The two main, low frequency radio components discovered at Neptune by
the Planetary Radio Astronomy experiment carried aboard Voyager 2 have
a well defined periodicity at about 16.1 hour. By analyzing all the a
vailable data, i.e. about 60 days around the closest approach for the
''Burst'' component and 15 days for the ''Smooth'' component, we deter
mine, for each component, die best estimate of the radio period. We co
nclude that the two estimates are not statistically different. While t
he two kinds of radio emissions have very different characteristics (i
n particular their frequency ranges and beaming properties), and proba
bly correspond to different emission processes, their modulation is ve
ry likely due to the rotation of the planetary magnetic field tied to
the core of the planet, as it has already been assumed for the other g
iant planets. The deduced estimate of the sidereal rotation period of
Neptune is 16.108 +/- 0.006 (or 16h06.5m +/- 00.4m).