2010
DOI: 10.1007/s11214-010-9665-8
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Chemical Composition of Icy Satellite Surfaces

Abstract: Much of our knowledge of planetary surface composition is derived from remote sensing over the ultraviolet through infrared wavelength ranges. Telescopic observations and, in the past few decades, spacecraft mission observations have led to the discovery of many surface materials, from rock-forming minerals to water ice to exotic volatiles and organic compounds. Identifying surface materials and mapping their distributions allows us to constrain interior processes such as cryovolcanism and aqueous geochemistry… Show more

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Cited by 65 publications
(53 citation statements)
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References 308 publications
(372 reference statements)
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“…Fig. 4 in Dalton et al 2010). Much less abundant (and difficult to observe) are the hydrated ions that we have synthesized in the experiments described here; nevertheless, they merit further investigation.…”
Section: Solar System Objectsmentioning
confidence: 73%
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“…Fig. 4 in Dalton et al 2010). Much less abundant (and difficult to observe) are the hydrated ions that we have synthesized in the experiments described here; nevertheless, they merit further investigation.…”
Section: Solar System Objectsmentioning
confidence: 73%
“…Dalton et al 2010). In particular, frozen SO 2 is the dominant species at the surface of Io, and it was also observed in cometary comae (see e.g.…”
Section: Introductionmentioning
confidence: 80%
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“…CH 4 band shifts to lower frequencies have also been observed in the spectrum of Pluto (Douté et al 1999), Quaoar (Licandro et al 2006a), and Makemake (Licandro et al 2006b). The coexistence of NH 3 and N 2 ices of solar system objects such as Enceladus or Charon is also thought to be very likely (Dalton 2010;Dalton et al 2010).…”
Section: Introductionmentioning
confidence: 99%
“…A&A 544, A30 (2012) Water ice is widely present, often as the most abundant chemical species, on the surfaces of the majority of the airless objects in the solar system. Many other molecules have also been identified or are suspected to be present (for a recent review see Dalton et al 2010). Concerning the molecules of interest to the present paper, O 2 has been observed on Europa, Callisto, and Ganymede (Spencer & Calvin 2002), possibly produced, along with other oxidants such as H 2 O 2 and O 3 , by radiolysis of water-ice and/or its mixtures with other species (e.g.…”
Section: Introductionmentioning
confidence: 76%