Rings of Chariklo
The minor planet and centaur 10199 Chariklo, with a diameter of about 250 kilometres (160 mi), is the second smallest object with rings and the sixth ringed object ever discovered in the Solar System. Orbiting Chariklo is a bright ring system consisting of two narrow and dense bands, 6–7 km (4 mi) and 2–4 km (2 mi) wide, separated by a gap of 9 kilometres (6 mi). The rings orbit at distances of about 400 kilometres (250 mi) from the centre of Chariklo, a thousandth the distance between Earth and the Moon. The discovery was made by a team of astronomers using ten telescopes at various locations in Argentina, Brazil, and Chile in South America during observation of a stellar occultation on 3 June 2013, and was announced on 26 March 2014.
The existence of a ring system around a minor planet was unexpected because it had been thought that rings could only be stable around much more massive bodies. Ring systems around minor bodies had not previously been discovered despite the search for them through direct imaging and stellar occultation techniques. Chariklo's rings should disperse over a period of at most a few million years, so either they are very young, or they are actively contained by shepherd moons with a mass comparable to that of the rings. The team nicknamed the rings Oiapoque (the inner, more substantial ring) and Chuí (the outer ring), after the two rivers that form the northern and southern coastal borders of Brazil. A request for formal names will be submitted to the IAU at a later date.
It was proposed in January 2015 that 2060 Chiron has a similar pair of rings.
Chariklo is the largest confirmed member of a class of small bodies known as centaurs, which orbit the Sun between Saturn and Uranus in the outer Solar System. Forecasts had shown that, as seen from South America, it would pass in front of the 12.4-magnitude star UCAC4 248-108672, located in the constellation Scorpius, on 3 June 2013.
With the aid of thirteen telescopes located in Argentina, Brazil, Chile, and Uruguay, a team of astronomers led by Felipe Braga Ribas, a post-doctoral astronomer of the National Observatory (ON), in Rio de Janeiro, and 65 other researchers from 34 institutions in 12 countries, was able to observe this occultation event, a phenomenon during which a star disappears behind its occulting body. The 1.54-metre Danish National Telescope at La Silla Observatory, due to the much faster data acquisition rate of its 'Lucky Imager' camera (10 Hz), was the only telescope able to resolve the individual rings.
During this event, the observed magnitude was predicted to increase from 14.7 (star + Chariklo) to 18.5 (Chariklo alone) for at most 19.2 seconds. This increase of 3.8 magnitudes is equivalent to a decrease in brightness by a factor 32.5. The primary occultation event was accompanied by four additional small decreases in the overall intensity of the light curve, which were observed seven seconds before ingress and seven seconds after egress. These secondary occultations indicated that something was partially blocking the light of UCAC4 248-108672. The symmetry of the secondary occultations and multiple observations of the event in various locations helped reconstruct not only the shape and size of the object, but also the thickness, orientation, and location of the ring planes. The relatively consistent ring properties inferred from several secondary occultation observations discredit alternative explanations for these features, such as cometary-like outgassing.
The origin of the rings is unknown, but both are likely to be remnants of a debris disk, which could have formed via an impact on Chariklo, a collision with or between one or more pre-existing moons, tidal disruption of a former retrograde moon, or from material released from the surface by cometary activity or rotational disruption. If the rings formed through an impact event with Chariklo, the object must have impacted at a low velocity to prevent ring particles from being ejected beyond Chariklo's Hill sphere.
Impact velocities in the outer Solar System are typically ≈ 1 km/s (compared with the escape velocity at the surface of Chariklo of ≈ 0.1 km/s), and were even lower before the Kuiper belt was dynamically excited, supporting the possibility that the rings formed in the Kuiper belt before Chariklo was transferred to its current orbit less than 10 Myr ago. Impact velocities in the asteroid belt are much higher (≈ 5 km/s), which could explain the absence of such ring features in minor bodies within the asteroid belt. Collisions between ring particles would cause the ring to widen substantially, and Poynting–Robertson drag would cause the ring particles to fall onto the central body within a few million years, requiring either an active source of ring particles or dynamical confinement by small (kilometre-sized) embedded or shepherd moons yet to be discovered. Such moons would be very challenging to detect via direct imaging from Earth due to the small radial separation of the ring system and Chariklo.
The orientation of the rings is consistent with an edge-on view from Earth in 2008, explaining the observed dimming of Chariklo between 1997 and 2008 by a factor of 1.75, as well as the gradual disappearance of water ice and other materials from its spectrum as the observed surface area of the rings decreased. Also consistent with this edge-on orientation is that since 2008, the Chariklo system has increased in brightness by a factor of 1.5 again, and the infrared water-ice spectral features have reappeared. This suggests that the rings are composed at least partially of water ice. An icy ring composition is also consistent with the expected density of a disrupted body within Chariklo's Roche limit.
The equivalent depth (a parameter related to the total amount of material contained in the ring based on the viewing geometry) of C1R was observed to vary by 21% over the course of the observation. Similar asymmetries have been observed during occultation observations of Uranus's narrow rings, and may be due to resonant oscillations responsible for modulating the width and optical depth of the rings. The column density of C1R is estimated to be 30–100 g/cm2, indicative of a mass equivalent to an icy body two kilometres across.
C2R is half the width of the brighter ring, and resides just outside it, at 404.8 kilometres (251.5 mi). With an optical depth of about 0.06, it is markedly more diffuse than its companion. Altogether it contains approximately a twelfth the mass of C1R, roughly equivalent to an icy body a kilometre across.
Telescopes and observatories
Telescopes that observed the occultation included the Danish National Telescope and the survey telescope TRAPPIST of La Silla Observatory, the PROMPT Telescopes (Cerro Tololo Inter-American Observatory), the Brazilian Southern Astrophysical Research Telescope or SOAR (Cerro Pachón), the 0.45-metre ASH telescope (Cerro Burek), and those of the State University of Ponta Grossa Observatory, the Polo Astronomical Pole Casimiro Montenegro Filho (at the Itaipu Technological Park Foundation, in Foz do Iguaçu), the Universidad Católica Observatory of the Pontifical Catholic University of Chile (Santa Martina) and several at Estación Astrofísica de Bosque Alegre, operated by the National University of Córdoba. Negative detections were recorded by El Catalejo Observatory (Santa Rosa, La Pampa, Argentina), the 20-inch Planewave telescope (part of the Searchlight Observatory Network) at San Pedro de Atacama, Chile and the OALM instrument at Los Molinos Astronomical Observatory in Uruguay. Some of the other participating instruments were those at the National Observatory in Rio de Janeiro, the Valongo Observatory (at the Federal University of Rio de Janeiro), the Oeste do Paraná State University Observatory or Unioeste (in the state of Paraná), the Pico dos Dias Observatory or OPL (in Minas Gerais) and the São Paulo State University (UNESP – Guaratinguetá) in São Paulo,
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