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Theoretical Distribution of the Ammonia Binding Energy at Interstellar Icy Grains: A New Computational Framework
Author(s) -
Lorenzo Tinacci,
Aurèle Germain,
Stefano Pantaleone,
Stefano Ferrero,
C. Ceccarelli,
Piero Ugliengo
Publication year - 2022
Publication title -
acs earth and space chemistry
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.876
H-Index - 19
ISSN - 2472-3452
DOI - 10.1021/acsearthspacechem.2c00040
Subject(s) - interstellar medium , interstellar ice , molecule , astrochemistry , chemical physics , amorphous solid , adsorption , oniom , binding energy , physics , desorption , molecular dynamics , astrophysics , materials science , chemistry , computational chemistry , atomic physics , crystallography , galaxy , quantum mechanics
The binding energies (BE) of molecules on the interstellar grains are crucial in the chemical evolution of the interstellar medium (ISM). Both temperature-programmed desorption (TPD) laboratory experiments and quantum chemistry computations have often provided, so far, only single values of the BE for each molecule. This is a severe limitation, as the ices enveloping the grain mantles are structurally amorphous, giving rise to a manifold of possible adsorption sites, each with different BEs. However, the amorphous ice nature prevents the knowledge of structural details, hindering the development of a common accepted atomistic icy model. In this work, we propose a computational framework that closely mimics the formation of the interstellar grain mantle through a water by water accretion. On that grain, an unbiased random (but well reproducible) positioning of the studied molecule is then carried out. Here we present the test case of NH 3 , a ubiquitous species in the molecular ISM. We provide the BE distribution computed by a hierarchy approach, using the semiempirical xTB-GFN2 as a low-level method to describe the whole icy cluster in combination with the B97D3 DFT functional as a high-level method on the local zone of the NH 3 interaction. The final ZPE-corrected BE is computed at the ONIOM(DLPNO-CCSD(T)//B97D3:xTB-GFN2) level, ensuring the best cost/accuracy ratio. The main peak of the predicted NH 3 BE distribution is in agreement with experimental TPD and computed data in the literature. A second broad peak at very low BE values is also present, which has never been detected before. It may provide the solution to a longstanding puzzle about the presence of gaseous NH 3 also observed in cold ISM objects.

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