2017
DOI: 10.1038/s41598-017-10681-8
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Asteroid surface impact sampling: dependence of the cavity morphology and collected mass on projectile shape

Abstract: In-situ exploration and remote thermal infrared observation revealed that a large fraction of Solar System small bodies should be covered with granular regolith. The complex and varied geology of the regolith layer may preserve the historical records of the surface modification and topographic evolution experienced by asteroids, especially cratering processes, in which the projectile shape plays a crucial role. Regarding the impact sampling scheme, the projectile-shape dependence of both the cavity morphology … Show more

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Cited by 12 publications
(3 citation statements)
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“…For example, it has been used to simulate impact processes on the asteroids Eros and Itokawa to explain the origin of exposed boulders on their surfaces via the Brazil nut effect (Tancredi et al 2012), the removal of surface materials on asteroids by strong centrifugal forces resulting from rapid rotation (Hirabayashi et al 2015), and catastrophic collisional disruptions of planetesimals and reaccumulation of their fragments to explain the formation and the bilobate shape of several comets including 67P (Schwartz et al 2018). The DEM has also been used to address engineering problems such as hopping mechanisms to relocate landers on asteroids (Cheng et al 2019) and techniques to sample material from asteroid surfaces (Cheng et al 2017). However, DEM modeling has not yet been widely used to study the surface morphology or mechanical properties of cometary material -a material in a low-gravity environment that, in addition to dust, consists of ices, and where the ices may form sinter bonds and sublime.…”
Section: Introductionmentioning
confidence: 99%
“…For example, it has been used to simulate impact processes on the asteroids Eros and Itokawa to explain the origin of exposed boulders on their surfaces via the Brazil nut effect (Tancredi et al 2012), the removal of surface materials on asteroids by strong centrifugal forces resulting from rapid rotation (Hirabayashi et al 2015), and catastrophic collisional disruptions of planetesimals and reaccumulation of their fragments to explain the formation and the bilobate shape of several comets including 67P (Schwartz et al 2018). The DEM has also been used to address engineering problems such as hopping mechanisms to relocate landers on asteroids (Cheng et al 2019) and techniques to sample material from asteroid surfaces (Cheng et al 2017). However, DEM modeling has not yet been widely used to study the surface morphology or mechanical properties of cometary material -a material in a low-gravity environment that, in addition to dust, consists of ices, and where the ices may form sinter bonds and sublime.…”
Section: Introductionmentioning
confidence: 99%
“…The mesh with the higher spatial resolution is utilized to compute the contact force. For each active contact element, the normal and tangential contact force can be ascertained by using the Hertz contact model and Coulomb friction model as (Hertz 1881;Cheng et al 2017Cheng et al , 2018 (2022) for the calculations of δ nk and δ sk , as well as more details of the contact model. Assume the total number of the active contact elements for a pairing of contacting bodies is N. The resulting contact force acting on the two contact bodies, i and j, yields…”
Section: Governing Equationsmentioning
confidence: 99%
“…Multitarget missions that are already being conducted are focused mostly on small celestial bodies in our solar system (except multi-gravity-assist missions). Small celestial bodies attract vast research interest because of their great significance in various aspects [1][2][3][4]. NASA's Near Earth Asteroid Rendezvous (NEAR) Shoemaker performed a flyby of the asteroid 253 Mathilde on the way to the asteroid 433 Eros [5].…”
mentioning
confidence: 99%