Characterization of thin film CO ice through the infrared combination mode
arXiv:1708.01600 · doi:10.1093/mnras/stx2412
Abstract
Carbon dioxide is abundant in ice mantles of dust grains; some is found in the pure crystalline form as inferred from the double peak splitting of the bending profile at about 650 cm. To study how CO segregates into the pure form from water-rich mixtures of ice mantles and how it then crystallizes, we used Reflection Absorption InfraRed Spectroscopy (RAIRS) to study the structural change of pure CO ice as a function of both ice thickness and temperature. We found that the combination mode absorption profile at 3708~cm provides an excellent probe to quantify the degree of crystallinity in CO ice. We also found that between 20 and 30~K, there is an ordering transition that we attribute to reorientation of CO molecules, while the diffusion of CO becomes significant at much higher temperatures. In the formation of pure crystalline CO in ISM ices, the rate limiting process is the diffusion/segregation of CO molecules in the ice instead of the phase transition from amorphous to crystalline after clusters/islands of CO are formed.
8 pages, 8 figures, submitted to MNRAS
References in corpus (3)
Cited by in corpus (6)
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