Binding Energies of Interstellar Relevant S-bearing Species on Water Ice Mantles: A Quantum Mechanical Investigation

• Published in: The Astrophysical journal 2022-10, Vol.938 (2), p.158
• Main Authors: Perrero, Jessica, Enrique-Romero, Joan, Ferrero, Stefano, Ceccarelli, Cecilia, Podio, Linda, Codella, Claudio, Rimola, Albert, Ugliengo, Piero
• Format: Article
• Language: English
• Subjects: Adsorption; Astrophysics; Binding energy; Binding sites; Computational methods; Crystal structure; Crystallinity; Dense interstellar clouds; Density functional theory; Interstellar dust; Interstellar dust processes; Interstellar gas; Interstellar matter; Interstellar medium; Interstellar molecules; Modelling; Planet formation; Protoplanetary disks; Quantum mechanics; Sciences of the Universe; Solid matter physics; Structural models; Sulfur; Surface chemistry; Surface ices; Vapor phases; Water ice
• ISSN: 0004-637X; 1538-4357
• DOI: 10.3847/1538-4357/ac9278

Binding energies (BEs) are one of the most important parameters for astrochemical modeling determining, because they govern whether a species stays in the gas phase or is frozen on the grain surfaces. It is currently known that, in the denser and colder regions of the interstellar medium, sulfur is severely depleted in the gas phase. It has been suggested that it may be locked into the grain icy mantles. However, which are the main sulfur carriers is still a matter of debate. This work aims to establish accurate BEs of 17 sulfur-containing species on two validated water ice structural models, the proton-ordered crystalline (010) surface and an amorphous water ice surface. We adopted density functional theory-based methods (the hybrid B3LYP-D3(BJ) and the hybrid meta-GGA M06-2X functionals) to predict structures and energetics of the adsorption complexes. London’s dispersion interactions are shown to be crucial for an accurate estimate of the BEs due to the presence of the high polarizable sulfur element. On the crystalline model, the adsorption is restricted to a very limited number of binding sites with single valued BEs, while on the amorphous model, several adsorption structures are predicted, giving a BE distribution for each species. With the exception of a few cases, both experimental and other computational data are in agreement with our calculated BE values. A final discussion on how useful the computed BEs are with respect to the snow lines of the same species in protoplanetary disks is provided.