Particle size-frequency distributions of the osiris-rex candidate sample sites on asteroid (101955) bennu
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Burke, K.N.Dellagiustina, D.N.
Bennett, C.A.
Walsh, K.J.
Pajola, M.
Bierhaus, E.B.
Nolan, M.C.
Boynton, W.V.
Brodbeck, J.I.
Connolly, H.C., Jr
Deshapriya, J.D.P.
Dworkin, J.P.
Elder, C.M.
Golish, D.R.
Hoover, R.H.
Jawin, E.R.
McCoy, T.J.
Michel, P.
Molaro, J.L.
Nolau, J.O.
Padilla, J.
Rizk, B.
Robbins, S.J.
Sahr, E.M.
Smith, P.H.
Stewart, S.J.
Susorney, H.C.M.
Enos, H.L.
Lauretta, D.S.
Affiliation
Lunar and Planetary Laboratory, University of ArizonaIssue Date
2021
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Burke, K. N., DellaGiustina, D. N., Bennett, C. A., Walsh, K. J., Pajola, M., Bierhaus, E. B., ... & Lauretta, D. S. (2021). Particle Size-Frequency Distributions of the OSIRIS-REx Candidate Sample Sites on Asteroid (101955) Bennu. Remote Sensing, 13(7), 1315.Journal
Remote SensingRights
Copyright © 2021 by the authors. Licensee MDPI, Basel, Switzerland. This article is an open access article distributed under the terms and conditions of the Creative Commons Attribution (CC BY) license (https://creativecommons.org/licenses/by/4.0/).Collection Information
This item from the UA Faculty Publications collection is made available by the University of Arizona with support from the University of Arizona Libraries. If you have questions, please contact us at repository@u.library.arizona.edu.Abstract
We manually mapped particles ranging in longest axis from 0.3 cm to 95 m on (101955) Bennu for the Origins, Spectral Interpretation, Resource Identification, and Security–Regolith Explorer (OSIRIS-REx) asteroid sample return mission. This enabled the mission to identify candidate sample collection sites and shed light on the processes that have shaped the surface of this rubble-pile asteroid. Building on a global survey of particles, we used higher-resolution data from regional observations to calculate particle size-frequency distributions (PSFDs) and assess the viability of four candidate sites for sample collection (presence of unobstructed particles ≤ 2 cm). The four candidate sites have common characteristics: each is situated within a crater with a relative abundance of sampleable material. Their PSFDs, however, indicate that each site has experienced different geologic processing. The PSFD power-law slopes range from −3.0 ± 0.2 to −2.3 ± 0.1 across the four sites, based on images with a 0.01-m pixel scale. These values are consistent with, or shallower than, the global survey measurements. At one site, Osprey, the particle packing density appears to reach geometric saturation. We evaluate the uncertainty in these measurements and discuss their implications for other remotely sensed and mapped particles, and their importance to OSIRIS-REx sampling operations. © 2021 by the authors. Licensee MDPI, Basel, Switzerland.Note
Open access journalISSN
2072-4292Version
Final published versionae974a485f413a2113503eed53cd6c53
10.3390/rs13071315
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Except where otherwise noted, this item's license is described as Copyright © 2021 by the authors. Licensee MDPI, Basel, Switzerland. This article is an open access article distributed under the terms and conditions of the Creative Commons Attribution (CC BY) license (https://creativecommons.org/licenses/by/4.0/).