The Si + SO2 collision and an extended network of neutral–neutral reactions between silicon and sulphur bearing species

Author:

Campanha Danilo R1,Mendoza Edgar2ORCID,Silva Mateus X1ORCID,Velloso Paulo F G1,Carvajal Miguel23ORCID,Wakelam Valentine4ORCID,Galvão Breno R L1ORCID

Affiliation:

1. Departamento de Química, Centro Federal de Educação Tecnológica de Minas Gerais , CEFET-MG Av. Amazonas 5253, 30421-169 Belo Horizonte, Minas Gerais, Brazil

2. Dpto. Ciencias Integradas y Centro de Estudios Avanzados en Fı́sica, Matemáticas y Computación, Unidad Asociada GIFMAN, CSIC-UHU, Universidad de Huelva , 21071 Huelva, Spain

3. Instituto Carlos I de Física Teórica y Computacional, Universidad de Huelva , Granada 18071, Spain

4. CNRS, Laboratoire d’astrophysique de Bordeaux, Univ. Bordeaux , B18N, allée Geoffroy Saint-Hilaire, F-33615 Pessac, France

Abstract

ABSTRACT The Si + SO2 reaction is investigated to verify its impact on the abundances of molecules with astrochemical interest, such as SiS, SiO, SO, and others. According to our results Si(3P) and SO2 react barrierlessly yielding only the monoxides SO and SiO as products. No favourable pathway has been found leading to other products, and this reaction should not contribute to SiS abundance. Furthermore, it is predicted that SiS is stable in collisions with O2, and that S(3P) + SiO2 and O(3P)+OSiS will also produce SO + SiO. Using these results and gathering further experimental and computational data from the literature, we provide an extended network of neutral–neutral reactions involving Si- and S-bearing molecules. The effects of these reactions were examined in a protostellar shock model, using the nautilus gas–grain code. This consisted in simulating the physicochemical conditions of a shocked gas evolving from (i) primeval cold core, (ii) the shock region itself, (iii) and finally the gas bulk conditions after the passage of the shock. Emphasizing on the cloud ages and including systematically these chemical reactions, we found that [SiS/H2] can be of the order of ∼10−8 in shocks that evolves from clouds of t = 1 × 106 yr, whose values are mostly affected by the SiS + O $\longrightarrow$SiO + S reaction. Perspectives on further models along with observations are discussed in the context of sources harbouring molecular outflows.

Funder

CAPES

CNPq

FAPEMIG

Horizon 2020

Junta de Andalucía

European Regional Development Fund

Ministerio de Ciencia, Innovación y Universidades

Publisher

Oxford University Press (OUP)

Subject

Space and Planetary Science,Astronomy and Astrophysics

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