The heavy ion counter (HIC) on the Galileo spacecraft consists of two low-e
nergy telescopes that were proof-test models of the telescopes used for the
cosmic ray subsystem (CRS) on Voyager. The telescopes on HIC were improved
to better withstand the intense radiation environment of the Jovian system
and to measure higher-energy particles with greater sensitivity. The simil
arity of these two instruments makes it natural to compare the data in an e
ffort to glean insight on the behavior of heavy ion fluxes at higher energi
es and how the inner Jovian magnetosphere has changed in the last 18 years.
Inside L = 6, the oxygen spectrum suggests a spectral break at similar to
7500 MeV/Gauss, corresponding to ions with gyroradii of similar to 1.5 R-Io
at L = 6. A comparison of the phase space densities show remarkable agreem
ent between the two time periods outside of the Io orbit, with differential
spectra consistent with gamma similar to -8 above similar to 6 MeV/nucleon
. Near Io Galileo observed a large density gradient not apparent in the Voy
ager data that may be due to local time asymmetries or a decrease in the ra
dial diffusion rate.