Context. The formation of carbon dioxide in quiescent regions of molecular clouds has not yet been fully understood, even though CO2 is one of the most abundant species in interstellar ices. Aims: CO2 formation is studied via oxidation of CO molecules on cold surfaces under conditions close to those encountered in quiescent molecular clouds. Methods: Carbon monoxide and oxygen atoms are codeposited using two differentially pumped beam lines on two different surfaces (amorphous water ice or oxydized graphite) held at given temperatures between 10 and 60 K. The products are probed via mass spectroscopy by using the temperature-programmed desorption technique. Results: We show that the reaction CO + O can form carbon dioxide in solid phase with an efficiency that depends on the temperature of the surface. The activation barrier for the reaction, based on modelling results, is estimated to be in the range of 780-475 K/kb. Our model also allows us to distinguish the mechanisms (Eley Rideal or Langmuir-Hinshelwood) at play in different temperature regimes. Our results suggest that competition between CO2 formation via CO + O and other surface reactions of O is a key factor in the yields of CO2 obtained experimentally. Conclusions: CO2 can be formed by the CO + O reaction on cold surfaces via processes that mimic carbon dioxide formation in the interstellar medium. Astrophysically, the presence of CO2 in quiescent molecular clouds could be explained by the reaction CO + O occurring on interstellar dust grains.

CO2 formation on interstellar dust grains: a detailed study of the barrier of the CO + O channel

MANICO', Giulio;PIRRONELLO, Valerio;
2013-01-01

Abstract

Context. The formation of carbon dioxide in quiescent regions of molecular clouds has not yet been fully understood, even though CO2 is one of the most abundant species in interstellar ices. Aims: CO2 formation is studied via oxidation of CO molecules on cold surfaces under conditions close to those encountered in quiescent molecular clouds. Methods: Carbon monoxide and oxygen atoms are codeposited using two differentially pumped beam lines on two different surfaces (amorphous water ice or oxydized graphite) held at given temperatures between 10 and 60 K. The products are probed via mass spectroscopy by using the temperature-programmed desorption technique. Results: We show that the reaction CO + O can form carbon dioxide in solid phase with an efficiency that depends on the temperature of the surface. The activation barrier for the reaction, based on modelling results, is estimated to be in the range of 780-475 K/kb. Our model also allows us to distinguish the mechanisms (Eley Rideal or Langmuir-Hinshelwood) at play in different temperature regimes. Our results suggest that competition between CO2 formation via CO + O and other surface reactions of O is a key factor in the yields of CO2 obtained experimentally. Conclusions: CO2 can be formed by the CO + O reaction on cold surfaces via processes that mimic carbon dioxide formation in the interstellar medium. Astrophysically, the presence of CO2 in quiescent molecular clouds could be explained by the reaction CO + O occurring on interstellar dust grains.
File in questo prodotto:
File Dimensione Formato  
Minissale2013_A&A.pdf

solo gestori archivio

Tipologia: Versione Editoriale (PDF)
Licenza: NON PUBBLICO - Accesso privato/ristretto
Dimensione 768.12 kB
Formato Adobe PDF
768.12 kB Adobe PDF   Visualizza/Apri

I documenti in IRIS sono protetti da copyright e tutti i diritti sono riservati, salvo diversa indicazione.

Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/20.500.11769/16684
Citazioni
  • ???jsp.display-item.citation.pmc??? ND
  • Scopus 35
  • ???jsp.display-item.citation.isi??? 35
social impact