Artículo

Collisional study of Hilda and quasi-Hilda asteroids

Zain, Patricio Salvador Icon; Di Sisto, Romina Paula Icon; Gil-hutton, Ricardo Alfredo Icon

Otros responsables

Fecha

02/2025

Editorial

EDP Sciences

Revista

Astronomy and Astrophysics

Título del libro

Nombre del evento

Fecha del evento

Institución organizadora

ISSN

0004-6361

eISSN

ISBN

Idioma

Inglés

Tipo del evento

Clasificación temática

Resumen

Context. The Hilda asteroids are located in the outer main belt (MB) in a stable 3:2 mean-motion resonance (MMR) with Jupiter,while the quasi-Hildas have similar orbits but are not directly under the effect of the MMR. Moreover, cometary activity has beendetected in quasi-Hildas.Aims. In this study, we aim to investigate the collisional evolution of Hilda asteroids and apply it to an investigation into the cratering onasteroid (334) Chicago; we also intend to determine whether impacts between Hildas and quasi-Hildas can serve as a viable mechanismfor inducing cometary activity.Methods. Using the Asteroid Collisions and Dynamic Computation (ACDC) code, we simulated the collisional evolution of Hildaasteroids over a period of 4 Gyr. We considered three initial size-frequency distributions (SFDs) and two scaling laws for the collisionaloutcomes and performed a large set of simulations for each scenario, which we used to construct median SFDs of the Hilda population.We also derived an impactor SFD on asteroid (334) Chicago and used it to calculate the crater SFD on (334) Chicago. Additionally,we evaluated the sub-catastrophic impact timescale between Hilda and quasi-Hilda objects.Results. The observed SFD of Hilda asteroids larger than 3 km is best matched by scenarios assuming that such an SFD is mostlyprimordial, implying minimal collisional activity over time. For smaller sizes, although unconstrained, the SFD steepens significantlydue to the catastrophic fragmentation of a small number of multi-kilometre-sized bodies. We determined that the largest impactor on(334) Chicago measures a few kilometres in size, resulting in a maximum crater size of approximately 30 km. Furthermore, the slopeof the crater SFD mirrors that of the initial SFD for sub-kilometric bodies. While impact events between Hildas and quasi-Hildascan induce observable activity, and although it is stochastic in nature, the timescale of such events exceeds the dynamical lifetime ofquasi-Hildas, making them an unlikely primary mechanism for inducing observable activity.

Aprobación

Revisión

Complementado por

Referenciado por

Licencia Creative Commons

Excepto donde se indique lo contrario, la licencia de este ítem se describe como by-nc-sa