6,345 research outputs found
Cosmic-ray induced diffusion in interstellar ices
Cosmic rays are able to heat interstellar dust grains. This may enhance
molecule mobility in icy mantles that have accumulated on the grains in dark
cloud cores. A three-phase astrochemical model was used to investigate the
molecule mobility in interstellar ices. Specifically, diffusion through pores
in ice between the subsurface mantle and outer surface, assisted by whole-grain
heating, was considered. It was found that the pores can serve as an efficient
transport route for light species. The diffusion of chemical radicals from the
mantle to the outer surface are most effective. These species accumulate in the
mantle because of photodissociation by the cosmic-ray induced photons. The
faster diffusion of hydrogen within the warm ice enhances the hydrogenation of
radicals on pore surfaces. The overall result of the whole grain
heating-induced radial diffusion in ice are higher abundances of the ice
species whose synthesis involve light radicals. Examples of stable species
synthesized this way include the complex organic molecules, OCS, H2O2 and
cyanoplyynes
The Effect of an Inert Solid Reservoir on Molecular Abundances in Dense Interstellar Clouds
The question, what is the role of freeze-out of chemical species in
determining the molecular abundances in the interstellar gas is a matter of
debate. We investigate a theoretical case of a dense interstellar molecular
cloud core by time-dependent modelling of chemical kinetics, where grain
surface reactions deliberately are not included. That means, the gas-phase and
solid-phase abundances are influenced by gas reactions, accretion on grains,
and desorption, only. We compare the results to a reference model, where no
accretion occurs and only gas-phase reactions are included. We can trace that
the purely physical processes of molecule accretion and desorption have major
chemical consequences on the gas-phase chemistry. The main effect of
introduction of the gas-grain interaction is long-term molecule abundance
changes that come nowhere near an equilibrium in during the typical lifetime of
a prestellar core.Comment: 8 pages, 6 figures, 1 table. Material initially presented in
conference BAASP 2012 at Ventspils University College, May 201
Modeling the processing of interstellar ices by energetic particles
Context. Interstellar ice is the main form of metal species in dark molecular
clouds. Experiments and observations have shown that the ice is significantly
processed after the freeze-out of molecules onto grains. The processing is
caused by cosmic-ray particles and cosmic-ray-induced UV photons. These
transformations are included in current astrochemical models only to a very
limited degree. Aims. We aim to establish a model of the "cold" chemistry in
interstellar ices and to evaluate its general impact on the composition of
interstellar ices. Methods. The ice was treated as consisting of two layers -
the surface and the mantle (or subsurface) layer. Subsurface chemical processes
are described with photodissociation of ice species and binary reactions on the
surfaces of cavities inside the mantle. Hydrogen atoms and molecules can
diffuse between the layers. We also included deuterium chemistry. Results. The
modeling results show that the content of chemically bound H is reduced in
subsurface molecules by about 30 % on average. This promotes the formation of
more hydrogen-poor species in the ice. The enrichment of ice molecules with
deuterium is significantly reduced by the subsurface processes. On average, it
follows the gas-phase atomic D-to-H abundance ratio, with a delay. The delay
produced by the model is on the order of several Myr. Conclusions. The
processing of ice may place new constraints on the production of deuterated
species on grains. In a mantle with a two-layer structure the upper layer (CO)
should be processed substantially more intensively than the lower layer (H2O).
Chemical explosions in interstellar ice might not be an important process. They
destroy the structure of the mantle, which forms over long timescales. Besides,
ices may lack the high radical content needed for the explosions.Comment: 13 pages, 9 figures, 3 tables, 94 reference
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