Abstract

Context.The vast majority of the geophysical and geological constraints (e.g., internal structure, cratering history) for main-belt asteroids have so far been obtained via dedicated interplanetary missions (e.g., ESA Rosetta, NASA Dawn). The high angular resolution of SPHERE/ZIMPOL, the new-generation visible adaptive-optics camera at ESO VLT, implies that these science objectives can now be investigated from the ground for a large fraction ofD≥ 100 km main-belt asteroids. The sharp images acquired by this instrument can be used to accurately constrain the shape and thus volume of these bodies (hence density when combined with mass estimates) and to characterize the distribution and topography ofD≥ 30 km craters across their surfaces.Aims.Here, via several complementary approaches, we evaluated the recently proposed hypothesis that the S-type asteroid (89) Julia is the parent body of a small compact asteroid family that formed via a cratering collisional event.Methods.We observed (89) Julia with VLT/SPHERE/ZIMPOL throughout its rotation, derived its 3D shape, and performed a reconnaissance and characterization of the largest craters. We also performed numerical simulations to first confirm the existence of the Julia family and to determine its age and the size of the impact crater at its origin. Finally, we utilized the images/3D shape in an attempt to identify the origin location of the small collisional family.Results.On the one hand, our VLT/SPHERE observations reveal the presence of a large crater (D~ 75 km) in Julia’s southern hemisphere. On the other hand, our numerical simulations suggest that (89) Julia was impacted 30–120 Myrs ago by aD~ 8 km asteroid, thereby creating aD≥ 60 km impact crater at the surface of Julia. Given the small size of the impactor, the obliquity of Julia and the particular orientation of the family in the (a,i) space, the imaged impact crater is likely to be the origin of the family.Conclusions.New doors into ground-based asteroid exploration, namely, geophysics and geology, are being opened thanks to the unique capabilities of VLT/SPHERE. Also, the present work may represent the beginning of a new era of asteroid-family studies. In the fields of geophysics, geology, and asteroid family studies, the future will only get brighter with the forthcoming arrival of 30–40 m class telescopes like ELT, TMT, and GMT.

Highlights

  • Our understanding of the surface composition of asteroids and its distribution across the asteroid belt has improved enormously over the last two decades; this is not the case for the surface topography and shape of asteroids

  • We performed numerical simulations to first confirm the existence of the Julia family and to determine its age and the size of the impact crater at its origin

  • The high angular resolution of SPHERE/ZIMPOL (∼20 mas at lambda = 600 nm; Schmid et al 2017), the new-generation visible adaptive-optics at ESO/VLT, implies that such a science objective can be investigated from the ground for a large fraction of D ≥ 100 km main-belt asteroids because most of these bodies display an angular diameter around opposition larger than 100 mas

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Summary

Introduction

Our understanding of the surface composition of asteroids and its distribution across the asteroid belt has improved enormously over the last two decades (see Burbine 2016 and Vernazza & Beck 2017 for recent reviews); this is not the case for the surface topography and shape of asteroids. Most large bodies (D ≥ 100 km) are seen as primordial remnants of the early solar system (Morbidelli et al 2009); in other words, their internal structure has likely remained intact since their formation, and they can be considered the smallest protoplanets For these objects, the macroporosity is expected to be minimal (≤10%) and their bulk density is an excellent tracer of their initial bulk composition and of their formation location. To make substantial progress in our understanding of the shape, internal compositional structure (i.e., density), and surface topography of large main-belt asteroids, we are carrying out an imaging survey As in the case of the single Keck image (see above), the occultations were mostly used as a consistency check (see Fig. B.2). 1 http://astro.troja.mff.cuni.cz/projects/asteroids3D

Reconstruction of Julia’s 3D shape with the ADAM algorithm
Method
Constraining the age of the Julia family and the size of the impact crater
Basic properties of the family
Constraining the family age
Conclusions
TRAPPIST-S
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