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hal.structure.identifierDepartment of Physics, The Ohio State University
dc.contributor.authorGARROD, R. T.
hal.structure.identifierDepartment of Physics, The Ohio State University
hal.structure.identifierDepartment of Physics
hal.structure.identifierDepartment of Physics [OSU]
hal.structure.identifierObservatoire aquitain des sciences de l'univers [OASU]
hal.structure.identifierLaboratoire d'Astrophysique de Bordeaux [Pessac] [LAB]
hal.structure.identifierLaboratoire d'astrodynamique, d'astrophysique et d'aéronomie de bordeaux [L3AB]
dc.contributor.authorWAKELAM, Valentine
hal.structure.identifierDepartment of Physics
hal.structure.identifierDepartment of Physics [OSU]
hal.structure.identifierOhio State University [Columbus] [OSU]
hal.structure.identifierDepartments of Astronomy and Chemistry, The Ohio State University
hal.structure.identifierDepartments of Astronomy and Chemistry
hal.structure.identifierDepartment of Physics [OHIO STATE UNIVERSITY]
dc.contributor.authorHERBST, E.
dc.date.created2007-03-08
dc.date.issued2007
dc.identifier.issn0004-6361
dc.description.abstractEnAims: The gas-phase abundance of methanol in dark quiescent cores in the interstellar medium cannot be explained by gas-phase chemistry. In fact, the only possible synthesis of this species appears to be production on the surfaces of dust grains followed by desorption into the gas. Yet, evaporation is inefficient for heavy molecules such as methanol at the typical temperature of 10 K. It is necessary then to consider non-thermal mechanisms for desorption. But, if such mechanisms are considered for the production of methanol, they must be considered for all surface species. Methods: Our gas-grain network of reactions has been altered by the inclusion of a non-thermal desorption mechanism in which the exothermicity of surface addition reactions is utilized to break the bond between the product species and the surface. Our estimated rate for this process derives from a simple version of classical unimolecular rate theory with a variable parameter only loosely contrained by theoretical work. Results: Our results show that the chemistry of dark clouds is altered slightly at times up to 10^6 yr, mainly by the enhancement in the gas-phase abundances of hydrogen-rich species such as methanol that are formed on grain surfaces. At later times, however, there is a rather strong change. Instead of the continuing accretion of most gas-phase species onto dust particles, a steady-state is reached for both gas-phase and grain-surface species, with significant abundances for the former. Nevertheless, most of the carbon is contained in an undetermined assortment of heavy surface hydrocarbons. Conclusions: The desorption mechanism discussed here will be better constrained by observational data on pre-stellar cores, where a significant accretion of species such as CO has already occurred.
dc.language.isoen
dc.publisherEDP Sciences
dc.subject.enastrochemistry
dc.subject.enISM: abundances
dc.subject.enISM: molecules
dc.subject.enmolecular processes
dc.title.enNon-thermal desorption from interstellar dust grains via exothermic surface reactions
dc.typeArticle de revue
dc.identifier.doi10.1051/0004-6361:20066704
dc.subject.halPhysique [physics]/Astrophysique [astro-ph]/Cosmologie et astrophysique extra-galactique [astro-ph.CO]
dc.subject.halPlanète et Univers [physics]/Astrophysique [astro-ph]
dc.identifier.arxivastro-ph/0703188
bordeaux.journalAstronomy and Astrophysics - A&A
bordeaux.page1103-1115
bordeaux.volume467
bordeaux.issue3
bordeaux.peerReviewedoui
hal.identifierhal-00155973
hal.version1
hal.popularnon
hal.audienceNon spécifiée
hal.origin.linkhttps://hal.archives-ouvertes.fr//hal-00155973v1
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