We have solved a stationary Boltzmann transport equation to describe the io
nosphere of Titan in two simple cases. The first one deals with the satelli
te being outside the Kronian magnetosphere on the dayside of Saturn, which
happens under strong solar wind conditions. In that case, the main energy s
ource of ionization is the solar photons. We show the effect of the photoio
nization and the secondary ion production for a solar zenith angle of 45 de
grees. The electron production peaks at 25 electrons s(-1) cm(-3) around 10
00 km, We estimate the electron density from a comprehensive chemical code.
This electron density is then compared with the one computed from a simple
recombination model. Finally, we determine the intensity of nitrogen emiss
ions, which are compared to the Voyager 1 measurements.
In the second case, the satellite is inside Saturn's magnetosphere. We show
the effect of the ionization due to electron precipitation at night, above
the polar regions. The input electron flux is measured by the Voyager prob
es, gathered from several instruments on board. A simple Kappa distribution
is given to model a mean electron flux precipitating on Titan, We show tha
t the electron production ranges between 1 to 5 electrons s(-1) cm(-3) betw
een about 550 and 650 km. The electron production due to the photoionizatio
n above the pole is evaluated and compared to the effect of the kronian ele
ctron precipitation. (C) 1999 Academic Press.