The Planetary Science Journal (Jan 2024)
The Unusual Brightness Phase Curve of (65803) Didymos
- P. H. Hasselmann,
- V. Della Corte,
- P. Pravec,
- S. Ieva,
- I. Gai,
- D. Perna,
- J. D. P. Deshapriya,
- E. Mazzotta-Epifani,
- E. Dotto,
- A. Zinzi,
- G. Poggiali,
- I. Bertini,
- A. Lucchetti,
- M. Pajola,
- J. Beccarelli,
- M. Dall’Ora,
- J.-Y. Li,
- S. L. Ivanovski,
- A. Rossi,
- J. R. Brucato,
- C. A. Thomas,
- O. Barnouin,
- J. M. Sunshine,
- A. S. Rivkin,
- M. Amoroso,
- A. Capannolo,
- S. Caporali,
- M. Ceresoli,
- G. Cremonese,
- R. T. Daly,
- G. Impresario,
- R. Lasagni-Manghi,
- M. Lavagna,
- D. Modenini,
- E. E. Palmer,
- P. Palumbo,
- S. Pirrotta,
- P. Tortora,
- M. Zannoni,
- G. Zanotti
Affiliations
- P. H. Hasselmann
- ORCiD
- INAF-Osservatorio Astronomico di Roma , Monte Porzio Catone, Italy ; [email protected]
- V. Della Corte
- INAF-Osservatorio Astronomico di Capodimonte , Naples, Italy
- P. Pravec
- ORCiD
- Astronomical Institute, Academy of Sciences of the Czech Republic , Ondřejov, Czech Republic
- S. Ieva
- ORCiD
- INAF-Osservatorio Astronomico di Roma , Monte Porzio Catone, Italy ; [email protected]
- I. Gai
- Alma Mater Studiorum—Universita di Bologna , Dipartimento di Ingegneria Industriale, Forlì, Italy
- D. Perna
- ORCiD
- INAF-Osservatorio Astronomico di Roma , Monte Porzio Catone, Italy ; [email protected]
- J. D. P. Deshapriya
- ORCiD
- INAF-Osservatorio Astronomico di Roma , Monte Porzio Catone, Italy ; [email protected]
- E. Mazzotta-Epifani
- ORCiD
- INAF-Osservatorio Astronomico di Roma , Monte Porzio Catone, Italy ; [email protected]
- E. Dotto
- ORCiD
- INAF-Osservatorio Astronomico di Roma , Monte Porzio Catone, Italy ; [email protected]
- A. Zinzi
- ORCiD
- Agenzia Spaziale Italiana , Via del Politecnico, 00133, Rome, Italy; Space Science Data Center , ASI, Rome, Italy
- G. Poggiali
- ORCiD
- INAF-Osservatorio Astrofisico di Arcetri , Florence, Italy; LESIA , Observatoire de Paris-Meudon, Meudon, Île-de-France, France
- I. Bertini
- ORCiD
- Università degli Studi di Napoli “Parthenope” , Naples, Italy
- A. Lucchetti
- ORCiD
- INAF-Osservatorio Astronomico di Padova , Padova, Italy
- M. Pajola
- ORCiD
- INAF-Osservatorio Astronomico di Padova , Padova, Italy
- J. Beccarelli
- INAF-Osservatorio Astronomico di Padova , Padova, Italy
- M. Dall’Ora
- ORCiD
- INAF-Osservatorio Astronomico di Capodimonte , Naples, Italy
- J.-Y. Li
- ORCiD
- Planetary Science Institute , Tucson, AZ, USA
- S. L. Ivanovski
- ORCiD
- INAF-Osservatorio Astronomico di Trieste , Trieste, Italy
- A. Rossi
- ORCiD
- IFAC-CNR , Sesto Fiorentino, Firenze, Italy
- J. R. Brucato
- ORCiD
- INAF-Osservatorio Astrofisico di Arcetri , Florence, Italy
- C. A. Thomas
- ORCiD
- Department of Physics and Astronomy, Northern Arizona University , Flagstaff, AZ, USA
- O. Barnouin
- ORCiD
- Johns Hopkins University Applied Physics Laboratory , Laurel, MD, USA
- J. M. Sunshine
- ORCiD
- University of Maryland , Department of Astronomy and Department of Geology, College Park, MD, USA
- A. S. Rivkin
- ORCiD
- University of Maryland , Department of Astronomy, MD, USA
- M. Amoroso
- Agenzia Spaziale Italiana , Via del Politecnico, 00133, Rome, Italy
- A. Capannolo
