The evolution of the newly created, picked-up cometary ion velocity di
stribution in the inner coma of comet Halley is studied. Calculations
are carried out for subsolar distances ranging from just inside the bo
w shock (almost-equal-to 350,000 km for comet P/Halley) to a cometocen
tric distance of about 9400 km which is a few thousand kilometers outs
ide of the diamagnetic cavity boundary (or contact surface). The effec
ts of energy diffusion, Coulomb collisons, charge transfer collisions,
dissociative recombination, and ion-neutral polarization interactions
have been included in these numerical calculations. Our results indic
ate that the ion distribution function retains its shell-like nature f
or radial distances greater than about 15,000 km, although charge tran
sfer collisions and wave-particle interactions tend to cool and thicke
n the shell, respectively. Our results also indicate that collisional
processes such as ion-neutral polarization and Coulomb collisions ther
malize the ion distribution function for distances inside about 15,000
km. We found that almost complete thermalization of a low-energy core
of the distribution occurs at a distance of 1-2 x 10(4) km. The exist
ence of a high-energy tail of the ion distribution in this inner regio
n is also discussed.