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The surface composition of Charon - Tentative identification of water iceThe Mar. 3, 1987, Charon occultation by Pluto was observed in the infrared at 1.5, 1.7, 2.0, and 2.35 micrometers. Subtraction of fluxes measured between second and third contacts from measurements made before and after the event has yielded individual spectral signatures for each body at these wavelengths. Charon's surface appears depleted in methane relative to Pluto. Constancy of flux at 2.0 micrometers throughout the event shows that Charon is effectively black at this wavelength, which is centered on a very strong water absorption band. Thus, the measurements suggest the existence of water ice on Pluto's moon.
Document ID
19880024368
Acquisition Source
Legacy CDMS
Document Type
Reprint (Version printed in journal)
Authors
Marcialis, Robert L.
(Arizona Univ. Tucson, AZ, United States)
Lebofsky, Larry A.
(Arizona, University Tucson, United States)
Rieke, George H.
(Arizona, University; Steward Observatory, Tucson, United States)
Date Acquired
August 13, 2013
Publication Date
September 11, 1987
Publication Information
Publication: Science
Volume: 237
ISSN: 0036-8075
Subject Category
Lunar And Planetary Exploration
Accession Number
88A11595
Funding Number(s)
CONTRACT_GRANT: NSG-7114
Distribution Limits
Public
Copyright
Other

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