’s apparent brightness
were observed. This indicates the presence of two narrow rings around Chariklo
that is obscuring the star’s light. In fact, the rings around Uranus and
Neptune were found in much the same manner back in 1977 and 1984.
In particular, the Danish 1.54 m telescope at La Silla in
the Chilean Atacama Desert observed the occultation event with a cadence of ~10Hz.
The acquisition rate was high enough to resolve the secondary events occurring
before and after the main occultation as two separate rings identified as
2013C1R and 2013C2R (C1R and C2R in short). Based on the observational data,
C1R and C2R have estimated respective widths of about 7 and 3 km, optical
depths of 0.4 and 0.06, and orbital radii of 391 and 405 km. A gap of 9 km separates
the two rings. The inner ring (C1R) is estimated to have a cumulative mass
equivalent to an icy object with a diameter of roughly 1 km. The outer ring
(C2R), being somewhat narrower and more tenuous, has an estimated total mass corresponding
to an icy object with a size of ~500 m.
Figure 2: Light curve of the occultation event observed by
the Danish 1.54 m telescope on 3 June 2013. F. Braga-Ribas et al. (2014).
The rings around Chariklo are dynamically unstable and would
dissipate in a span of a few million years. As a result, the rings are either
very young or actively confined by the presence of one or more kilometre-size
shepherd moons around Chariklo. Observations of Chariklo between 1997 and 2008
show a gradual disappearance of the water-ice signature from the spectrum. It
implies that the rings are partly made of water-ice because during that period,
the rings would have appeared edge-on, resulting in the disappearance of the
water-ice signature. Observations made in 2013 show that the system has
brightened and the water-ice signature is detectable again as more of the
ring-plane becomes visible.
Several origins for Chariklo’s rings have been proposed. All
scenarios resulted in the presence of a disk of debris around Chariklo. The
debris came either from collisional events or from the tidal disruption of a
pre-existing moon. In the aftermath, the largest pieces of debris probably became
shepherd moons that shaped the rings into their present configuration. If the
rings are older than ~10 million years, they would have formed when Chariklo
was still in trans-Neptunian space and have thus survived the gravitational
perturbations by Uranus which brought Chariklo to its current orbit between
Saturn and Uranus. With this remarkable discovery, there are now 5 known
objects in the Solar System with rings around them - Jupiter, Saturn, Uranus,
Neptune and tiny Chariklo.
Reference:
F. Braga-Ribas et al., “A ring system detected around the
Centaur (10199) Chariklo”, Nature 508, 72-75 (03 April 2014)