TY - JOUR
T1 - Molecular cloud chemistry and the importance of dielectronic recombination
AU - Bryans, P.
AU - Kreckel, H.
AU - Roueff, E.
AU - Wakelam, V.
AU - Savin, D. W.
PY - 2009
Y1 - 2009
N2 - Dielectronic recombination (DR) of singly charged ions is a reaction pathway that is commonly neglected in chemical models of molecular clouds. In this study we include state-of-the-art DR data for He+, C +, N+, O+, Na+, and Mg+ in chemical models used to simulate dense molecular clouds, protostars, and diffuse molecular clouds. We also update the radiative recombination (RR) rate coefficients for H+, He+, C+, N+, O+, Na+, and Mg+ to the current state-of-the-art values. The new RR data have little effect on the models. However, the inclusion of DR results in significant differences in gas-grain models of dense, cold molecular clouds for the evolution of a number of surface and gas-phase species. We find differences of a factor of 2 in the abundance for 74 of the 655 species at times of 104-106 yr in this model when we include DR. Of these 74 species, 16 have at least a factor of 10 difference in abundance. We find the largest differences for species formed on the surface of dust grains. These differences are due primarily to the addition of C+ DR, which increases the neutral C abundance, thereby enhancing the accretion of C onto dust. These results may be important for the warm-up phase of molecular clouds when surface species are desorbed into the gas phase. We also note that no reliable state-of-the-art RR or DR data exist for Si +, P+, S+, Cl+, and Fe+. Modern calculations for these ions are needed to better constrain molecular cloud models.
AB - Dielectronic recombination (DR) of singly charged ions is a reaction pathway that is commonly neglected in chemical models of molecular clouds. In this study we include state-of-the-art DR data for He+, C +, N+, O+, Na+, and Mg+ in chemical models used to simulate dense molecular clouds, protostars, and diffuse molecular clouds. We also update the radiative recombination (RR) rate coefficients for H+, He+, C+, N+, O+, Na+, and Mg+ to the current state-of-the-art values. The new RR data have little effect on the models. However, the inclusion of DR results in significant differences in gas-grain models of dense, cold molecular clouds for the evolution of a number of surface and gas-phase species. We find differences of a factor of 2 in the abundance for 74 of the 655 species at times of 104-106 yr in this model when we include DR. Of these 74 species, 16 have at least a factor of 10 difference in abundance. We find the largest differences for species formed on the surface of dust grains. These differences are due primarily to the addition of C+ DR, which increases the neutral C abundance, thereby enhancing the accretion of C onto dust. These results may be important for the warm-up phase of molecular clouds when surface species are desorbed into the gas phase. We also note that no reliable state-of-the-art RR or DR data exist for Si +, P+, S+, Cl+, and Fe+. Modern calculations for these ions are needed to better constrain molecular cloud models.
KW - Astrochemistry
KW - Atomic data
KW - Atomic processes
KW - Dust, extinction
KW - ISM: atoms
KW - ISM: molecules
UR - https://www.scopus.com/pages/publications/75149132204
U2 - 10.1088/0004-637X/694/1/286
DO - 10.1088/0004-637X/694/1/286
M3 - Article
AN - SCOPUS:75149132204
SN - 0004-637X
VL - 694
SP - 286
EP - 293
JO - Astrophysical Journal
JF - Astrophysical Journal
IS - 1
ER -