Bl. Haas et Fs. Milos, SIMULATED RAREFIED ENTRY OF THE GALILEO PROBE INTO THE JOVIAN ATMOSPHERE, Journal of spacecraft and rockets, 32(3), 1995, pp. 398-403
Flowfield properties and aerodynamics are computed with a direct simul
ation Monte Carlo method in the rarefied flow regime during entry of t
he Galileo Probe into the atmosphere of Jupiter. The objective is to p
redict accurately the vehicle's drag coefficient, which is needed to a
ssess atmospheric properties from the onboard atmospheric structure ex
periment, where highly sensitive accelerometers will measure the drag
effects to within 10(-5) m/s(2) during the initial entry phase at high
altitudes. The corresponding flow rarefaction extends from the free-m
olecule limit to the near-continuum transition regime (Re-infinity < 1
000). Simulation results, employing a simple radiative equilibrium sur
face model, indicate that C-D varies from 2.1 at the free-molecule lim
it down to 1.6 at Re-infinity = 1000. Results compared very well to th
ose from ballistic-range experiments. Detailed material response of th
e carbon-phenolic heat shield was then coupled directly into the DSMC
code to account accurately for conductivity, heat capacity, and pyroly
sis, and the simulations were repeated. The predicted pyrolysis mass e
fflux was 8-14 times higher than the incident freestream mass flux and
had significant effects on the drag.