Rn. Gupta et al., ASSESSMENT OF THERMOCHEMICAL NONEQUILIBRIUM AND SLIP EFFECTS FOR ORBITAL REENTRY EXPERIMENT, Journal of thermophysics and heat transfer, 11(4), 1997, pp. 562-569
Results are provided from a viscous shock layer (VSL) analysis of the
re-entry flowfield around the forebody of the Japanese Orbital Re-entr
y Experiment (OREX) vehicle. This vehicle is a 50-deg spherically blun
ted cone with a nose radius of 1.35 m and a base diameter of 3.4 m. Ca
lculations are performed for the OREX trajectory from a 105 to 48.4 km
altitude range. A seven-species chemical model for air is found adequ
ate for the flowfield analysis. However, for altitudes greater than 84
km, the low-density effects (such as thermal nonequilibrium and slip)
must be implemented to accurately predict flight-inferred heat transf
er rate data. At altitudes lower than 84 km, a finite surface recombin
ation probability employed in place of a noncatalytic surface enhances
the agreement between the calculations and flight data. VSL results a
re also compared with the direct simulation Monte Carlo predictions at
high altitudes (>80 km) and the electron number density data for thre
e altitudes in the OREX trajectory. Overall, the agreement between the
flight data and calculated results is quite good.