The time evolution of the ring current population during the recovery
phase of a typical moderate magnetic storm is studied, using a newly d
eveloped kinetic model for H+, He+ and O+ ions which includes nonequat
orially mirroring particles. The bounce-averaged distribution function
is defined for variables that are accessible to direct measurement, a
nd some useful formulas for calculating the total energy and number de
nsity of the ring current are derived. The bounce-averaged kinetic equ
ation is solved, including losses due to charge exchange with neutral
hydrogen and Coulomb collisions with thermal plasma along ion drift pa
ths. Time-dependent magnetospheric electric fields and anisotropic ini
tial pitch angle distributions are considered. The generation of ion p
recipitating fluxes is addressed, a process that is still not complete
ly understood. It is shown that both the decrease of the distribution
function due to charge exchange losses and the buildup of a low-energy
population caused by Coulomb collisions proceed faster for particles
with smaller pitch angles. The maximum of the equatorial precipitating
fluxes occurs on the nightside during the early recovery phase and is
found to be of the order of 10(4) - 10(5) cm(-2)sr(-1)s(-1)keV(-1). T
he mechanisms considered in this paper indicate that magnetospheric co
nvection plays the predominant role in causing ion precipitation; Coul
omb scattering contributes significantly to the low-energy ion precipi
tation inside the plasmasphere.