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The OSIRIS-REx target asteroid (101955) Bennu: Constraints on its physical, geological, and dynamical nature from astronomical observations

TLDR
In this article, the results of an extensive campaign to determine the physical, geological, and dynamical properties of asteroid (101955) Bennu were presented, and the results were used to develop a hypothetical timeline for Bennu's formation and evolution.
Abstract
We review the results of an extensive campaign to determine the physical, geological, and dynamical properties of asteroid (101955) Bennu. This investigation provides information on the orbit, shape, mass, rotation state, radar response, photometric, spectroscopic, thermal, regolith, and environmental properties of Bennu. We combine these data with cosmochemical and dynamical models to develop a hypothetical timeline for Bennu's formation and evolution. We infer that Bennu is an ancient object that has witnessed over 4.5 Gyr of solar system history. Its chemistry and mineralogy were established within the first 10 Myr of the solar system. It likely originated as a discrete asteroid in the inner Main Belt approximately 0.7–2 Gyr ago as a fragment from the catastrophic disruption of a large (approximately 100-km), carbonaceous asteroid. It was delivered to near-Earth space via a combination of Yarkovsky-induced drift and interaction with giant-planet resonances. During its journey, YORP processes and planetary close encounters modified Bennu's spin state, potentially reshaping and resurfacing the asteroid. We also review work on Bennu's future dynamical evolution and constrain its ultimate fate. It is one of the most Potentially Hazardous Asteroids with an approximately 1-in-2700 chance of impacting the Earth in the late 22nd century. It will most likely end its dynamical life by falling into the Sun. The highest probability for a planetary impact is with Venus, followed by the Earth. There is a chance that Bennu will be ejected from the inner solar system after a close encounter with Jupiter. OSIRIS-REx will return samples from the surface of this intriguing asteroid in September 2023.

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Journal ArticleDOI

OSIRIS-REx: Sample Return from Asteroid (101955) Bennu

TL;DR: The OSIRIS-REx spacecraft departed for near-Earth asteroid (101955) Bennu via an United Launch Alliance Atlas V 411 evolved expendable launch vehicle at 7:05 p.m. EDT on September 8, 2016, on a seven-year journey to return samples from Bennu as discussed by the authors.
Journal ArticleDOI

Properties of Rubble-Pile Asteroid (101955) Bennu from OSIRIS-REx Imaging and Thermal Analysis

Daniella DellaGiustina, +57 more
- 19 Mar 2019 - 
TL;DR: Using images and thermal data from NASA's Origins, Spectral Interpretation, Resource Identification, and Security-Regolith Explorer (OSIRIS-REx) spacecraft, this paper showed that asteroid (101955) Bennu's surface is globally rough, dense with boulders, and low in albedo.
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Hayabusa2 Mission Overview

TL;DR: The Hayabusa2 mission as mentioned in this paper was the first mission to explore a C-type near-Earth asteroid (162173) Ryugu (1999 JU3) to observe and explore the 900 m-sized object, and return samples collected from the surface layer.
References
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Journal ArticleDOI

Debiased Orbital and Absolute Magnitude Distribution of the Near-Earth Objects

TL;DR: In this article, a best-fit model of the near-Earth objects (NEOs) population is presented, which is fit to known NEs discovered or accidentally rediscovered by Spacewatch.
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THE YARKOVSKY AND YORP EFFECTS: Implications for Asteroid Dynamics

TL;DR: The Yarkovsky and YORP effects are thermal radiation forces and torques that cause small objects to undergo semimajor axis drift and spin vector modifications, respectively, as a function of their spin, orbit, and material properties as discussed by the authors.
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A Population of Comets in the Main Asteroid Belt

TL;DR: Optical data is presented showing the existence of a population of comets originating in a third reservoir: the main asteroid belt, which lends new support to the idea that main-belt objects could be a major source of terrestrial water.
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Linking the collisional history of the main asteroid belt to its dynamical excitation and depletion

TL;DR: This paper used a collisional evolution code to track the evolution of the main belt over 4.6 Gyr and found that only a small fraction of the fragments survived the dynamical depletion event described above.
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Fast and Slow Rotation of Asteroids

TL;DR: In this paper, the authors present an analysis of the distribution of asteroid spin rates vs. size, and find that significant populations of both slow and fast rotators among asteroids smaller than D =40 km, and especially below 10 km.
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