We present a first attempt to model the profile of ion emission lines
in a cometary plasma tail with the aid of a 3D-MHD model of the comet-
solar wind interaction, and to compare the calculated line profiles to
high-resolution measurements of the H2O+ doubler at 6159 Angstrom in
comet 1P/Halley on January 6, 1986. The modelled line profiles are asy
mmetric and show a high velocity wing originating from fast ions in th
e outer parts of the tail along the line-of-sight. Comparison with the
measured profiles shows that such high-velocity wings are indeed obse
rved and are needed to fully approximate the observed profiles. We per
formed a quantitative analysis of the contribution of fast ions to the
ion flow to examine if they are really sufficient to explain the disc
repancy between measured H2O+ production rates and the rates expected
from photoionization of water. It is found that the combined effect of
fast ions and the limited field-of-view can indeed reduce the measure
d flux. However, the reduction seems not be sufficient to explain the
whole discrepancy.