Using data from the MASS high-resolution solar wind spectrometer on the WIN
D spacecraft, six enhanced He-3(2+)/He-4(2+) periods were identified from J
anuary 1995 to May 1998. The ratios observed in these events are four to te
n times higher than previously reported average solar wind values. All enha
nced He-3(2+) periods were associated with the passage of CME-ejecta. The o
bserved time periods were either within but towards the end of the CME-asso
ciated magnetic clouds or trailing the magnetic cloud by about 24 hours. Al
l the enhanced He-3(2+) periods have a mixture of low (cold) iron charge st
ates along with high (hot) oxygen charge states. The unusual charge state c
omposition of these enhanced He-3(2+) events suggests the plasma came from
a relatively cold and dense solar region, or from a rapidly expanding plasm
a parcel in the corona. We suggest that the enhanced He-3(2+) plasma origin
ated from the prominence core embedded within the CME.