Mathematics – Logic
Scientific paper
Dec 2009
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2009agufm.p51e1175s&link_type=abstract
American Geophysical Union, Fall Meeting 2009, abstract #P51E-1175
Mathematics
Logic
[5422] Planetary Sciences: Solid Surface Planets / Ices, [5494] Planetary Sciences: Solid Surface Planets / Instruments And Techniques, [6221] Planetary Sciences: Solar System Objects / Europa, [6222] Planetary Sciences: Solar System Objects / Ganymede
Scientific paper
In the upcoming joint ESA/NASA mission two flagship spacecraft wills be launched to study the Jovian system. In the second phase of operation the spacecrafts will settle into orbits around Ganymede and Europa, respectively. Of primary interests are the characterization of the icy shells, the global surface composition and chemistry in order to understand geological evolution, confirm the presence of liquid water under the icy core and investigate the habitability of these interesting planetary objects. On their orbit around the moons, the spacecrafts will be bombarded by micron-sized particles originating from the surface. These dust particles are kicked-up to high altitudes by the continual micrometeoroid bombardment of the surface. This permanently present dust cloud enshrouding the moons has already been detected by the Galileo spacecraft. These particles are a direct link to the place of origin (surface) and their composition can be analyzed by existing instruments. The mass analysis is based on the time-of-flight mass analysis of the ions generated upon the impact of the dust on the instrument’s target surface. The high scientific value of this method was recently demonstrated by the analysis of particles originating from Enceladus’s plumes by the Cosmic Dust Analyzer onboard the Cassini spacecraft [Postberg et al., Nature 459, 1098, 2009]. This analyzing method is particularly sensitive to salts and other minerals as well as organic compounds embedded in the ice as the ionization of these is greatly enhanced. (Resent experiments showed that we are sensitive to organic compounds at least down to 0.001% mixing ratio). The small abundance of these elements are difficult to detect by other methods, yet they are considerable scientific significance as proof of interaction between the rocky core and the liquid water underneath the icy surface, for example. In this presentation we review capabilities of the existing instrument and the applicability of this method to Europa and Ganymede. The speed of a spacecraft orbiting either of the moons will be > 1 km/s, which is sufficient to get chemical information from a highly resolved impact ionization mass spectrum. Instruments far exceeding the sensitivity and mass resolution of CDA are now available and can greatly enhance the science return and answer many question of the next Jupiter mission.
Gruen Eberhard
Horanyi Mihaly
Kempf Sascha
Postberg Frank
Srama Ralf
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