Production and evolution of carbonaceous material by ion irradiation in space.
We review recent experimental studies concerning the evolution, driven by ion irradiation, of carbonaceous material from frozen gas to a refractory molecular solid.  Under further irradiation the latter changes to a polymer-like material and ultimately to amorphous carbon.  Most of the results have been obtained by "in situ" and remote IR and Raman spectroscopy.  The results have been applied to demonstrate that molecular solids may be easily formed by irradiation of frozen mantles in dense interstellar clouds.  Polymer-like material and amorphous carbons may result by further irradiation of organic mantles on grains in the diffuse interstellar medium.  Those grains, during the aggregation to form extended bodies like comets (T-Tau phase of the Sun), are further modified.  These latter are also irradiated, after the comet formation, during their long stay in the Oort cloud.  In particular it has been suggested that comet may develop an ion-produced cometary organic crust that laboratory evidences show to be stable against temperature increases experienced during passages near the Sun.  The comparison between the Raman spectra of some IDP (Interplanetary Dust Particles) and the Raman spectra of some ion-produced amorphous carbons, is also discussed.
Strazzulla
G
G
Instituto di Astronomia, Università di Catania, Italy.
Baratta
G A
GA
Spinella
F
F
D001554:Benzene / Q000737:chemistry*; D002244:Carbon / Q000737:chemistry*; D019443:Cosmic Dust; D003359:Cosmic Radiation; D019418:Evolution, Chemical; D019419:Evolution, Planetary; D005118:Extraterrestrial Environment; D007053:Ice / Q000032:analysis*; D007477:Ions; D019110:Meteoroids; D017550:Spectroscopy, Fourier Transform Infrared; D013059:Spectrum Analysis, Raman
D019443:Cosmic Dust; D007053:Ice; D007477:Ions; D002244:Carbon; D001554:Benzene