Secrets of Asteroid Minerva and its Moons
The campaign to “weigh” the asteroid and derive its density and other characteristics was undertaken by an international team of planetary astronomers led by Franck Marchis, researcher at the Carl Sagan Center of the SETI Institute. Marchis reported on their findings at the EPSC-DPS Joint Meeting 2011 in Nantes, France.
Minerva is the fourth asteroid located in the main-belt known to possess two moons. With a diameter of 156 km and two tiny 5-km size moons, this triple system orbits around the Sun between Mars and Jupiter. The two moons were discovered in 2009 using the Keck II telescope by members of this team. Other triple asteroids in the main-belt are 87 Sylvia (triplicity discovered in 2005), 45 Eugenia (2006), and 216 Kleopatra (2008). Marchis and his team were involved in the discovery of the triplicity of these asteroids and the follow-up studies.
“Very little was known about Minerva apart from the asteroid’s orbit around the Sun and a rough estimate of its size and shape. Shortly after the discovery of its two moons our group focused on re-analyzing previous data from ground-based and space telescopes, and organizing a campaign of new observations to better understand the nature of this intriguing asteroid,” said Marchis.
The team studied the asteroid in detail using the large W.M. Keck telescope in Hawaii and a small robotic telescope at Kitt Peak. Together, these observations enabled the astronomers to make precise determinations of the orbits of the moons by directly imaging the system and by detecting an eclipse event.
“Eighteen months after the discovery of the moons with the 10-m Keck II telescope we requested telescope time with the super-LOTIS telescope, a small 60-cm robotic telescope at Kitt Peak, to refine the spin period and shape of the large 156-km asteroid,” said Descamps, an astronomer at the Institut de Mecanique Celeste et de Calcul des Ephemerides at Paris, France.
“The determination of the shape was complicated by Minerva’s unusually round form,” emphasized Josef Durech, astronomer at Charles University in Prague, Czech Republic. “The shape model could not have been derived without combining these three types of data.”
Interestingly, the three other main-belt asteroids known to have moons have very elongated shapes, suggesting that Minerva may have a different interior composition or structure. Studying the composition of asteroids is important in determining whether or not they could have delivered materials to the early Earth that were essential for the origins of life.
The existence of moons around an asteroid provides a direct means of measuring the mass of the system, and if the size of the central asteroid is well known astronomers can derive its density as well. In the case of Minerva it was possible to determine the size of the asteroid in two different ways: by analyzing the stellar occultation event observed on December 24, 2010, and by re-analyzing archived data of the IRAS infrared space telescope obtained in 1983. Both methods indicate that Minerva has a diameter of about 156 km. Assuming a similar composition for the moons and the asteroid, and using the adaptive-optics observations from the Keck telescope, the team of astronomers have now concluded that the moons are tiny: around 5 km in diameter.
From the shape, size, and mass of the asteroid, the astronomers calculated its density to be 1.9 grams per cubic centimeter. Minerva appears to be a primitive type of asteroid known as a carbonaceous chondrite. Assuming it has the same composition as the denser carbonaceous chondrite meteorites collected on Earth, its macro-porosity, or percentage of empty space, is around 30 percent.
The asteroid 93 Minerva was discovered by J. C. Watson in 1867 at Ann Arbor, Michigan, and named after Minerva, the Roman equivalent of Athena, the goddess of wisdom. The moons orbit around the 156-km asteroid at distances of 650 km and 380 km in 58 hours and 27 hours, respectively (near the equator of the primary and in almost perfectly circular orbits). The moons have not yet received official names.
The coauthors of the EPSC-DPS presentation are F. Marchis and his student J.E. Enriquez of the Carl Sagan Center at the SETI Institute, CA; P. Descamps, J. Berthier, F. Vachier of the Institut de Mecanique Celeste et de Calcul des Ephemerides, France; J. Durech of Charles University in Prague, Czech Republic; P. Dalba, student at UC Berkeley, CA; A.W. Harris of the DLR Institute of Planetary Research, Berlin, Germany; J.P. Emery of the University of Tennessee at Knoxville; J. Melbourne of Caltech, Pasadena, CA; A. Stockton, H.-Y. Shih, K. Larson and T.J. Dupuy of the University of Hawaii, Honolulu; C.D. Fassnacht of the University of California at Davis, CA. The authors would like to thank the IOTA group for helping to coordinate and gather observations of the December 24, 2010, stellar occultation especially the observers: R. Peterson, G. Lucas, J. Ray, S. Herchak, J. Menke, W. Thomas, D.J. Dunham , B. Jones, S. Conard.