Gas phase Elemental abundances in Molecular cloudS (GEMS): III. Unlocking the CS chemistry: the CS plus O reaction

dc.contributor.authorBulut, N.
dc.contributor.authorRoncero, O.
dc.contributor.authorAguado, A.
dc.contributor.authorLoison, J-C
dc.contributor.authorNavarro-Almaida, D.
dc.contributor.authorWakelam, V
dc.contributor.authorHacar, A.
dc.date.accessioned2026-08-12T18:06:38Z
dc.date.issued2021
dc.departmentFırat Üniversitesi
dc.description.abstractContext. Carbon monosulphide (CS) is among the most abundant gas-phase S-bearing molecules in cold dark molecular clouds. It is easily observable with several transitions in the millimeter wavelength range, and has been widely used as a tracer of the gas density in the interstellar medium in our Galaxy and external galaxies. However, chemical models fail to account for the observed CS abundances when assuming the cosmic value for the elemental abundance of sulfur. Aims. The CS+O -> CO + S reaction has been proposed as a relevant CS destruction mechanism at low temperatures, and could explain the discrepancy between models and observations. Its reaction rate has been experimentally measured at temperatures of 150-400 K, but the extrapolation to lower temperatures is doubtful. Our goal is to calculate the CS+O reaction rate at temperatures <150 K which are prevailing in the interstellar medium. Methods. We performed ab initio calculations to obtain the three lowest potential energy surfaces (PES) of the CS+O system. These PESs are used to study the reaction dynamics, using several methods (classical, quantum, and semiclassical) to eventually calculate the CS + O thermal reaction rates. In order to check the accuracy of our calculations, we compare the results of our theoretical calculations for T similar to 150-400 K with those obtained in the laboratory. Results. Our detailed theoretical study on the CS+O reaction, which is in agreement with the experimental data obtained at 150-400 K, demonstrates the reliability of our approach. After a careful analysis at lower temperatures, we find that the rate constant at 10 K is negligible, below 10(-15) cm(3) s(-1), which is consistent with the extrapolation of experimental data using the Arrhenius expression. Conclusions. We use the updated chemical network to model the sulfur chemistry in Taurus Molecular Cloud 1 (TMC 1) based on molecular abundances determined from Gas phase Elemental abundances in Molecular CloudS (GEMS) project observations. In our model, we take into account the expected decrease of the cosmic ray ionization rate, zeta(H2), along the cloud. The abundance of CS is still overestimated when assuming the cosmic value for the sulfur abundance.
dc.description.sponsorshipMICIU (Spain) [FIS2017-83473-C2, AYA2016-75066-C2-2-P, ESP2017-86582-C4-1-R, AYA2017-85111-P, PID2019-105552RB-C41, PID2019-106235GB-I00]; Marenostrum (BSC) under RES [ACCT-2019-3-0004, AECT-2020-1-0003]; European Union [639450]
dc.description.sponsorshipThe research leading to these results has received funding from MICIU (Spain) under grants FIS2017-83473-C2, AYA2016-75066-C2-2-P, ESP2017-86582-C4-1-R, AYA2017-85111-P, PID2019-105552RB-C41 and PID2019-106235GB-I00. N.B. acknowledges the computing facilities by TUBITAK-TRUBA, and O.R. and A.A. acknowledge computing time at Finisterre (CESGA) and Marenostrum (BSC) under RES computational grants ACCT-2019-3-0004 and AECT-2020-1-0003. SPTM acknowledges the European Union's Horizon 2020 research and innovation program for funding support under agreement No 639450 (PROMISE).
dc.identifier.doi10.1051/0004-6361/202039611
dc.identifier.issn0004-6361
dc.identifier.issn1432-0746
dc.identifier.orcid0000-0002-2569-1253
dc.identifier.orcid0000-0002-8499-7447
dc.identifier.orcid0000-0003-2407-1025
dc.identifier.orcid0000-0001-9819-1658
dc.identifier.orcid0000-0003-1837-3772
dc.identifier.orcid0000-0002-3972-1978
dc.identifier.orcid0000-0003-3248-3564
dc.identifier.scopus2-s2.0-85100389601
dc.identifier.scopusqualityQ1
dc.identifier.urihttps://doi.org/10.1051/0004-6361/202039611
dc.identifier.urihttps://hdl.handle.net/11508/62390
dc.identifier.volume646
dc.identifier.wosWOS:000616952000003
dc.identifier.wosqualityQ1
dc.indekslendigikaynakWeb of Science
dc.indekslendigikaynakScopus
dc.language.isoen
dc.publisherEdp Sciences S A
dc.relation.ispartofAstronomy & Astrophysics
dc.relation.publicationcategoryMakale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanı
dc.rightsinfo:eu-repo/semantics/openAccess
dc.snmzKA_WoS_20260511
dc.subjectastrochemistry
dc.subjectmolecular processes
dc.subjectISM: clouds
dc.subjectISM: molecules
dc.subjectISM: abundances
dc.titleGas phase Elemental abundances in Molecular cloudS (GEMS): III. Unlocking the CS chemistry: the CS plus O reaction
dc.typeArticle

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