Variations in color and reflectance on the surface of asteroid (101955) Bennu

D. N. DellaGiustina(Planetary Science Institute), K. N. Burke(Planetary Science Institute), K. J. Walsh(Southwest Research Institute), Peter H. Smith(Planetary Science Institute), D. R. Golish(Planetary Science Institute), E. B. Bierhaus(Lockheed Martin (United States)), Ronald‐Louis Ballouz(Planetary Science Institute), T. L. Becker(Planetary Science Institute), H. Campins(University of Central Florida), Eri Tatsumi(Universidad de La Laguna), Koki Yumoto, Seiji Sugita, J. D. P. Deshapriya(Centre National de la Recherche Scientifique), E. A. Cloutis(University of Winnipeg), B. E. Clark(Ithaca College), Amanda Hendrix(Planetary Science Institute), Antara Sen(Ithaca College), M. Al Asad(University of British Columbia), M. G. Daly(York University), D. M. Applin(University of Winnipeg), Chrysa Avdellidou(Centre National de la Recherche Scientifique), M. A. Barucci(Centre National de la Recherche Scientifique), K. J. Becker(Planetary Science Institute), C. A. Bennett(Planetary Science Institute), W. F. Bottke(Southwest Research Institute), J. Brodbeck(Planetary Science Institute), H. C. Connolly(Rowan University), Marco Delbò(Centre National de la Recherche Scientifique), J. de León(Universidad de La Laguna), C. Drouet d’Aubigny(Planetary Science Institute), K. L. Edmundson(Planetary Science Institute), S. Fornasier(Centre National de la Recherche Scientifique), V. E. Hamilton(Southwest Research Institute), P. H. Hasselmann(Centre National de la Recherche Scientifique), C. W. Hergenrother(Planetary Science Institute), E. S. Howell(Planetary Science Institute), E. R. Jawin(Smithsonian Institution), H. H. Kaplan(Goddard Space Flight Center), L. Le Corre(Planetary Science Institute), L. F. Lim(Smithsonian Institution), Jian‐Yang Li(Planetary Science Institute), Patrick Michel(Centre National de la Recherche Scientifique), J. L. Molaro(Planetary Science Institute), M. C. Nolan(Planetary Science Institute), J. O. Nolau(Lockheed Martin (United States)), M. Pajola(Osservatorio Astronomico di Padova), Alexis Parkinson(University of Winnipeg), Marcel Popescu(Universidad de La Laguna), N. A. Porter(Planetary Science Institute), B. Rizk(Planetary Science Institute), J. L. Rizos(Universidad de La Laguna), A. J. Ryan(Planetary Science Institute), B. Rozitis(The Open University), N. Shultz(Planetary Science Institute), Amy Simon(Goddard Space Flight Center), D. Trang(University of Hawaiʻi at Mānoa), Robin B. Van Auken(Planetary Science Institute), C. W. V. Wolner(Planetary Science Institute), D. S. Lauretta(Planetary Science Institute)
Science
October 8, 2020
Cited by 137Open Access
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Abstract

The complex history of Bennu's surface The near-Earth asteroid (101955) Bennu is a carbon-rich body with a rubble pile structure, formed from debris ejected by an impact on a larger parent asteroid. The Origins, Spectral Interpretation, Resource Identification, Security, Regolith Explorer (OSIRIS-REx) spacecraft is designed to collect a sample of Bennu's surface and return it to Earth. After arriving at Bennu, OSIRIS-REx performed a detailed survey of the asteroid and reconnaissance of potential sites for sample collection. Three papers present results from those mission phases. DellaGiustina et al. mapped the optical color and albedo of Bennu's surface and established how they relate to boulders and impact craters, finding complex evolution caused by space weathering processes. Simon et al. analyzed near-infrared spectra, finding evidence for organic and carbonate materials that are widely distributed across the surface but are most concentrated on individual boulders. Kaplan et al. examined more detailed data collected on the primary sample site, called Nightingale. They identified bright veins with a distinct infrared spectrum in some boulders, which they interpreted as being carbonates formed by aqueous alteration on the parent asteroid. Together, these results constrain Bennu's evolution and provide context for the sample collected in October 2020. Science , this issue p. eabc3660 , p. eabc3522 , p. eabc3557


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