Significant gas-phase chemistry occurs in the comae of bright comets,
as is demonstrated here for the case of Comet Hale-Bopp. The abundance
ratio of the two isomers, hydrogen cyanide and hydrogen isocyanide, i
s shown to vary with heliocentric distance in a way that is consistent
with production of HNC by ion-molecule chemistry initiated by the pho
toionization of water. Likewise, the first maps of emission from HCOshow an abundance and an extended distribution that are consistent wit
h the same chemical model.