T276 Big Science from Small Worlds
Wednesday, 25 September 2024
1:30 PM - 5:30 PM
213A
INSIGHTS INTO REGOLITH DEVELOPMENT ON RUBBLE-PILE ASTEROID (101955) BENNU FROM REMOTE SENSING AND SAMPLE ANALYSIS
Paper number: T276-5
Program: Technical Sessions
Time: 2:25 PM – 2:45 PM
Authors
-
Ronald-Louis Ballouz Presenting AuthorJohns Hopkins University Applied Physics Laboratory, Laurel, MD
-
Andrew J. RyanUniversity of Arizona, Tucson, AZ
-
Olivier S. BarnouinJohns Hopkins University Applied Physics Laboratory, Laurel, MD
-
Robert J. MackeVatican City State
-
Harold C. ConnollyAmerican Museum of Natural History, New York, NY
-
Harold C. ConnollyUniversity of Arizona, Tucson, AZ
-
Harold C. ConnollyRowan University, Glassboro, NJ
-
Dante S. LaurettaUniversity of Arizona, Tucson, AZ
Abstract
Here, we focus on the physical evolution of the boulder population on Bennu. The combined census of boulders and craters on Bennu showed that boulders effectively armor the surface against impacts, frustrating the formation of small (<~ 2 m) craters. The effect of the armoring process is also evident in high-resolution images of small craters formed on the surfaces of Bennu boulders. We present evidence for in situ collisional processing of boulders. We leverage the high-resolution images and altimetry data from OSIRIS-REx to better understand the boulder disruption process. Our findings suggest an evolutionary path for boulder fragmentation on asteroids, where (i) an impact generates widespread fractures and flaws within the target, and (ii) subsequently, a lower-strain-rate process (e.g., thermal fatigue) results in the complete fracturing of the boulder, while allowing the fragments to be retained on a micro-gravity surface. We will discuss this evolutionary pathway in the context of evidence from density measurements and X-ray computed tomography data of the Bennu sample. The combined remote sensing and sample analysis results inform our understanding of regolith development on small solar system bodies.
Geological Society of America Abstracts with Programs. Vol. 56, No. 5
doi: 10.1130/abs/2024AM-403895
© Copyright 2024 The Geological Society of America (GSA), all rights reserved. Permission is hereby granted to the author(s) of this abstract to reproduce and distribute it freely, for noncommercial purposes. Permission is hereby granted to any individual scientist to download a single copy of this electronic file and reproduce up to 20 paper copies for noncommercial purposes advancing science and education, including classroom use, providing all reproductions include the complete content shown here, including the author information. All other forms of reproduction and/or transmittal are prohibited without written permission from GSA Copyright Permissions.