Abstract:From a set of adaptive optics (AO) observations collected with the W.M. Keck telescope between August and September 2009, we derived the orbital parameters of the most recently discovered satellites of the large C-type asteroid (93) Minerva. The satellites of Minerva, which are approximately 3 and 4 km in diameter, orbit very close to the primary (~5 & ~8 × R p and ~1% & ~2% × R Hill ) in a circular manner, sharing common characteristics with most of the triple asteroid systems in the main-belt. Combining these AO observations with lightcurve data collected since 1980 and two stellar occultations in 2010 & 2011, we removed the ambiguity of the pole solution of Minerva's primary and showed that it has an almost regular shape with an equivalent diameter D eq = 154 ± 6 km in agreement with IRAS observations. The surprisingly high bulk density of 1.75 ± 0.30 g/cm 3 for this C-type asteroid, suggests that this taxonomic class is composed of asteroids with different compositions, For instance, Minerva could be made of the same material as dry CR, CO, and CV meteorites. We discuss possible scenarios on the origin of the system and conclude that future observations may shine light on the nature and composition of this fifth known triple main-belt asteroid.
Keyword:Asteroids -Satellites of asteroids -Adaptive optics -Photometry -Orbit determination -Interior 1 Introduction The serendipitous discovery of Dactyl, a companion of the main-belt asteroid (243) Ida, seen during the Galileo spacecraft voyage to Jupiter (Chapman et al. 1995), gave birth to a new field of study for small solar system bodies. Today, using techniques such as high angular resolution imaging with the Hubble Space Telescope (HST), adaptive optics (AO) on ground-based telescopes, radar observations and photometric studies, about 200 multiple asteroids (asteroids with one or several moons) are known in all populations of small solar system bodies, from the Near-Earth Asteroids to the Kuiper Belt Objects. The study of these multiple asteroids is an opportunity for planetary astronomers to obtain insights on the asteroids such as their masses and densities and how these quantities possibly relate to their compositions, see e.g. Marchis et al. 2012a. Their existence and the understanding of their formation and evolution also provide a direct window to the history of our solar system. In this work, we describe a study of one of these recently discovered triple asteroid systems. (93) Minerva is a large (H v = 7.7, P spin = 5.97909 hours in Tungalag 2002) asteroid discovered by J.C. Watson at Ann Arbor, MI, USA in 1867. Located in the middle of the main-belt (a Minerva = 2.75 AU, e Minerva = 0.14, i Minerva = 9 deg), it was initially classified as a member of an old collisional family (1.2 ± 0.4 Gyrs) named "Gefion" consisting of 973 members based on Nesvorny et al. (2005). Because most of the members of this family are identified as S-type, and (93) Minerva is known to be a C b -type (Lazarro et al. 2004) Ryan & Woodward, 2010). There is a clear ...