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Carbon dioxide and sulfur dioxide on the surfaces of the Galilean satellites Ganymede and Callisto

Posted on:2002-09-18Degree:Ph.DType:Dissertation
University:University of HawaiiCandidate:Hibbits, Charles ArthurFull Text:PDF
GTID:1461390011991672Subject:Geology
Abstract/Summary:
The surfaces of Ganymede and Callisto are made mostly of water-ice and a spectrally bland non-ice material. Small amounts of other materials, including CO2 and SO2, have recently been discovered on the surfaces of the them [Carlson et al., 1996; McCord et al., 1998] as well as a very thin exosphere of CO2 on Callisto [Carlson, 1999]. These discoveries were made by the detection of absorption bands in infrared spectra obtained from the Near Infrared Mapping Spectrometer (NIMS) aboard the Galileo spacecraft over the last 5 years. Both the CO2 and SO2 on the surface appear to be contained in a less-volatile host material that keeps them stable when they would otherwise quickly escape into space. McCord et al. also showed that the distribution of CO2 and SO2 over the surfaces of Ganymede and Callisto are affected by the local geology and space environment.; One goal of this dissertation is to pin down the relationships between the surface geology and the distribution of these volatiles on Ganymede and Callisto. The other goals are to determine if all the CO2 and SO 2 are trapped in similar host materials, identify this host material, determine the origins of the CO2 and SO2, and determine what implications can be inferred from the distribution of CO2 and SO2. These are grand objectives to fulfill in a single dissertation and there have been many hurdles along the way, including a very complex and still not completely resolved calibration of the NIMS data. Additionally, the distribution of SO2 could only be mapped on Callisto because its band is too shallow to be observed in most places on Ganymede. Despite these limitations, I have been able to accomplish most of the goals. The CO 2 and SO2 on their surfaces, are indigenous to the satellites, and are contained in the darker, non-ice materials that are likely either oxyhydroxides or clay-like serpentines. It also appears that the subsurface of Ganymede may have lost much of its internal CO2 compared to Callisto.
Keywords/Search Tags:Ganymede, Callisto, Surfaces
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