Cometary analogue material - Types, tests, and results

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Comet Nuclei, Mineralogy, Mission Planning, Regolith, Space Environment Simulation, Space Missions, Astronomical Models, Compression Tests, Microstructure, Penetration, Petrography, Thermal Conductivity

Scientific paper

The paper reviews a geological model of the regolith of cometary nuclei and the current status of a premission test program with cometary analog material with regard to the Rosetta Comet Sample Return Mission. Cometary analog material was prepared from four major end-member components and their mixtures using natural and synthetic materials. Results of penetration tests show that the force required to pierce a teflon rod into porous snow (H2O/CO2)-olivine-montmorillonite mixtures with layers of variable coherence varied from 0.15 to 5 MPa (at about 100 K). Results of compression tests indicate that the compressive strength of snow (H2O)-olivine-montmorillonite-kaolinite-tuff mixtures (0.5 and 0.8 Mg/cu cm) increased from 1.5 to 7.5 MN/sq m if temperatures were decreased from 253 to 123 K. A technique was developed to prepare polished sections and thin sections of snow-dust mixtures. It makes it possible to quantify the microtexture of the test samples by stereometric analysis and to monitor their properties induced by sublimation, compression, and drilling tests.

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