Title of article :
A spectroscopic study of the surfaces of Saturnʹs large satellites: H2O ice, tholins, and minor constituents
Author/Authors :
Cruikshank، نويسنده , , Dale P. and Owen، نويسنده , , Tobias C. and Ore، نويسنده , , Cristina Dalle and Geballe، نويسنده , , Thomas R. and Roush، نويسنده , , Ted L. and de Bergh، نويسنده , , Catherine and Sandford، نويسنده , , Scott A. and Poulet، نويسنده , , Francois and Benedix، نويسنده , , Gretchen K. and Emery، نويسنده , , Joshua P.، نويسنده ,
Issue Information :
روزنامه با شماره پیاپی سال 2005
Pages :
16
From page :
268
To page :
283
Abstract :
We present spectra of Saturnʹs icy satellites Mimas, Enceladus, Tethys, Dione, Rhea, and Hyperion, 1.0–2.5 μm, with data extending to shorter (Mimas and Enceladus) and longer (Rhea and Dione) wavelengths for certain objects. The spectral resolution ( R = λ / Δ λ ) of the data shown here is in the range 800–1000, depending on the specific instrument and configuration used; this is higher than the resolution ( R = 225 at 3 μm) afforded by the Visual-Infrared Mapping Spectrometer on the Cassini spacecraft. All of the spectra are dominated by water ice absorption bands and no other features are clearly identified. Spectra of all of these satellites show the characteristic signature of hexagonal H2O ice at 1.65 μm. We model the leading hemisphere of Rhea in the wavelength range 0.3–3.6 μm with the Hapke and the Shkuratov radiative transfer codes and discuss the relative merits of the two approaches to fitting the spectrum. In calculations with both codes, the only components used are H2O ice, which is the dominant constituent, and a small amount of tholin (Ice Tholin II). Tholin in small quantities (few percent, depending on the mixing mechanism) appears to be an essential component to give the basic red color of the satellite in the region 0.3–1.0 μm. The quantity and mode of mixing of tholin that can produce the intense coloration of Rhea and other icy satellites has bearing on its likely presence in many other icy bodies of the outer Solar System, both of high and low geometric albedos. Using the modeling codes, we also establish detection limits for the ices of CO2 (a few weight percent, depending on particle size and mixing), CH4 (same), and NH4OH (0.5 weight percent) in our globally averaged spectra of Rheaʹs leading hemisphere. New laboratory spectral data for NH4OH are presented for the purpose of detection on icy bodies. These limits for CO2, CH4, and NH4OH on Rhea are also applicable to the other icy satellites for which spectra are presented here. The reflectance spectrum of Hyperion shows evidence for a broad, unidentified absorption band centered at 1.75 μm.
Keywords :
Infrared observations , ICES , satellites of Saturn , Spectroscopy , Surfacessatellite , organic chemistry
Journal title :
Icarus
Serial Year :
2005
Journal title :
Icarus
Record number :
2373475
Link To Document :
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