THE EFFECT OF HEAVY COSMIC-RAY IONS ON SILICATE GRAINS IN THE INTERSTELLAR DUST

被引:22
作者
Szenes, G. [1 ]
Kovacs, V. K. [2 ]
Pecz, B. [2 ]
Skuratov, V. [3 ]
机构
[1] Eotvos Lorand Univ, Dept Mat Phys, H-1518 Budapest, Hungary
[2] Res Inst Tech Phys & Mat Sci, H-1525 Budapest, Hungary
[3] Joint Inst Nucl Res, Flerov Lab Nucl React, Dubna 141980, Russia
关键词
cosmic rays; dust; extinction; IRRADIATION-INDUCED AMORPHIZATION; LATENT TRACK FORMATION; MAGNETIC INSULATORS; SPECTROSCOPY; OLIVINE; DAMAGE; SPIKE;
D O I
10.1088/0004-637X/708/1/288
中图分类号
P1 [天文学];
学科分类号
0704 ;
摘要
Electronmicroscopic samples of crystalline Mg(2)SiO(4) forsterite were irradiated by energetic Ar, Fe, Kr, and Xe ions at room temperature. Tracks with a mean radius R(e) = 1.36 nm were observed after irradiation by 56 MeV Fe ions, while no tracks were induced by a 48 MeV Ar beam. Amorphization of forsterite grains by cosmic-ray (CR) Fe ions are discussed, including the effects of low temperature, ion velocity, and ion-induced crystallization. CR Fe ions induce amorphous tracks in crystalline forsterite only in the range 40-140 MeV, and the period of time for complete amorphization is tau(cr) approximate to 13,400 Myr. Our estimate is tau(cr) approximate to 1300 Myr for enstatite. Thus, heavy CR particles do not reduce the crystallinity of silicate grains within a reasonable time, as supposed previously. However, energetic ions can induce crystallization in amorphous solids, and this may be partially or fully responsible for the estimated 0.2% crystallinity of silicates in the interstellar medium.
引用
收藏
页码:288 / 292
页数:5
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