UV photodesorption of interstellar CO ice analogues: from subsurface excitation to surface desorption.
Carbon monoxide is after H(2) the most abundant molecule identified in the interstellar medium (ISM), and is used as a major tracer for the gas phase physical conditions. Accreted at the surface of water-rich icy grains, CO is considered to be the starting point of a complex organic--presumably prebiotic--chemistry. Non-thermal desorption processes, and especially photodesorption by UV photons, are seen as the main cause that drives the gas-to-ice CO balance in the colder parts of the ISM. The process is known to be efficient and wavelength-dependent, but, the underlying mechanism and the physical-chemical parameters governing the photodesorption are still largely unknown. Using monochromatized photons from a synchrotron beamline, we reveal that the molecular mechanism responsible for CO photoejection is an indirect, (sub)surface-located process. The local environment of the molecules plays a key role in the photodesorption efficiency, and is quenched by at least an order of magnitude for CO interacting with a water ice surface.
UPMC Univ. Paris 6, Laboratoire de Physique Moléculaire pour l'Atmosphère et l'Astrophysique-CNRS UMR 7092, F-75252 Paris, France. mathieu.bertin@upmc.fr
Mathieu
M
Bertin
Edith C
EC
Fayolle
Claire
C
Romanzin
Karin I
KI
Öberg
Xavier
X
Michaut
Audrey
A
Moudens
Laurent
L
Philippe
Pascal
P
Jeseck
Harold
H
Linnartz
Jean-Hugues
JH
Fillion