@article{c7dab8eabe794fb387ac473b12f9d7c0,
title = "Meteoroid Impacts as a Source of Bennu's Particle Ejection Events",
abstract = "Asteroid (101955) Bennu, a near-Earth object with a primitive carbonaceous chondrite-like composition, was observed by the Origins, Spectral Interpretation, Resource Identification, and Security-Regolith Explorer (OSIRIS-REx) spacecraft to undergo multiple particle ejection events near perihelion between December 2018 and February 2019. The three largest events observed during this period, which all occurred 3.5 to 6 hr after local noon, placed numerous particles <10 cm on temporary orbits around Bennu. Here we examine whether these events could have been produced by sporadic meteoroid impacts using the National Aeronautics and Space Administration's (NASA) Meteoroid Engineering Model 3.0. Most projectiles that impact Bennu come from nearly isotropic or Jupiter-family comets and have evolved toward the Sun by Poynting-Robertson drag. We find that 7,000-J impacts on Bennu occur with a biweekly cadence near perihelion, with a preference to strike in the late afternoon (~6 pm local time). This timing matches observations. Crater scaling laws also indicate that these impact energies can reproduce the sizes and masses of the largest observed particles, provided the surface has the cohesive properties of weak, porous materials. Bennu's ejection events could be caused by the same kinds of meteoroid impacts that created the Moon's asymmetric debris cloud observed by the Lunar Atmosphere and Dust Environment Explorer (LADEE). Our findings also suggest that fewer ejection events should take place as Bennu moves further away from the Sun, a result that can be tested with future observations.",
keywords = "Bennu, OSIRIS-REx, asteroids, ejecta, impacts, meteoroids",
author = "Bottke, {W. F.} and Moorhead, {A. V.} and Connolly, {H. C.} and Hergenrother, {C. W.} and Molaro, {J. L.} and P. Michel and Nolan, {M. C.} and Schwartz, {S. R.} and D. Vokrouhlick{\'y} and Walsh, {K. J.} and Lauretta, {D. S.}",
note = "Funding Information: We thank Keith Holsapple, Kevin Housen, and Jay Melosh for their comments that helped us to better understand the nature of hypervelocity impacts for micron‐ and millimeter‐sized bodies. We also thank Peter Brown and an anonymous referee for their helpful and constructive comments. We are grateful to the OSIRIS‐REx Team for making the encounter with Bennu possible. The Meteoroid Engineering Model is publicly available from NASA's Meteoroid Environment Office upon request ( https://www.nasa.gov/offices/meo/software/mem_detail.html ). The data generated in this work are reported in the text and figures. Model data and other numerical values can be found at the figshare repository: https://doi.org/10.6084/m9.figshare.11819448 (see Bottke, 2020 ). This paper is based upon work supported by NASA's OSIRIS‐REx mission through NASA Contract NNM10AA11C issued through the New Frontiers Program and Grant No. 80NSSC18K0226 as part of the OSIRIS‐REx Participating Scientist Program. The work of David Vokrouhlick{\'y} was partially funded by Grant 18‐06083S of the Czech Science Foundation. Funding Information: We thank Keith Holsapple, Kevin Housen, and Jay Melosh for their comments that helped us to better understand the nature of hypervelocity impacts for micron- and millimeter-sized bodies. We also thank Peter Brown and an anonymous referee for their helpful and constructive comments. We are grateful to the OSIRIS-REx Team for making the encounter with Bennu possible. The Meteoroid Engineering Model is publicly available from NASA's Meteoroid Environment Office upon request (https://www.nasa.gov/offices/meo/software/mem_detail.html). The data generated in this work are reported in the text and figures. Model data and other numerical values can be found at the figshare repository: https://doi.org/10.6084/m9.figshare.11819448 (see Bottke,?2020). This paper is based upon work supported by NASA's OSIRIS-REx mission through NASA Contract NNM10AA11C issued through the New Frontiers Program and Grant No. 80NSSC18K0226 as part of the OSIRIS-REx Participating Scientist Program. The work of David Vokrouhlick? was partially funded by Grant 18-06083S of the Czech Science Foundation. Publisher Copyright: {\textcopyright} 2020. The Authors.",
year = "2020",
month = aug,
day = "1",
doi = "10.1029/2019JE006282",
language = "English (US)",
volume = "125",
journal = "Journal of Geophysical Research: Planets",
issn = "2169-9097",
number = "8",
}