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Published September 2013 | public
Journal Article

Near-infrared spectra of the uranian ring system

Abstract

We present the first high-resolution near-infrared (1.18–2.38 μm) spectrum of the rings of Uranus, as observed with adaptive optics on the W.M. Keck II telescope in August 2010. We derive ring equivalent widths, as well as ring and particle reflectivities for the ∊ ring and ringlet groups based on H- and K-band data. We find the rings to be gray, indicating that they are dominated by large particles rather than dust, and we find no evidence for water ice. We present a reflectivity spectrum for the ∊ ring alone, which we also find to be consistent with a flat spectrum. We derive H-band ring particle reflectivities of 0.022 ± 0.010, 0.051 ± 0.009 0.042 ± 0.012, and 0.043 ± 0.001 and K-band ring particle reflectivities of 0.016 ± 0.010, 0.034 ± 0.012, 0.047 ± 0.008 and 0.041 ± 0.002 for the 456, αβ, ηγδ, and ∊ ring groups. Previous observations have found ring particle reflectivities in the 0.033–0.044 range (de Pater, I., Gibbard, S., Macintosh, B.A., Roe, H.G. [2002]. Icarus 160, 359–374; Gibbard, S.G., de Pater, I., Hammel, H.B. [2005]. Icarus 174, 253–262), and are generally consistent with our results.

Additional Information

© 2013 Published by Elsevier. Received 25 September 2012, Revised 5 July 2013, Accepted 10 July 2013, Available online 22 July 2013. The authors thank Dr. Phil Nicholson and Dr. Erich Karkoschka for their careful reviews and valuable input regarding ring particle reflectivities in particular. The near-infrared data were obtained with the W.M. Keck Observatory, which is operated by 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 extend special thanks to those of Hawaiian ancestry on whose sacred mountain we are privileged to be guests. Without their generous hospitality, none of the observations presented would have been possible. This research has also made use of the SIMBAD database, operated at CDS, Strasbourg, France. This research was supported by NASA's Planetary Astronomy Program under Grant NNX07AK70G to the University of California, Berkeley.

Additional details

Created:
August 22, 2023
Modified:
October 20, 2023