Abstract The nuclei of comets and the small icy moons of the outer planets are thought to be the most primitive objects in the solar system. Because of their pristine nature, in-situ measurements of composition, temperature, and mechanical properties will be a powerful tool in realization of one of NASA's major objectives: determination of the Solar System's origins and evolution. Cryo penetrators are a new class of penetrator vehicle investigated intensively since 1985 for NASA's Comet Rendezvous/Asteroid Flyby (CRAF) mission. They are specifically optimized for penetration and operation in icy bodies at temperatures below 150 degrees K. The CRAF studies were directed at investigation of comet nuclei, but the same design should be applicable to the icy moons of the outer planets and, with appropriate delivery systems, (similar to those envisioned for NASA's MESUR mission) to the Martian polar caps. This paper describes the design of a cryopenetrator based on the CRAF Configuration and designed for in-situ measurements of a comet nucleus as part of the Comet Nucleus Penetrator (CNP) Discovery mission. The ROSETTA nucleus rendezvous mission recently selected by ESA is another potential cryo penetrator application.
[1]
E. Anders.
Origin, age, and composition of meteorites
,
1964
.
[2]
J. Lunine,et al.
Sublimation and reformation of icy grains in the primitive solar nebula
,
1991
.
[3]
G. Carle,et al.
Miniature triaxial metastable ionization detector for gas chromatographic trace analysis of extraterrestrial volatiles.
,
1984,
Analytical chemistry.
[4]
Richard D. Starr,et al.
Science applications of the Mars Observer gamma ray spectrometer
,
1992
.
[5]
S. Squyres,et al.
Temperatures within comet nuclei.
,
1985,
Journal of geophysical research.
[6]
A. Bar-Nun,et al.
Amorphous water ice and its ability to trap gases.
,
1987,
Physical review. B, Condensed matter.