Diffusion and Clustering of Carbon Dioxide on non-porous Amorphous Solid Water
arXiv:1611.02182 · doi:10.3847/1538-4357/aa5f52
Abstract
Observations by ISO and Spitzer towards young stellar objects (YSOs) showed that CO segregates in the icy mantles covering dust grains. Thermal processing of ice mixture was proposed as responsible for the segregation. Although several laboratory studied thermally induced segregation, a satisfying quantification is still missing. We propose that the diffusion of CO along pores inside water ice is the key to quantify segregation. We combined Temperature Programmed Desorption (TPD) and Reflection Absorption InfraRed Spectroscopy (RAIRS) to study how CO molecules interact on a non-porous amorphous solid water (np-ASW) surface. We found that CO diffuses significantly on a np-ASW surface above 65~K and clusters are formed at well below one monolayer. A simple rate equation simulation finds that the diffusion energy barrier of CO on np-ASW is 215050 K, assuming a diffusion pre-exponential factor of 10 s. This energy should also apply to the diffusion of CO on wall of pores. The binding energy of CO from CO clusters and CO from HO ice have been found to be and ~K, respectively, assuming the same prefactor for desorption. CO-CO interaction is stronger than CO-HO interaction, in agreement with the experimental finding that CO does not wet np-ASW surface. For comparison, we carried out similar experiments with CO on np-ASW, and found that the CO-CO interaction is always weaker than CO-HO. As a result, CO wets np-ASW surface. This study should be of help to uncover the thermal history of CO on the icy mantles of dust grains.
8 pages, 11 figures, submitted to ApJ
References in corpus (2)
Cited by in corpus (5)
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