- ISAE-SUPAERO, Université de Toulouse , Toulouse, France; Politecnico di Milano , Dip. di Scienze e Tecnologie Aerospaziali, Milano, Italy
- S. Caporali
- INAF-Osservatorio Astrofisico di Arcetri , Florence, Italy
- M. Ceresoli
- Politecnico di Milano , Dip. di Scienze e Tecnologie Aerospaziali, Milano, Italy
- G. Cremonese
- INAF-Osservatorio Astronomico di Padova , Padova, Italy
- R. T. Daly
- ORCiD
- Johns Hopkins University Applied Physics Laboratory , Laurel, MD, USA
- G. Impresario
- Agenzia Spaziale Italiana , Via del Politecnico, 00133, Rome, Italy
- R. Lasagni-Manghi
- Alma Mater Studiorum—Universita di Bologna , Dipartimento di Ingegneria Industriale, Forlì, Italy
- M. Lavagna
- Politecnico di Milano , Dip. di Scienze e Tecnologie Aerospaziali, Milano, Italy
- D. Modenini
- Alma Mater Studiorum—Universita di Bologna , Dipartimento di Ingegneria Industriale, Forlì, Italy
- E. E. Palmer
- ORCiD
- Planetary Science Institute , Tucson, AZ, USA
- P. Palumbo
- Università degli Studi di Napoli “Parthenope” , Naples, Italy
- S. Pirrotta
- Agenzia Spaziale Italiana , Via del Politecnico, 00133, Rome, Italy
- P. Tortora
- Alma Mater Studiorum—Universita di Bologna , Dipartimento di Ingegneria Industriale, Forlì, Italy
- M. Zannoni
- Alma Mater Studiorum—Universita di Bologna , Dipartimento di Ingegneria Industriale, Forlì, Italy
- G. Zanotti
- Politecnico di Milano , Dip. di Scienze e Tecnologie Aerospaziali, Milano, Italy
- DOI
- https://doi.org/10.3847/PSJ/ad2add
- Journal volume & issue
-
Vol. 5,
no. 4
p. 91
Abstract
On 2022 September 26, NASA's Double Asteroid Redirection Test (DART) successfully hit Dimorphos, the smaller companion of the binary system formed with the asteroid (65803) Didymos. Both the binary system and the impact event were imaged by the Light Italian Cubesat for Imaging of Asteroids, detached from DART 15 days before the impact. Images from the onboard LUKE red, green, and blue camera together with ground-based observations enabled the reconstruction of Didymos's brightness phase curve, with phase angles ranging from 2.35° to 107.7°. The opposition effect regime was studied using the exponential-linear equation, the “Shevchenko” function and the linear-by-parts model while the IAU-official HG1G2 magnitude system was applied to the full phase curve. The opposition effect indicates an unusual asteroid surface for an S type, with characteristics similar to M-type asteroids. While the HG1G2 parameters from the full phase curve place Didymos well among asteroids of the taxonomic C complex. Didymos’s phase curve parameters when compared to near-Earth asteroids are very close to the Q type (1862) Apollo, indicating possible depletion of fine submicrometric grains through resurfacing. Didymos's geometric albedo (0.15 ± 0.01) is reported to be 30%–45% smaller than the average geometric albedo for near-Earth S types (0.26 ± 0.04). We propose that Didymos might be an LL ordinary chondrite analog containing albedo-suppressing, shock-darkened/impact melt minerals that have undergone resurfacing processes in the past. A comparison with meteorites indicates that, less likely, Didymos could also contain materials analog to carbon-bearing brecciated L3 ordinary chondrites.
Keywords