Carbon accretion and desorption by interstellar polycyclic aromatic hydrocarbons

Abstract

Two key questions of the chemistry of Polycyclic Aromatic Hydrocarbons (PAHs) in the interstellar medium (ISM) are addressed: i) the way carbon is returned from PAHs to the interstellar gas after the very efficient accretion of C+ ions onto PAHs; ii) the PAH contribution to the high abundance of small carbon molecules observed in UV-irradiated regions. They are addressed based on the structure and stability of the various isomers of the complexes formed by PAHs and their cations with atomic carbon. Carbon complexes with coronene are studied by B3LYP/6-311+G**) calculations, in order to determine the behaviour of C+ and C complexes with larger pericondensed interstellar PAHs, which are thought to be dominant in the ISM. The most stable forms of [C-coronene]+ cation include 7C and 4C rings, C+ insertion into a CH bond, and a 5C ring with a short exocyclic cumulene chain, and similarly for neutral [C-coronene]. The subsequent evolution of similar complexes with pericondensed PAHs, in diffuse clouds, is discussed under the action of interstellar UV photons and H atoms, as a function of the PAH size. Despite the complexity of such a processing, it seems probable that, for small PAHs, these complexes efficiently lose a C2H2 molecule from repeated photodissociations. However, this conclusion needs to be confirmed by the identification of reaction paths and the computation of activation energies. The case of the evolution of larger [C-PAH] complexes is less clear. The processing may explain the observed balance between C+ and PAHs, at least in the diffuse ISM. The formation of C2H2 from PAH catalysis is a key input for the chemistry of small carbon molecules in diffuse clouds. C+ accretion might frequently form stable PAHs that contain a peripheral pentagonal ring and form a significant fraction of interstellar PAHs.