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The ISO-SWS instrument offering a large wavelength coverage and a resolution well adapted to the solid phase has changed our
knowledge of the physical-chemical properties of ices in space. The discovery of many new ice features was reported and the
comparison with dedicated laboratory experiments allowed the determination of more accurate abundances of major ice components.
The presence of CO2 ice has recently been confirmed with the SWS (Short Wavelength Spectrometer) as a dominant ice component of interstellar
grain mantles. The bending mode of CO2 ice shows a particular triple-peak structure which provides first evidence for extensive ice segregation in the line-of-sight
toward massive protostars. A comparison of interstellar and cometary ices using recent ISO data and ground-based measurements
has revealed important similarities but also indicated that comets contain, beside pristine interstellar material, admixtures
of processed material. The investigation of molecules in interstellar clouds is essential to reveal the link between dust
in the interstellar medium and in the Solar System.
This revised version was published online in June 2006 with corrections to the Cover Date. 相似文献
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Emmanuel Dartois 《Space Science Reviews》2005,119(1-4):293-310
The instruments on board the Infrared Space Observatory have for the first time allowed a complete low (PHOT, CVF) to medium
resolution (SWS) spectroscopic harvest, from 2.5 to 45 μm, of interstellar dust. Amongst the detected solids present in starless
molecular clouds surrounding recently born stellar and still embedded objects or products of the chemistry in some mass loss
envelopes, the so-called “ice mantles” are of specific interest. They represent an interface between the very refractory carbonaceous
and silicates materials that built the first grains with the rich chemistry taking place in the gas phase. Molecules condense,
react on ices, are subjected to UV and cosmic ray irradiation at low temperatures, participating efficiently to the evolution
toward more complex molecules, being in constant interaction in an ice layer. They also play an important role in the radiative
transfer of molecular clouds and strongly affect the gas phase chemistry. ISO results shed light on many other species than
H2O ice. The detection of these van der Waal's solids is mainly performed in absorption. Each ice feature observed by ISO spectrometer
is an important species, with abundance in the 10−4–10−7 range with respect to H2. Such high abundances represent a substantial reservoir of matter that, once released later on, replenishes the gas phase
and feeds the ladder of molecular complexity. Medium resolution spectroscopy also offers the opportunity to look at individual
line profiles of the ice features, and therefore to progressively reveal the interactions taking place in the mantles.
This article will give a view on selected results to avoid to overlap with the numerous reviews the reader is invited to consult
(e.g. van Dishoeck, in press; Gibb et al., 2004.).
Based on observations with ISO, an ESA project with instruments funded by ESA Member States (especially the PI countries:
France, Germany, The Netherlands, and the United Kingdom), and with the participation of ISAS and NASA. 相似文献
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A.A. Berezhnoy E.A. Kozlova M.P. Sinitsyn A.A. Shangaraev V.V. Shevchenko 《Advances in Space Research (includes Cospar's Information Bulletin, Space Research Today)》2012
Temperature regime at the LCROSS impact site is studied. All detected species in the Cabeus crater as well as CH4 and CO clathrate hydrates except H2, CO, and CH4 are stable against evaporation at the LCROSS impact site. CO and CH4 can be chemisorbed at the surface of the regolith particles and exist in the form of clathrate hydrates in the lunar cold traps. Flux rates of delivery of volatile species by asteroids, micrometeoroids, O-rich, C-rich, and low-speed comets into the permanently shadowed regions are estimated. Significant amounts of H2O, CO, H2, H2S, SO2, and CO2 can be impact-produced during collisions between asteroids and O-rich comets with the Moon while CH3OH, NH3 and complex organic species survive during low-speed comet impacts as products of disequilibrium processes. C-rich comets are main sources of CH4, and C2H4. 相似文献
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