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Book ChapterDOI

Modelling Collisions Between Asteroids: From Laboratory Experiments to Numerical Simulations

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TLDR
In this article, the authors present a brief review of the current understanding of the fragmentation process of solid bodies and its im- plementation in numerical codes aimed at simulating asteroid break-up events.
Abstract
Thanks to the development of sophisticated numerical codes, a major breakthrough has been achieved in our understanding of the process involved in small body collisions. Such events play a fundamental role in all the stages of the formation and evolution of planetary systems, and more particularly of our Solar System. Laboratory experiments on centimeter-sized targets have been performed to improve our knowledge on this process, but their extrapolation to asteroid scales remains confronted to major difficulties. In this lecture, we present a brief review of our current understanding of the fragmentation process of solid bodies and its im- plementation in numerical codes aimed at simulating asteroid break-up events. The most recent results provided by numerical simulations are also presented. Although our current understanding is still based on several limitations and assumptions, the development of sophisticated numerical codes accounting for the fragmentation of an asteroid and for the gravitational interactions of the generated fragments have allowed to improve greatly our knowledge on the main mechanisms that are at the origin of some observed features in the asteroid belt. In particular, the simulations have demonstrated that, for bodies larger than several kilometers, the collisional process does not only involves the fragmentation of the asteroid but also the gravi- tational interactions between the fragments that are ejected. This latter mechanism can lead to the formation of large agregates by gravitational reaccumulation of smaller fragments, allowing to explain the presence of large members within aster- oid families. Numerical simulations of the complete process have thus been able to reproduce for the first time the main properties of asteroid families, each formed by the disruption of a large parent body, and also to derive some information on the possible internal structure of the parent bodies. A large amount of work remains however necessary to understand in deeper details the physical process as a function of material properties that are relevant to asteroids and to determine in a more quantitative way the outcome properties such as fragments' shapes and rotational states.

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Citations
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Journal ArticleDOI

The Asteroid Veritas: An intruder in a family named after it?

TL;DR: In this paper, the formation of the Veritas family via numerical simulations of catastrophic disruption of a 140-km-diameter parent body, which was considered to be made of either porous or non-porous material, and a projectile impacting at 3 or 5 km/s with an impact angle of 0° or 45°.

Is the Moon's Orbit "Ringing" from an Asteroid Collision Event which Triggered the Flood?

TL;DR: In this article, the authors use ordinary Newtonian orbital mechanics to explore the possibility that near side lunar maria are giant impact basins left over from a catastrophic impact event that caused the present orbital configuration of the moon.
Book ChapterDOI

Asteroids and Their Collisional Disruption

TL;DR: In this paper, the authors used impact experiments in laboratory, using as targets terrestrial rocks whose mechanical properties are similar to those of some meteorite meteorites to understand the collisional process between small bodies.
Book ChapterDOI

Asteroids from Observations to Models

TL;DR: In this paper, the authors discuss some specific applications to the rotation state and the shapes of moderately large asteroids, and techniques of observations putting some emphasis on the HST/FGS instrument.
Book ChapterDOI

On the Strength and Disruption Mechanisms of Small Bodies in the Solar System

TL;DR: Several important aspects of material strengths that are believed to be adapted to solar system small bodies and review the most recent studies of the different mechanisms that can be at the origin of the disruption of these bodies are discussed in this paper.
References
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Book

Fracture of Brittle Solids

TL;DR: In this article, the authors present a unified continuum, microstructural and atomistic treatment of modern day fracture mechanics from a materials perspective, focusing on the basic elements of bonding and microstructure that govern the intrinsic toughness of ceramics.
Book

Impact Cratering: A Geologic Process

H. J. Melosh
TL;DR: In this article, the authors derived the Hugoniot equations for impact cratering, and derived the state of the art for the state for the impact crater problem in the United States.
Journal ArticleDOI

The effect of cracks on the compressibility of rock

TL;DR: In this article, it was shown that porosity can be determined quite precisely from compressibility measurements, in particular for material in which all porosity occurs as narrow cracks, and that a crack increases compressibility nearly as much as a spherical pore of the same diameter as the length of the crack.
Journal ArticleDOI

Catastrophic Disruptions Revisited

TL;DR: In this article, the authors used a smooth particle hydrodynamics method to simulate colliding rocky and icy bodies from centimeter scale to hundreds of kilometers in diameter in an effort to define self-consistently the threshold for catastrophic disruption.
Book ChapterDOI

Smooth Particle Hydrodynamics: A Review

TL;DR: A review of the Smooth Particle Hydrodynamics (SPH) method is presented in this article, where the derivation of the SPH equations from the hydrodynamical conservation equations is discussed.
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