The present spectroscopic study of the ultraviolet coronal emission in a po
lar hole, detected on 1996 April 6-9 with the Ultraviolet Coronagraph Spect
rometer aboard the Solar and Heliospheric Observatory spacecraft, identifie
s the interplume lanes and background coronal hole regions as the channels
in which the fast solar wind is preferentially accelerated. In interplume l
anes, at heliocentric distance 1.7 R., the corona expands at a rate between
105 and 150 km s(-1), that is, much faster than in plumes in which the out
flow velocity is between 0 and 65 km s(-1). The wind velocity is inferred f
rom the Doppler dimming of the O VI lambda lambda 1032, 1037 lines, within
a range of values, whose lower and upper limit corresponds to anisotropic a
nd isotropic velocity distribution of the oxygen coronal ions, respectively
.