Characterization of Temporarily Captured Minimoon 2020 CD₃ by Keck Time-resolved Spectrophotometry
- Creators
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Bolin, Bryce T.
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Fremling, Christoffer
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Holt, Timothy R.
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Hankins, Matthew J.
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Ahumada, Tomás
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Anand, Shreya
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Bhalerao, Varun B.
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Burdge, Kevin B.
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Copperwheat, Chris M.
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Coughlin, Michael
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Deshmukh, Kunal P.
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De, Kishalay
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Kasliwal, Mansi M.
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Morbidelli, Alessandro
- Purdum, Josiah N.
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Quimby, Robert
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Bodewits, Dennis
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Chang, Chan-Kao
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Ip, Wing-Huen
- Hsu, Chen-Yen
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Laher, Russ R.
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Lin, Zhong-Yi
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Lisse, Carey M.
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Masci, Frank J.
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Ngeow, Chow-Choong
- Tan, Hanjie
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Zhai, Chengxing
- Burruss, Rick S.
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Dekany, Richard
- Delacroix, Alexandre
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Duev, Dmitry A.
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Graham, Matthew
- Hale, David
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Kulkarni, Shrinivas R.
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Kupfer, Thomas
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Mahabal, Ashish
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Mróz, Przemyslaw J.
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Neill, James D.
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Riddle, Reed
- Rodriguez, Hector
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Smith, Roger M.
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Soumagnac, Maayane T.
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Walters, Richard
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Yan, Lin
- Zolkower, Jeffry
Abstract
We present time-resolved visible spectrophotometry of 2020 CD₃, the second known minimoon. The spectrophotometry was taken with the Keck I/Low Resolution Imaging Spectrometer between wavelengths 434 and 912 nm in the B, g, V, R, I, and RG850 filters as it was leaving the Earth–Moon system on 2020 March 23 UTC. The spectrum of 2020 CD₃ resembles V-type asteroids and some lunar rock samples with a 434–761 nm reddish slope of ~18%/100 nm (g–r = 0.62 ± 0.08 and r–i = 0.21 ± 0.06) with an absorption band at ~900 nm corresponding to i–z = −0.54 ± 0.10. Combining our measured H of 31.9 ± 0.1 with an albedo of 0.35 typical for V-type asteroids, we determine 2020 CD₃'s diameter to be ~0.9 ± 0.1 m, making it the first minimoon and one of the smallest asteroids to be spectrally studied. We use our time-series photometry to detect significant periodic light-curve variations with a period of ~573 s and amplitude of ~1. In addition, we extend the observational arc of 2020 CD₃ to 37 days, to 2020 March 23 UTC. From the improved orbital solution for 2020 CD₃, we estimate the likely duration of its capture to be ~2 yr and the nongravitational perturbation on its orbit due to radiation pressure with an area-to-mass ratio of (6.9 ± 2.4) × 10⁻⁴ m² kg⁻¹ implying a density of 2.3 ± 0.8 g cm⁻³, broadly compatible with other meter-scale asteroids and lunar rock. We searched for prediscovery detections of 2020 CD₃ in the Zwicky Transient Facility archive as far back as 2018 October but were unable to locate any positive detections.
Additional Information
© 2020 The American Astronomical Society. Received 2020 July 24; revised 2020 August 11; accepted 2020 August 12; published 2020 September 15. This work was supported by the GROWTH project, funded by the National Science Foundation under PIRE grant No. 1545949. Some of the data presented herein were obtained at the W. M. Keck Observatory, which is operated as a scientific partnership among the California Institute of Technology, the University of California, and the National Aeronautics and Space Administration. The Observatory was made possible by the generous financial support of the W. M. Keck Foundation. The authors wish to recognize and acknowledge the very significant cultural role and reverence that the summit of Maunakea has always had within the indigenous Hawaiian community. We are most fortunate to have the opportunity to conduct observations from this mountain. C.F. gratefully acknowledges support of his research by the Heising-Simons Foundation (No. 2018-0907). M.W.C. acknowledges support from the National Science Foundation with grant No. PHY-2010970. Based on observations obtained with the Samuel Oschin Telescope 48 inch and the 60 inch telescope at the Palomar Observatory as part of the Zwicky Transient Facility project. The ZTF is supported by the National Science Foundation under grant No. AST-1440341 and a collaboration including Caltech, IPAC, the Weizmann Institute for Science, the Oskar Klein Center at Stockholm University, the University of Maryland, the University of Washington, Deutsches Elektronen-Synchrotron and Humboldt University, Los Alamos National Laboratories, the TANGO Consortium of Taiwan, the University of Wisconsin at Milwaukee, and Lawrence Berkeley National Laboratories. Operations are conducted by COO, IPAC, and UW. This work has made use of data from the European Space Agency (ESA) mission Gaia (https://www.cosmos.esa.int/gaia), processed by the Gaia Data Processing and Analysis Consortium (DPAC; https://www.cosmos.esa.int/web/gaia/dpac/consortium). Funding for the DPAC has been provided by national institutions, in particular the institutions participating in the Gaia Multilateral Agreement. Facilities: Keck I Telescope - , P48 Oschin Schmidt telescope/Zwicky Transient Facility. -Attached Files
Published - Bolin_2020_ApJL_900_L45.pdf
Accepted Version - 2008.05384.pdf
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Additional details
- Eprint ID
- 105264
- Resolver ID
- CaltechAUTHORS:20200908-080643358
- NSF
- AST-1545949
- W. M. Keck Foundation
- Heising-Simons Foundation
- 2018-0907
- NSF
- PHY-2010970
- NSF
- AST-1440341
- ZTF partner institutions
- Gaia Multilateral Agreement
- Created
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2020-09-08Created from EPrint's datestamp field
- Updated
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2021-11-16Created from EPrint's last_modified field
- Caltech groups
- Astronomy Department, Infrared Processing and Analysis Center (IPAC), Zwicky Transient Facility, Division of Geological and Planetary Sciences (GPS)