In this note a kinetic interaction process between a fast plasmoid ejected
by the Sun, which represents another form of CME, and the background solar
wind in the corona is discussed. We consider a system which consists of the
plasmoid ions moving faster than the solar wind. We are interested in the
time evolution of the ion distribution functions due to wave-particle inter
actions. Simulation results show that both perpendicular and parallel tempe
ratures of the solar wind ions increase when the relative velocity between
the plasmoid and the solar wind is sufficiently greater than the Alfven vel
ocity of the plasmoid ions. We suggest that this process is significant for
the heating and acceleration of the solar wind in the low-heliographic lat
itude regions near the Sun.