Abstract Small aromatic molecules, including functionalized derivatives of benzene, are known to be present throughout the different stages of star and planet formation. In particular, oxygen-bearing monosubstituted aromatics, likely including phenol, have been identified in the coma of comet 67P. This suggests that, earlier in the star and planet formation evolution, icy grains may act as both reservoirs and sites of functionalization for these small aromatics. We investigate the ice-phase reactivity of singlet oxygen atoms (O( 1 D)) with benzene, using ozone as a precursor that is readily photodissociated by relatively low energy. Our experiments show that O( 1 D) efficiently reacts with benzene, forming phenol, benzene oxide, and oxepine as the main products. Phenol formation is temperature-independent, consistent with a barrierless insertion mechanism. In contrast, the formation of benzene oxide/oxepine shows a slight temperature dependence, suggesting that additional reaction pathways involving either ground-state or excited-state oxygen atoms may contribute. In H 2 O and CO 2 ice matrices we find that dilution does not suppress the formation of phenol. We extrapolate an experimental upper limit for the benzene-to-phenol conversion fraction of 27%–44% during the lifetime of an interstellar cloud, assuming O( 1 D) production rates based on CO 2 ice abundances and a cosmic-ray-induced UV field. We compare these estimates with a new analysis of data from the comet 67P, where the C 6 H 6 O/C 6 H 6 ratio is 20% ± 6%. This value lies within our estimated range, suggesting that O( 1 D)-mediated chemistry is a viable pathway for producing oxygenated aromatics in cold astrophysical ices, potentially enriching icy planetesimals with phenol and other biorelevant compounds.
Piacentino et al. (Tue,) studied this question.