The icy Galilean satellites of Jupiter are subject to magnetospheric p
lasma ion bombardment, which induces chemical changes within the ice.
The possible detection of CO2 on the surface of Ganymede by the Galile
o spacecraft makes for a more complicated chemistry and increases the
number of chemical compounds that may then be present. We outline chem
ical schemes for the irradiation of pure and mixed ices H2O/CO2 and su
ggest species which observers may detect on Europa, Ganymede, and Call
isto, such as C3O2, H2CO3, H2O2, CO3, HO2, CO, H2CO, CH2CO, as well as
K2O, KOH, and SO3, from plasma implantation. Column abundances of com
pounds in the ice are calculated using a specified energy input and G
values (yield per 100 eV).