期刊
FRONTIERS IN ASTRONOMY AND SPACE SCIENCES
卷 8, 期 -, 页码 -出版社
FRONTIERS MEDIA SA
DOI: 10.3389/fspas.2021.645243
关键词
interstellar; ices; binding energies; theoretical; amorphous; interstellar medium
资金
- CaPPA project (Chemical and Physical Properties of the Atmosphere) - French National Research Agency (ANR) through the PIA (Programme d'Investissement d'Avenir) [ANR-10-LABX-005]
- Region Hauts de France
- Ministere de l'Enseignement Superieur et de la Recherche (CPER Climibio)
- European Fund for Regional Economic Development
- GENCI-TGCC [2020-A0050801859]
This study investigated the adsorption of atoms and small molecules on hexagonal crystalline and amorphous ice clusters. The binding energies at different adsorption sites were explored, with most species forming physisorption with small binding energies, while carbon atoms formed unique molecules. The interaction energies obtained may help refine astrochemical models, and the methodology could be applied to other surfaces and larger adsorbates.
The adsorption of a series of atoms and small molecules and radicals (H, C, N, O, NH, OH, H2O, CH3, and NH3) on hexagonal crystalline and amorphous ice clusters were obtained via classical molecular dynamics and electronic structure methods. The geometry and binding energies were calculated using a QMHigh:QMLow hybrid method on model clusters. Several combination of basis sets, density functionals and semi-empirical methods were compared and tested against previous works. More accurate binding energies were also refined via single point Coupled Cluster calculations. Most species, except carbon atom, physisorb on the surface, leading to rather small binding energies. The carbon atom forms a COH2 molecule and in some cases leads to the formation of a COH-H3O+ complex. Amorphous ices are characterized by slightly stronger binding energies than the crystalline phase. A major result of this work is to also access the dispersion of the binding energies since a variety of adsorption sites is explored. The interaction energies thus obtained may serve to feed or refine astrochemical models. The present methodology could be easily extended to other types of surfaces and larger adsorbates.
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