High-Speed Boulders and the Debris Field in DART Ejecta

dc.contributor.authorFarnham, Tony L.
dc.contributor.authorSunshine, Jessica M.
dc.contributor.authorHirabayashi, Masatoshi
dc.contributor.authorErnst, Carolyn M.
dc.contributor.authorDaly, R. Terik
dc.contributor.authorAgrusa, Harrison F.
dc.contributor.authorBarnouin, Olivier S.
dc.contributor.authorLi, Jian-Yang
dc.contributor.authorKumamoto, Kathryn M.
dc.contributor.authorSyal, Megan Bruck
dc.contributor.authorWiggins, Sean E.
dc.contributor.authorBjonnes, Evan
dc.contributor.authorStickle, Angela M.
dc.contributor.authorRaducan, Sabina D.
dc.contributor.authorCheng, Andrew F.
dc.contributor.authorGlenar, David A.
dc.contributor.authorLolachi, Ramin
dc.contributor.authorStubbs, Timothy J.
dc.contributor.authorFahnstock, Eugene G.
dc.contributor.authorAmoroso, Marilena
dc.contributor.authorBertini, Ivano
dc.contributor.authorBrucato, John R.
dc.contributor.authorCapannolo, Andrea
dc.contributor.authorCremonese, Gabriele
dc.contributor.authorDall'Ora, Massimo
dc.contributor.authorCorte, Vincenzo Della
dc.contributor.authorDeshapriya, J. D. P.
dc.contributor.authorDotto, Elisabetta
dc.contributor.authorGai, Igor
dc.contributor.authorHasselmann, Pedro H.
dc.contributor.authorIeva, Simone
dc.contributor.authorImpresario, Gabriele
dc.contributor.authorIvanovski, Stavro L.
dc.contributor.authorLavagna, Michele
dc.contributor.authorLucchetti, Alice
dc.contributor.authorMarzari, Francesco
dc.contributor.authorEpifani, Elena Mazzotta
dc.contributor.authorModenini, Dario
dc.contributor.authorPajola, Maurizio
dc.contributor.authorPalumbo, Pasquale
dc.contributor.authorPirrotta, Simone
dc.contributor.authorPoggiali, Giovanni
dc.contributor.authorRossi, Alessandro
dc.contributor.authorTortora, Paolo
dc.contributor.authorZannoni, Marco
dc.contributor.authorZanotti, Giovanni
dc.contributor.authorZinzi, Angelo
dc.date.accessioned2025-07-09T17:55:05Z
dc.date.issued2025-06-20
dc.description.abstractOn 26 September 2022 the Double Asteroid Redirection Test (DART) spacecraft collided with Dimorphos, the moon of the near-Earth asteroid 65803 Didymos, in a full-scale demonstration of a kinetic impactor concept. The companion LICIACube spacecraft documented the aftermath, capturing images of the expansion and evolution of the ejecta from 29 to 243 s after the impact. We present results from our analyses of these observations, including an improved reduction of the data and new absolute calibration, an updated LICIACube trajectory, and a detailed description of the events and phenomena that were recorded throughout the flyby. One notable aspect of the ejecta was the existence of clusters of boulders, up to 3.6 m in radius, that were ejected at speeds up to 52 m s⁻¹. Our analysis of the spatial distribution of 104 of these boulders suggests that they are likely the remnants of larger boulders shattered by the DART spacecraft in the first stages of the impact. The amount of momentum contained in these boulders is more than 3 times that of the DART spacecraft, and it is directed primarily to the south, almost perpendicular to the DART trajectory. Recoil of Dimorphos from the ejection of these boulders has the potential to change its orbital plane by up to a degree and to impart a non-principal axis component to its rotation state. Damping timescales for these phenomena are such that the Hera spacecraft, arriving at the system in 2026, should be able to measure these effects.
dc.description.sponsorshipThis study was supported in part by the DART mission, National Aeronautics and Space Administration (NASA) contract No. 80MSFC20D0004 to JHU/APL. H.A. was supported by the French government, through the UCA J.E.D.I. Investments in the Future project managed by the National Research Agency (ANR) with the reference number ANR-15-IDEX-01. Portions of this work were performed under the auspices of the U.S. Department of Energy by Lawrence Livermore National Laboratory under Contract DE-AC52- 07NA27344. LLNL-JRNL-2002297. R. L. and D. G. acknowledge support by the NASA/GSFC Internal Scientist Funding Model (ISFM) Exospheres, Ionospheres, Magnetospheres Modeling (EIMM) team, and the NASA Solar System Exploration Research Virtual Institute (SSERVI). R. L. and D. A. acknowledge work done through the Center for Research and Exploration in Space Science and Technology (CRESST-II) supported by NASA award number 80GSFC24M0006. The LICIACube team members acknowledge financial support from Agenzia Spaziale Italiana (ASI, contract No. 2019-31-HH.0 CUP F84I190012600).
dc.description.urihttp://arxiv.org/abs/2506.16694
dc.format.extent47 pages
dc.genrejournal articles
dc.genrepreprints
dc.identifierdoi:10.13016/m2j0w9-zdsa
dc.identifier.urihttps://doi.org/10.48550/arXiv.2506.16694
dc.identifier.urihttp://hdl.handle.net/11603/39261
dc.language.isoen_US
dc.relation.isAvailableAtThe University of Maryland, Baltimore County (UMBC)
dc.relation.ispartofUMBC Center for Space Sciences and Technology (CSST) / Center for Research and Exploration in Space Sciences & Technology II (CRSST II)
dc.relation.ispartofUMBC Faculty Collection
dc.rightsThis work was written as part of one of the author's official duties as an Employee of the United States Government and is therefore a work of the United States Government. In accordance with 17 U.S.C. 105, no copyright protection is available for such works under U.S. Law.
dc.rightsPublic Domain
dc.rights.urihttps://creativecommons.org/publicdomain/mark/1.0/
dc.subjectAstrophysics - Earth and Planetary Astrophysics
dc.titleHigh-Speed Boulders and the Debris Field in DART Ejecta
dc.typeText
dcterms.creatorhttps://orcid.org/0000-0001-5764-7639

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